Earth's Water

Earth's water distribution
Earth's water distribution
C. M. Glee
Nov. 26, 2011
Wikipedia earth's water distribution
CC BY-SA 3.0
Earth's water is stored and located above and below Earth's surface, and in the atmosphere. More than 99% is contained in oceans, seas and bays, with small amounts in lakes, rivers and streams, with even smaller amounts hidden as permafrostthick subsurface layer of soil that remains frozen throughout the year, usually in polar regions and as water vapor in the atmosphere.

Changes in water location, availability, temperature, purity and salinitythe degree to which something is salty can produce additional climate and weather changes, flooding, droughts, disruption in the natural balances of plants and animal species and the spread of diseases.

If all of Earth's water, located in oceans, icecaps and glaciers, lakes, rivers, groundwater and water in the atmosphere, were put into a sphere, the diameter of that water ball would be about 860 miles (about 1,385 km), a little more than the distance between Salt Lake City, Utah and Topeka, Kansas. The volume of all water would be about 332.5 miles3, or 1,386 km3.[1]

A mile3 of water equals more than 1.1 trillion gallons. A km3 of water equals about 264 billion gallons, or 1 trillion liters.[1]

About 3,100 mile3 (12,900 km3) of water, mostly in the form of water vapor, is in the atmosphere. If it all fell as precipitation at once, the Earth would be covered with only about 1 inch of water.[1]

Each day, the lower 48 U.S. states receive a total volume of about 4 mile3 (17.7 km3) of precipitation and 280 mile3 (1,170 km3) of water evaporate or transpire into the atmosphere.[1]

If all of the world's water was poured on the contiguous U.S. states, it would cover the land to a depth of about 107 miles (145 km).[1]

Of the fresh water on Earth, more is stored in the ground than is available in rivers and lakes. More than 2,000,000 mile3 (8,400,000 km3) of fresh water is stored in the Earth, most within one-half mile of the surface. Most fresh water is stored in the 7,000,000 mile3 (29,200,000 km3) of glaciers and icecaps in the polar regions and in Greenland.[1]


[1] USGS. (n. d.). How much water is there on Earth?

Ice Sheets

An ice sheet forms through snowfall accumulation, when annual snowfall exceeds annual snowmelt. Snow layers build up for thousands of years, creating a flowing ice sheet thousands of meters thick. Increasing snow height puts pressure on the layers below, which deform and spread out in all directions.[1]

Earth's two ice sheetsa mass of glacial land ice extending more than 50,000 square kilometers (20,000 square miles) cover most of Greenland and Antarctica. They contain more than 99% of Earth's fresh water ice.[1]

Oct. 5, 2006
Wikipedia Antarctica
public domain
Ice Sheets[2]
location surface area in km2 volume in km3 description sea level rise
in m if melted
Antarctica 14 million 30 million approximately the size of
United States and
Mexico combined
Greenland 1.7 million 310,410,900 three times the size of

Due to increased carbon emissions and global warming they are now melting six times faster than in the 1990s, the worst-case climate warming scenario set out by the Intergovernmental Panel on Climate Change (IPCC). In the near future melting ice could produce a sea level rise that could leave 400 million people living near coasts subject to major flooding.[3]

Average annual Greenland and Antarctica ice loss in the 2010s was 475 billion tons, six times greater than the 81 billion tons lost each year during the 1990s. Between 1992 and 2017, the two ice caps lost 6.4 trillion tons of ice, 60% from Greenland, and the remaining 40% from Antarctica.[3]

In 2022, Greenland experienced its largest September melting event, due to global warming. The first day of September marks the end of the Greenland melt season, as the Sun appears to move lower in the sky, causing decreasing temperatures.[4]

But warm air moved over Baffin Bay, Baffin Bay
Baffin Bay
Jun. 12, 2009
Wikipedia Baffin Bay
CC BY-SA 3.0
resulting in tens of billions of tons of lost ice. Parts of western Greenland experienced 35oF (20oC) temperatures. About 35% of the ice was affected, far above the usual 10% for September. During the event, Greenland may have lost about 20 billion tons of ice, about 7% of the annual total ice loss.[4]

Meltwater runoff rates were as high as 12 billion tons per day, one of the top ten largest runoff events on record. If it refreezes, it creates ice sheets that prevent meltwater from percolating through snowpack, contributing to sea level rise. For every 360 billion tons of ice lost, sea level rises about 1 millimeter. Greenland is the largest contributor to that rise.[4]

Milne fjord and surrounding land
Milne fjord and surrounding land
Aug. 15, 2006
Wikipedia Milne land
public domain
Milne Fjord is a research station about 500 miles from the North Pole. It sits on the coast of a site called the Last Ice Area, a 400,000-square-mile region north of Greenland and the Canadian Arctic Archipelago, between ice floes. Its epishelf lakea freshwater lake which is dammed by an ice shelf, with a layer of freshwater floating on saltier marine water has now disappeared, due to global warming.[6]

In the past, scientists found four liquid lakes below the Greenland ice sheet, but 50 more have recently been located. There are about 470 lakes beneath Antarctica.

The largest, Lake Vostok, Satellite view of Lake Vostok
Satellite view of Lake Vostok
Goddard Spaceflight Center/NASA
May 23, 2005
Wikipedia Lake Vostok
public domain
is 250 kilometers long. The biggest subglacial lake under Greenland is only 6 kilometers in length.[5]

Water pools under ice sheets due to ice pressure from above and geothermal heat from below which keeps the water in liquid form. Melting surface water also drains into subsurface lakes.[5]

Scientists study these lakes and their interaction with the ice sheets to determine how they are affected by global warming and how they will contribute to rising sea levels.[5] If all of Greenland's ice melts, it will increase global ocean height by 7 meters.[5]


[1] National Snow & Ice Data Center. (n. d.). State of the cryosphere: Ice sheets.

[2] National Snow & Ice Data Center. (n. d.). Quick facts on ice sheets.

Why does ice float?
[3] Carrington, D. (Mar. 11, 2020). Polar ice caps melting six times faster than in 1990s. The Guardian.

[4] Patel, K., & Mooney, C. (Sep. 6, 2022). For first time on record, Greenland saw extensive melting in September. The Washington Post.

What is the source of the Ganges River?
[5] Amos, J. (Jun. 26, 2019). Greenland ice sheet: 'More than 50 hidden lakes' detected. BBC.

[6] Nunn, A. S. (Feb. 10, 2023). The 'last ice area' is already disappearing. Grist.

Arctic Region

Arctic population
Arctic population
S. Harder, Arctic Council
Jan. 1, 2009
Wikipedia Arctic
public domain
The Arctic is defined as the area within the Arctic Circle, a line of latitude about 66.5o north of the Equator. Within this circle are the Arctic ocean basin, the northern parts of Scandinavia, Russia, Canada, Greenland, Alaska, glaciers and icebergs, which make up about 20% of Earth's fresh water.[2]

Most of the Arctic consists of liquid saltwater of the Arctic ocean basin. Some parts of the ocean's surface remain frozen all year as sea ice which may be covered in snow. Sea ice affects Earth's climate by reflecting about 80% of the light that strikes it.[2]

Following sunset on the September equinox,when the Sun appears directly above the equator, rising due east and setting due west, around March 20 and September 23 the Earth's axial tiltthe 23o tilt of Earth's axis relative to the plane of its orbit around the Sun and revolutionrefers to Earth's orbit around the Sun of approximately 365 days, 6 hours, 9 minutes around the sun reduce the light and heat reaching the Arctic until no sunlight penetrates the darkness.[2]

The sun rises again during the March equinox and increases the light and heat reaching the Arctic. By the June solsticeoccurs when the Sun appears to reach its most northerly, around June 21, or southerly, around December 21, positions relative to the celestial equator on the celestial sphere the Arctic experiences 24 hours of daylight.[2]

The Arctic includes the Bering, Beaufort and Chukchi seas, and sea ice, coastal wetlands, upland tundra,a vast, flat, treeless Arctic region of Europe, Asia and North America in which the subsoil is permanently frozen mountains, wide rivers. About 4 million people from several cultures live in the Arctic, parts of which belong to 8 different countries.[1]

Frozen Arctic soil holds about 1,460 to 1,600 billion tons of trapped carbon, about twice the amount in the atmosphere.[3]

Greenhouse gases from fossil fuel burning is causing temperatures in the Arctic to warm at twice the rate of the rest of the world.[2] Methanea powerful greenhouse gas and the simplest hydrocarbon, consisting of one carbon atom and four hydrogen atoms and carbon are found in Arctic permafrost,thick subsurface layer of soil that remains frozen throughout the year, usually in polar regions frozen peat bogs and under sea floor sediment. As they thaw, methane and carbon are released into the atmosphere, adding more global greenhouse gases and global warming. More warming results in more permafrost loss and more atmospheric greenhouse gases.[3]

What happens in the Arctic has an effect on wildfires in the western U.S. Ice loss causes land and sea surface warming, resulting in hotter and drier summers subjected to fire-related conditions.[4]

Arctic Ocean ice helps regulate global land and sea temperatures. White sea ice reflects about 50 to 70% of solar radiation, preventing Earth from getting warmer.[3]

Perennial Arctic Sea ice decline 1984-2016
Oct. 29, 2016
Embedded video, no copy made
But Arctic sea ice is shrinking. While the lowest amount ever recorded was in 2012, 2022 Arctic sea ice extent was tied with 2007 and 2016 for the second-lowest minimum on record. An NOAA report concluded that Arctic sea ice shrunk by 40% since 1979.[3]

Disappearing sea ice also exposes the darker ocean surface. The ocean reflects only 6% of solar radiation, absorbing the rest and warming water and surrounding atmosphere. The disappearance of this ice is moving toward an irreversible tipping point. Within the next 20 to 25 years, there may be no sea ice in September in the Arctic.[3]

Fossil fuels also increase the acidity of Arctic water, harming zooplankton,plankton consisting of small animals and the immature stages of larger animals which are the base of the Arctic food chain.[1]

The decrease in volume and extent of Arctic sea ice has serious implications for the habitat of polar and brown bears, several whale species, ringed seals, Arctic wolves, Pacific salmon, porpoises and dolphins that live on Arctic land and the surrounding sea.[2]

The reduction in sea ice has warmed Alaska's climate, accelerated coastal erosion, reduced walrus and other marine mammal habitat, changed the timing and location of microscopic plant life and lowered survival rates for some fish species.[3]


What is the world`s second largest ice sheet?
[1] World Wildlife Fund. (2022). Arctic.

[2] National Geographic Society. (2022). The Arctic.

[3] The Climate Reality Project. (n. d.). How feedback loops are making the climate crisis worse.

[4] Berwyn, B. (Jul. 27, 2022). Wildfire pollution may play a surprising role in the fate of Arctic sea ice. Inside Climate News.,will%20disappear%20completely%20in%20summer.

Antarctic Region

Jan. 1, 2009
Wikipedia Antarctica
public domain
With about 98% of its land covered by ice, Antarctica is the highest, driest, windiest, coldest and iciest continent. It is about about 5.5 million square miles (14.2 million square km). It is divided into East Antarctica, composed of a high ice-covered plateau, and West Antarctica, an ice sheet covering a mountainous archipelagoan area that contains a chain or group of islands scattered in lakes, rivers or the ocean[1]

The ice sheet contains approximately 7 million cubic miles (about 29 million cubic km) of ice, representing about 90% of the world's ice and 80% of its fresh water. Its average thickness is about 5,900 feet (1,800 m).[1]

Ice shelves cover parts of the Ross and Weddell seas. The Ross Ice Shelf, the Filchner-Ronne Ice Shelf and other continental margin shelves create the border of about 45% of the continent. Around the coast, shelves, glaciers and ice sheets release icebergs into the seas.[1]

Scientific investigation began during the 1957-58 International Geophysical Year (IGY). On December 1, 1959, the 12 countries active in Antarctica during the IGY signed the Antarctic Treaty, preserving the continent for nonmilitary scientific pursuits and placing Antarctica under an international regime binding members to review of its provisions after 30 years. The treaty placed the boundary at 60o south latitude.[1]

The 1991 Madrid Protocol prohibited mining, required environmental impact assessments for new activities, and designated the continent as a natural reserve.[1]

Scientists have mapped the continent's mountain regions, and until the 1970s relied on ground-based seismic surveys to find mountain ranges and peaks. Airborne radio-echo sounding systemsa transmitter and receiver system that sends out radio waves and detects those waves bounced from objects now measure ice-thickness, facilitating systematic surveys.[1]

An underwater robot called Icefin deployed beneath the Thwaites ice shelf and confirmed that it is one of the least stable ice shelves in Antarctica. Researchers estimate that its collapse could lead to a two-foot rise in sea level over the next few centuries. Thwaites contributes about 4% to current overall rate of global sea level rise, about 1.5 inches per decade.[2]

Why are massive ocean currents slowing down?
Australian Academy of Sciences
Mar. 29, 2023
Embedded video, no copy made
Antarctic waters are warming because of climate change. As warmer water flows beneath the ice shelf, it melts, thinning and weakening the shelf. Its grounding linethe region where ice transitions from a grounded ice sheet to freely floating ice shelf has moved inland about 8 miles over the past two decades.[2]

Fresh water melting ice could slow currents by as much as 40% in the next 30 years by reducing ocean salinity. Slower currents deliver less oxygen, carbon dioxide and nutrients to the world's marine ecosystem and warmer water can't absorb as much atmospheric carbon dioxide as in the past.[3]

Deeper and warmer water creates a positive environmental feedback loop.accelerates an environmental response, such as increasing ice melting rates or raising global temperatures More melting releases more fresh water into the oceans, affecting rainfall and agriculture.[3]


[1] van der Watt, L. (May 20, 2022). Antarctica. Encyclopedia Britannica.

[2] Fountain, H. (Feb. 15, 2023). Scientists get a close-up look beneath a troubling ice shelf in Antarctica. The New York Times.

What mountain range`s snow feeds the Amazon River?
[3] Myers, K. (Apr. 3, 2023). Melting Antarctic ice may strangle vital ocean currents. Grist.


Glaciers, made from compressed snow that develops into thick ice masses, have been melting since the early 1900s and 95% of the oldest and thickest ice in the Arctic has disappeared.[5]

Pakistan's Baltoro Glacier is one of the world's longest alpine glaciers
Pakistan's Baltoro Glacier is one of
the world's longest alpine glaciers
G. Vellut
Oct. 23, 2005
Wikipedia glacier
CC BY-SA 2.0
Unlike ice sheets, which flow in all directions, glaciers flow like rivers, usually due to gravity. Glacier sizes range from a few hundreds of meters to hundreds of kilometers in length.[1]

About 10% of Earth's surface is covered by glaciers, most of which are located in Antarctica, Greenland, and the Canadian Arctic. Most glaciers were formed during the Little Ice Ageclimate cooling period that occurred from the early 14th century through the mid-19th century, when mountain glaciers expanded at several locations, including the European Alps, New Zealand, Alaska, and the southern Andes, and mean annual temperatures across the Northern Hemisphere declined by 0.6Co when ice covered about 32% of Earth's land area, and 30% of the oceans.[1]

There are several types of glaciers: calving,a glacier that ends in a body of water into which it drops icebergs cirque,a small glacier that forms in a basin high on the side of a mountain hanging,a glacier that begins high on a glacier valley wall and descends only part of the way to the surface of the main glacier piedmont,a fan or lobe-shaped glacier, located at the front of a mountain range polar,a glacier in which ice temperatures always remain below the freezing point reconstituteda glacier formed below the bottom of a hanging glacier by the accumulation, and reconstitution by pressure melting of ice blocks that have fallenor avalanched from the end of the hanging glacier rock,a glacier-like landform that consists of a valley-filling accumulation of angular rock blocks, has little or no visible surface ice temperate,a glacier in which liquid water coexists with glacier ice during part or even all of the year tidewatera glacier that ends in a body of water influenced by tides, such as the ocean or a large lake and valley.a glacier that flows for all or most of its length within the walls of a mountain valley, also called an alpine glacier or a mountain glacier[2]

Glacier facts:

Global warming is having a significant effect on Earth's glaciers:

The number of glacial lake outburst floodsa flood caused by the failure of a dam containing a glacial lake has increased significantly since 1990, affecting nearly 15 million people. About 1 million residents of High Mountains Asia live within 10 kilometers of a glacial lake, with more than half living in India, Pakistan, Peru and China.[7]

While white snow is Earth's most reflective surface, pink algae, found at high altitudes on glaciers, forms what scientists call watermelon snow. This pink snow absorbs heat, forcing snow to melt quickly, leaving large pools of red water. Scientists are studying how this algae, Chlamydomonas nivalis, affects seasonal water supplies and its potential impact on flooding and how climate change may alter the algal growth.[6]


[1] National Snow & Ice Data Center. (n. d.). What is a glacier?

Watermelon snow on Mount Ritter in California
Watermelon snow on Mount Ritter in California
Pacific Southwest Forest Service/P. Wade
Aug. 29, 2017
Wikipedia watermelon snow
public domain
[2] USGS. (n. d.). Glossary of glacier terminology.

[3] National Snow & Ice Data Center. (n. d.). Glacier quick facts.

[4] Glick, D. (n. d.). The big thaw. National Geographic.

[5] World Wildlife Foundation. (2022). Why are glaciers and sea ice melting?

[6] Mohr, K. (Nov. 29, 2022). Pink snow is a red flag for the West's water. High Country News.

[7] Taylor, C., et al. (2023). Glacial lake outburst floods threaten millions globally. Nature Communications, 14(487).

Oceans, Seas, Currents

Earth has 5 major oceans: Pacifichome to the Mariana trench, the deepest oceanic trench on Earth, measuring about 2,550 kilometers (1,580 miles) in length and 69 kilometers (43 miles) in width.[1], Atlanticthe breakup of Pangaea created the Atlantic Ocean[2], Indianthe smallest and geographically youngest ocean[3], Southernwater cooled by cold air, outgoing radiation, and katabatic winds off of the Antarctic continent sinks and flows northward along the ocean bottom and replaced at the surface by warmer water flowing south from the Indian, Pacific, and Atlantic oceans[4] and Arcticalmost completely circled by North America, Eurasia, and Greenland[5] that are all part of a global ocean.

Perpetual Ocean
NASA/Goddard Spaceflight Center
Jul. 13, 2013
Embedded video, no copy made
Sea level is measured using tide stationsa device that enables sea water to enter a well that measures the water height and satellite laser instrument that measures altitude These measurements show that seal level is rising about an eighth of an inch per year.[17]

The Pacific contains the Middle America trench middle_america_trench
Middle America trench
U.S. Government
Mar. 8, 2006
Wikipedia Middle America trench
public domain
located off the west coast of Central Ameica. It extends northwest-southeast for more than 1,700 miles (2,750 km) from central Mexico to Costa Rica. The trench reaches a maximum depth of 21,880 feet (6,669 m) and covers a total area of 37,000 square miles (96,000 square km).[23]

The Peru-Chile trench, Peru-Chile trench
Peru-Chile trench
U.S. Government
Mar. 7, 2006
Wikipedia Peru-Chile trench
public domain
also called Atacama Trench, is a submarine trench in the eastern Pacific Ocean, about 100 miles (160 km) from the Peru and Chile coast. It reaches a maximum depth of 26,460 feet (8,065 m) below sea level in Richards Deep and is approximately 3,666 miles (5,900 km) long. It covers about 228,000 square miles (590,000 square km).[24]

The Mariana trench Mariana trench
Mariana trench
Aug. 7, 2007
Wikipedia Mariana trench
CC BY 2.5
is located in the western North Pacific.[21] It is about 35, 876 feet (10, 935 m) deep. It was designated a U.S. national monument in 2009.[22]

More than 70% of Earth's surface is covered by water. The deepest known ocean depth is nearly 11,000 m (36,000 feet or almost 7 miles).[11] Scientists estimate the hydrospherethe combined mass of water found on, under, and above Earth`s surface contains about 1.36 billion cubic kilometers of water. The second most common form of the water molecule on our planet is ice. If all of Earth's ice melted, sea-level would rise by about 70 meters.[6]

Ocean currents, which can flow for thousands of kilometers, are generated by Earth's rotation, the wind, temperature gradients,an increase or decrease in the magnitude of a physical property salinitythe degree to which something is salty variations, density and the gravitational influence of the Moon. Ocean depths, shorelines, and other currents affect current strength, direction and speed. Currents influence climate.[7]

The Gulf Stream, Peru-Chile trench
Gulf Stream
May 24, 2006
Wikipedia Gulf Stream
public domain
for example, makes northwest Europe much more temperate than any other region at the same latitude.[7]

Thermohalinerelating to the effects of temperature and salinity circulation produces conveyor-belt like motion in deep ocean density-driven currents called submarine rivers.a river-like current on the seabed [7]

Studies have suggested that one of the world's largest currents, the Atlantic Meridional Overturning Circulation (AMOC), Atlantic Meridional Overturning Circulation
Atlantic Meridional Overturning Circulation (AMOC)
C. Lee
Oct. 30, 2021
Wikipedia Atlantic meridional overturning circulation
CC BY-SA 4.0
is slowing down due to global warming. The AMOC helps move heat between the equator and the Arctic. It also regulates climate and weather patterns in the Northern Hemisphere. Some scientists have warned that this current may disappear.[12]

Oct. 8, 2007
Wikipedia ocean
public domain
Earth's Oceans➔
ocean surface area in km2 volume in km3 description percent
Pacific 162,250,000 669,880,000 largest and deepest ocean 48.3
Atlantic 106,460,000 310,410,900 extends between
Europe and Asia
Indian 70,560,000 264,000,000 world's warmest ocean,
bounded by Asia on the north,
Africa to the west,
Australia to the east
Southern 71,800,000 20,330,000 composed of water from
the South Pole to
60oS latitude
Arctic 18,750,000 14,060,000 the smallest and
shallowest ocean

There are five major gyres:large systems of rotating currents the North and South Pacific Subtropical gyres, the North and South Atlantic Subtropical gyres, and the Indian Ocean Subtropical gyre.[9]

The 1958 Convention on the High Seas established that the high seas were open to all nations for freedom of navigation, freedom of fishing, freedom to lay submarine cables and pipelines and freedom to fly over the high seas. The convention also addressed safety, warships, piracy and pursuit.[26]

The 1982 Law of the Sea Conventionoff (LOSC) established a legal framework for the use and protection of natural and cultural resources of the sea, the seabed and subsoil and the marine environment. The LOSC includes clear guidelines on states' navigational rights, maritime zones and boundaries and economic jurisdiction. It also provides international cooperation and dispute resolution guidelines. The U.S. is not a party to the LOSC but follows it. The treaty has not obtain sufficient Congressional support needed for U.S. accession.[25]

In April 2023 a new U.N. high seas treaty was written to address rules that have failed to prevent fishery depletion, loss of fragile habitats, decline of whale, sea turtle and bird populations and other marine life and ambiguities and lack of cooperation between entities claiming to have legal jurisdiction. It would also establish marine protected areas (MPAs).areas that include marine sanctuaries, estuarine research reserves, ocean parks and marine wildlife refuges[27]

According to the U.S. Department of Energy ocean tides and river currents generate a small fraction of U.S. electricity today, but have the the potential to account for about 8% of U.S. power generation in the future.[15]

The U.N. Environmental Program estimated that each year, about 11 million tons of plastic end up in the oceans. Approximately 300 million tons of plastic waste, equal to the weight of the world's human population, are produced every year. About 9% is recycled. The rest accumulates in landfills and the environment.[13]

The Great Pacific Garbage Patch, about the size of Texas, is a Pacific Ocean zone between Hawaii and California with a high plastic waste concentration. Garbage from the west coast of the U.S. and east coast of Japan is carried by the California current, the North Equatorial current, the North Pacific current, and the Kuroshio current to the North Pacific subtropical gyre, the clockwise rotation of which draws in and traps solid matter including plastics.[8]

Ocean currents
Ocean currents
M. Pidwirny
Aug. 10, 2007
Wikipedia ocean currents
public domain
Over time, larger pieces break into microplastics, which seep into the food chain, water systems and the atmosphere.[13] The garbage undergoes photodegradationdecay of material due to light exposure causing the small pieces to break down further, into tiny, nearly invisible pieces, creating a microplastic soup. The patch's dimensions and depth change constantly.[8]

The ocean's plastic problems have been known since the late 1980s. In 2015 and 2016, Ocean Cleanup discovered that the garbage patch plastic density was more than expected and that the plastics absorbed pollutants, making them poisonous to marine life.[8]

Scientists discovered that garbage patch plastics are providing a home for coastal species in the open ocean. Some of these species, including bryzoans,a non-moving aquatic invertebrate of the phylum Bryozoa which comprises of the moss animals jellyfish, sponges and worms, are reproducing in their new and alien environments along with open ocean species. Future research may determine whether these coastal and open ocean species are competing or cooperating.[19]

The International Coastal Cleanup® began more than 35 years ago, with coastal Texas community working together to collect and document coastal litter. Local and state volunteers in the U.S. and more than 150 countries participate in a cleanup events.[14]

In March 2023 scientists found more than 13 million tons of Sargassumbrown algae with leafy segments, air bladders or spore-bearing structures drifting in the Atlantic Ocean. The seaweed is washing up on beaches in southwest Florida and Mexico.[20]

Larger than usual mats were first identified in 2011. Scientists speculate that nutrient-rich runoff from the Congo, Amazon and Mississippi Rivers is encouraging algae growth. When Sarassum reaches the shore it decomposes, degrades water quality, pollutes beaches and produces hydrogen sulfide.gaseous substance found in several inorganic water pollutant such as electric power waste, oil and gas extraction operations waste, sewage treatment plants, large pig farms and other confined animal feeding operations, Portland cement kilns, municipal waste landfills, coke ovens, sulfur products, asphalt production and storage and geothermal power plants[20]

Oceanic basins consist of continental shelves,a portion of a continent that is submerged under an area of relatively shallow water continental slopes,the slope between the outer edge of the continental shelf and the deep ocean floor abyssal plains,an underwater plain on the deep ocean floor abyssal hills,a hill that rises from the sea floor seamounts,a large ocean mountain that does not rise above the sea surface ocean trenches,a long, narrow depression in the ocean floor volcanic islandsan island created from volcanic eruptions[10] and six zones:

In March 2023 193 countries agreed on a world ocean protection treaty. Work on the agreement began at the U.N. in 2004 and it has not been formally adopted or ratified by its individual member countries. If ratified, the treaty will establish a new set of rules on the high seasopen ocean that begins 200 nautical miles from a coastline and is not under the jurisdiction of the laws of any specific country aimed at protecting marine species and the balance of its ecosystems.[16]

Territorial seas are coastal ocean waters subject to the jurisdiction of coastal nations that extend up to 12 nautical milesunit used in measuring distances at sea equal to approximately 2,025 yards or 1,852 meters from shore. These seas:


Which continent is the driest?
[1] Cotter, C. H. (n. d.). Pacific Ocean. Encyclopedia Britannica.

[2] LaMourie, M. J. (n. d.). Atlantic Ocean. Encyclopedia Britannica.

[3] Verlaan, P. A. (n. d.). Indian Ocean.

[4] Editors of Encyclopedia Britannica. (n. d.). Southern Ocean. Encyclopedia Britannica.

[5] Ostenso, N. A. (n. d.). Arctic Ocean. Encyclopedia Britannica.

Ocean divisions
Ocean divisions
C. Huh
Aug. 16, 2006
Wikipedia abyssal plain
public domain
[6] (n. d.). Physical properties of water.

[7] Science Daily. (n. d.). Ocean current.

[8] Bauer, P. (2022). Great Pacific garbage patch. Encyclopedia Britannica.

[9] National Oceanic and Atmospheric Administration. (n. d.). What is a gyre?

[10] National Oceanic and Atmospheric Administration. (May 1, 2020). Ocean floor features.

[11] Oceana. (n. d.). Open oceans.

[12] Harvey, C. (Mar. 8, 2022). Amazon rain forest nears dangerous 'tipping point.' Scientific American.

[13] U.N. Environment Program. (Feb. 16, 2022). World leaders set sights on plastic pollution.

Ocean basins
Ocean basins
C. Huh
Mar. 20, 2017
Wikipedia abyssal plain
public domain
[14] Ocean Conservancy. (2022). Fighting for trash free seas. International Coastal Cleanup®

[15] Winters, J. (Oct. 24, 2022). An untapped source of power: Rivers and tides. Grist.

[16] Teirstein, Z. (Mar. 6, 2023). UN reaches historic agreement to protect the world's oceans. Grist.

[17] National Ocean Service. (n. d.). Is sea level rising? NOAA.

[18] (n. d.). The case for protecting and managing the world's territorial seas.

[19] Bartels, M. (Apr. 17, 2023). Surprising creatures lurk in the Great Pacific Garbage Patch. Scientific American.

[20] Shao, E. (Apr. 19, 2023). Those seaweed blobs headed for Florida? See how big they are. The New York Times.

[21] McKenna, A. (n. d.). Mariana trench. Encyclopedia Britannica.

[22] National Oceanic and Atmospheric Administration. (n. d.). How deep is the ocean? National Ocean Service.,meters%20(35%2C876%20feet)%20deep.

[23] Gorlinski, V. (n. d.). MIddle America trench. Encyclopedia Britannica.

[24] Editors of Encyclopedia Britannica. (n. d.). Peru-Chili trench. Encyclopedia Britannica.

[25] National Oceanic and Atmospheric Administration. (n. d.). Law of the Sea convention.,both%20natural%20and%20cultural%20resources.

[26] United Nations. (2005). Convention on the high seas. Treaty Series, vol. 450, p. 11, p. 82.

[27] Turrentine, J., & Palmer, B. (Apr. 14, 2023). Finally, a high seas treaty to protect the world's oceans. NRDC.


A river forms when water moves from uphill at a higher elevation to downhill, at a lower elevation, because of gravity. Small creeks and streams frequently merge to form rivers, most of which flow into oceans.[1]

Rivers contain fresh water,characterized by having low concentrations of dissolved salts and other total dissolved solids and all of the world's rivers carry about 3.6 billion metric tons of salt from land to the ocean each year.[2]

River water sources include melting glaciers, like the Gangotri glacier Gangotri glacier
Gangotri glacier
P. Basak
Sep. 8, 2015
Wikipedia Gangotri glacier
CC BY-SA 4.0
the source of the Ganges River in Asia. The snows of the Andes feed the Amazon River. A river's source could be a lake with an outflowing stream, such as Lake Itasca Lake Itasca Mississippi source
Lake Itasca Mississippi source
C. Karim
May 25, 2004
Wikipedia Lake Itasca
CC BY-SA 3.0
in Minnesota, as the source of the Mississippi River. The source of the Danube River Danube River in Budapest
Danube River in Budapest
Visions of Domino
Jul. 5, 2016
Wikipedia Danube River
CC BY-SA 2.0
is a spring in the Black Forest of Germany.[5]

Rivers can form estuaries,the tidal mouth of a large river, where the tide meets the stream and large sources of brackish water.having more salinity than fresh water, but not as much as seawater

Oceans are what percent of Earth`s living space?
Rivers and their floodplainsan area of low-lying ground adjacent to a river, formed mainly of river sediments and subject to flooding provide habitats for aquatic animals and terrestrial species. Many of the world's large rivers experience an annual flooding cycle that is important for spreading water, nutrients and sediment into floodplains.[3]

Many cities were established around rivers, which were used primarily for irrigation, drinking water, and waste disposal, and later for power generation.[1]

The Colorado River at Horseshoe Bend, Page, Arizona
The Colorado River at Horseshoe Bend, Page, Arizona
P. Hermans
Sep. 27, 2012
Wikipedia rivers
CC BY-SA 3.0
Large dams have been constructed near rivers to reduce flooding and to produce hydroelectricity. Sometimes these mitigation actions taken to reduce the seriousness of something efforts work, but sometimes they do not, leaving those who move into locations where mitigation has been attempted subject to unpredictable water flows, flooding and environmental damage.[3]

Only 17% of rivers are free-flowing and within protected areas. Freshwater species have declined by 84% since 1970 as a result of river degradation. Free-flowing rivers sustain diverse ecosystems and food chains, provide drinking water and serve as cultural sites for billions of people.[8]

An Oregon State University study concluded that in the past 20 to 30 years 70% of fish species in Japanese and New Zealand rivers were threatened or endangered. Poor living conditions for fish and insects exist in 50% of European, 44% of U.S., 25% of South Korea and 30% of Australian rivers.[9]

Water resources managers and scientists explore ways to restore natural river environments without further flood damage. One of the solutions involves controlled water release from reservoirsa large natural or artificial lake used as a source of water supply to reconstruct natural flood patterns.[3]

The Amazon carries more water than any other river on Earth and about one-fifth of all fresh water to the oceans.[5]

The Mississippi River is North America's largest, connecting the Ohio River to the east and Missouri River to the west.[3] In October 2022, low water levels in the Mississippi backed up about 3,000 barges. The river and its tributaries transport more than $17 billion of farm products.[6]

Some states fed by Mississippi water are developing new ways to deal with decreasing water, including low-impact hydropower, naturally moving sediments to restore water habitats and utilizing satellite images to create three dimensional measurements of water levels and distribution.[6]

Oceans, seas and bays contain what percent of Earth`s water?
An American Rivers report listed the Upper Mississippi River as the most endangered river of 2020 as a result of climate change, changes in land use, artificial cropland drainage and poor watershed management and planning. The river is prone to deadly flooding which is predicted to increase. In 2019 floods on the river broke records resulting in submerged homes, farms, roads and businesses for almost 100 days.[7]

American Rivers called on governors in Iowa, Illinois, Missouri, Minnesota and Wisconsin to fund the Keys to the River 2020: An Upper Mississippi River Flood Risk, Sediment and Drought Study completed by the Army Corps of Engineers.[7]

Redlining,refusing a loan or insurance to someone because they live in an area deemed to be a poor financial risk economic injustice and leveean earthen barrier along a stream, lake or river that protects the surrounding land from flooding failures disproportionally affect low income communities which are often left out of decision-making processes aimed at economic growth, rather than human impacts.[7]

U.S. rivers
U.S. rivers
U.S. Department of the Interior
Jul. 27, 2009
Wikipedia list of rivers of the United States
public domain
America's Most Endangered Rivers of 2020[7]
river↕ states threats
Upper Mississippi Illinois, Iowa, Missouri, Minnesota, Wisconsin climate change,
poor flood management
Lower Missouri Missouri, Iowa, Nebraska, Kansas climate change,
poor flood management
Big Sunflower Mississippi Yazoo pumps project
Puyallup Washington Electron Dam
South Fork Salmon Idaho gold mine
Menominee Michigan, Wisconsin open pit sulfide mining
Rapid Creek South Dakota gold mining
Okefenokee Swamp Georgia, Florida titanium mining
Ocklawaha Florida Rodman Dam
Lower Youghiogheny Pennsylvania natural gas development

In 2023, the American Rivers list, based on river significance to people and wildlife, river threats and public influence, had changed.

America's Most Endangered Rivers of 2023[10]
river↕ states threats risk
Colorado Arizona, California, Colorado, Nevada, New Mexico, Utah, Wyoming climate change,
outdated water management
ecosystem health, reliable water delivery, regional economy
Ohio Pennsylvania, Ohio, West Virginia, Kentucky, Indiana, Illinois pollution,
climate change
clean water for 5 million people
Pearl Mississippi dredging and dam construction clean drinking water, local and downstream community health, fish and wildlife habitats
Snake Idaho, Oregon, Washington four federal dams Tribal treaty rights and culture, endangered salmon runs, rural and local community health
Clark Fork Montana pulp mill pollution public health, fish and wildlife habitats
Eel California dams fish and wildlife habitats, Tribal culture and sustenance
Lehigh Pennsylvania poorly planned development clean water, fish and wildlife habitats, rural and local community health, open spaces
Chilkat and Klehini Alaska mining bald eagle, fish and wildlife habitats, Tribal culture and sustenance
Rio Gallinas New Mexico climate change, outdated forest and watershed management clean driking water, farming, watershed operation
Okefenokee Swamp Georgia, Florida mining fish and wildlife habitats, wetlands, water quality

The U.S. and Canada share the Columbia River and the St. Lawrence River. In the Pacific Northwest, the Columbia and its dams comprise the world's largest hydropower system, and those dams have caused contention between salmon fisheries and dam operators. The boundary between eastern Canada and the U.S. is formed by the St. Lawrence, which flows into the Atlantic Ocean.[3]

In the southwestern U.S., the Colorado River flows through arid and highly populated regions, providing water to millions of people. This river has been so dammed and diverted that it no longer reaches its previous mouth, and now ends, dried up in the Mexican desert. Environmental groups are developing strategies for restoring the Colorado to its previous conditions.[3]

Nile River at night
Nile River at night
Nov. 8, 2010
Visible Earth
public domain
World's 10 Longest Rivers[4]
river↕ tributaries↕ countries↕ outflows
in km↕
area in
Nile White Nile, Kagera,
Mwogo, Rukarara
Ethiopia, Eritrea,
Sudan, others
Mediterranean 6,650 3,349,000
Amazon Ucayali, Tambo,
Ene, Mantaro
Brazil, Peru,
Bolivia, others
Atlantic Ocean 6,575 6,915,000
Yangtze Jinsha, Tongtian,
Ulan Moron
China East China Sea 6,300 1,800,000
Mississippi Missouri, Jefferson,
U.S. Gulf of Mexico 6,275 3,230,000
Yenisei Angara, Selenge,
Kara Sea 5,539 2,580,000
Huang He   China Bohai Sea 5,464 745,000
Ob-Irtysh   Russia,
China, Mongolia
Gulf of Ob 5,410 2,990,000
Río de la Plata Paraná,
Rio Grande
Brazil, Argentina
Paraguay, others
Rio de la Plata 4,880 2,582,672
Congo Chambeshi Dem. Rep. Congo,
Cen. African Rep.,
Angola, others
Atlantic Ocean 4,700 3,882,000
Amur Argun, Kherlen Russia, China,
Sea of Okhotsk 4,444 1,855,000

Rivers have played major roles in history, transportation, warfare, culture and geography. Civilizations have grown around river deltas, where food could be easily grown and traded.

Amazon River
Amazon River
Feb. 25, 2013
Wikipedia Amazon River
CC BY-SA 3.0
Historically Significant Rivers[5]
river↕ length
in km↕
continent↕ country/state↕
Amazon 6,575 South America Peru, Ecuador, Colombia, Venezuela, Bolivia, Brazil
Colorado 2,334 North America Colorado, Utah, Arizona, Nevada, California
Congo 4,700 Africa Republic of the Congo, Central African Republic, eastern Zambia, northern Angola, parts of Cameroon, Tanzania
Darling 1,472 Australia New South Wales
Euphrates 2,800 Asia Iraq, Syria, Turkey
Hudson 507 North America New York
Mississippi 3,766 North America Minnesota, Wisconsin, Iowa, Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, Louisiana
Murray 2,508 Australia New South Wales, South Australia Victoria
Nile 6,650 Africa Burundi, Ethiopia, Egypt, Sudan
Rhine 1,233 Europe Switzerland, Liechtenstein, Austria, Germany, France, Netherlands
St. Lawrence 1,197 North America Ontario and Quebec in Canada, Minnesota, Wisconsin, Illinois, Indiana, Ohio, Pennsylvania, New York, Vermont, Michigan
Thames 346 Europe England
Tigris 1,900 Asia Iran, Iraq, Turkey, Syria
Volga 3,685 Europe Russian Federation
Yangtze 6,300 Asia China

What made recent western U.S. wildfires more extreme?
[1] USGS. (n. d.). Rivers, streams, and creeks.

[2] National Geographic. (n. d.). River.

[3] Water Encyclopedia. (n. d.). Rivers, major world.

[4] Gupta, A. (2007). Large rivers: Geomorphology and management.

[5] National Geographic. (2022). Understanding rivers.

Ice melting in what location is responsible for Texas` rising coastal sea level?
[6] Smith, L. C. (Nov. 27, 2022). Long stretches of the Mississippi River have run dry. What's next? The New York Times.

[7] Water Online. (Apr. 14, 2020). Mississippi River named America's #1 most endangered river.

[8] The NAU Review. (May 12, 2021). Only 17 percent of free-flowing rivers are protected, new research shows.,rely%20on%20them%20%E2%80%94at%20risk.

[9] Oregon State University. (Feb. 17, 2021). Biological assessment of world's rivers presents incomplete but bleak picture.

[10] Dominguez, C. (Apr. 18, 2023). American Rivers announces America's most endangered rivers of 2023. Water Online.


Lakes are created when large basins are filled with water. Basins have been formed by glaciers during ice ages, and dams that were created by rocks and debris left behind. The lakes in Minnesota, "The Land of 10,000 Lakes," and the Great Lakes were created by glaciers.[1] Most of these lakes, including the Great Lakes, are often hundreds of meters deep.[3]

Both the Caspian Sea Caspian Sea
Caspian Sea
J. Schmaltz, MODIS Rapid Response Team/NASA
Jun. 11, 2003
Wikipedia Caspian sea
public domain
and Lake Baikal Lake Baikal
Lake Baikal
J. Descloitres, MODIS Land Rapid Response Team, NASA
Oct. 23, 2001
Wikipedia Lake Baikal
public domain
were formed by plate tectonics which created faults, natural lake basins.[1] Baikal is the world's oldest and deepest fresh water lake, and more water than all of the Great Lakes combined.[3]

What is the largest ocean?
Other lakes were formed from inactive volcanoes and calderas,a bowl-shaped depression that forms when a volcano collapses which filled with melted snow or rain. Oregon's Crater Lake Crater Lake in Winter
Crater Lake in Winter
Nov. 14, 2012
Wikipedia Crater Lake
CC BY-SA 3.0
was created when Mount Mazama's volcanic cone collapsed.[1]

Some lakes are created by rivers forming meanders.a river following a winding course The lake left behind is called an oxbow lake.a curved lake formed where the main stream of a river has cut across the narrow end and no longer flows around the loop of the bend[1]

Lakes can also be created by landslides or mudslides, creating piles of debris blocking the flows of streams. Beavers also create natural dams out of tree branches can plug up rivers or streams and make large ponds or marshes.[1]

First letters of U.S. Great Lakes spell what common word?
Fresh water lakes contain about 98% of usable surface water, and play a significant role in the water cycle, as water vapor from lake surfaces evaporate into the atmosphere, falling later as precipitation. These lakes receive the drainage from vast tracts of land, store it, pass it on seaward, or lose it to the atmosphere by evaporation. Small lakes have a high surface area to volume ratio, and an even higher evaporation rates per volume.[2]

The Great Lakes
The Great Lakes
NASA/Goddard Spaceflight Center
Apr. 24, 2000
Wikipedia Great Lakes
public domain

Most lakes contain fresh water, but some lakes become saline when their waters cannot combine with other fresh water lakes and rivers. Some of these lakes were formed when they were connected to seas, but they have been shrinking since the last ice age. Lake Bonneville,Lake Bonneville
Lake Bonneville
May 1, 2019
Wikipedia Lake Bonneville
public domain
an ancient U.S. lake, was once as big as Lake Michigan, and the Great Salt Lake Great Salt Lake
Great Salt Lake
J. Morris
Dec. 16, 2008
Wikipedia Great Salt Lake
CC BY-SA 3.0
was once about 14 times larger than it is now, and it is saltier than the oceans.[3]

Most lakes support a lot of aquatic life, but life is rarer in salty lakes. The Dead Sea Dead sea halite deposits
Dead sea halite deposits
Mar. 17, 2012
Wikipedia Dead Sea
CC BY-SA 3.0
in the Middle East is too salty to support aquatic life.[3]

The Aral Sea,Aral Sea
Aral Sea
Aug. 10, 2017
Wikipedia Aral Sea
CC BY-SA 4.0
located in Central Asia, is one of the world's largest inland water bodies. in the second half of the 20th century its area was reduced by two-fifths and its level dropped by more than 12 meters, because of the diversion of the Syr DaryaSyr Darya
Syr Darya
Feb. 5, 2010
Wikipedia Syr Darya
CC BY-SA 4.0
and Amu DaryaAmu Darya
Amu Darya
J. Pyrek
Feb. 10, 2010
Wikipedia Amu Darya
CC BY-SA 2.0
rivers, for field irrigation.[2]

Some lakes, like the Chad BasinChad Basin
Chad Basin
Sting and Aymatth2
May 6, 2013
Wikipedia Chad Basin
CC BY-SA 3.0
in Africa, have no outflow. Their levels rise and fall based on local climate conditions and water usage.[2]

Lakes serve as recreational scenic sites. Their water is an important natural resource. They serve as habitats for aquatic and wildlife.[2]

Lake ecosystems are easily affected by their environments, including the purity of local groundwater and human activities, which can be mitigated if those affects are identified. Nutrients, including fertilizer phosphorousa poisonous, combustible nonmetal which exists as white phosphorus, a yellowish waxy solid which ignites spontaneously in air and glows in the dark, and red phosphorus, a less reactive form used in making matches and nitrogena colorless, odorless unreactive gas that forms about 78% of Earth's atmosphere can significantly affect algae growth, producing bacteria.

Many cities have human-made lakes in parks.[3] Water quality in those lakes need to be continuously monitored and maintained because humans and their pets drink, swim in, sail, and kayak in those waters.

Caspian Sea
U. Dedering
Nov. 26, 2010
Wikipedia Caspian Sea
CC BY-SA 3.0
Largest Lakes[4]
lake ↕ location ↕ type ↕ surface area in km2 volume in km3
Caspian Sea Azerbaijan-Russia-
salt water 371,000 78,200
Lake Superior U.S. and Canada fresh water 82,170 12,232
Lake Victoria Tanzania-Uganda fresh water 68,800 2,424
Lake Huron U.S. and Canada fresh water 59,600 3,538
Lake Michigan U.S. fresh water 58,000 4,918
Tanganyika Tanzania-Congo fresh water 32,900 18,800
Baikal Russia fresh water 31,722 23,013
Great Bear Canada fresh water 31,153 2,236
Malawi Malawi-Mozambique-
fresh water 29,500 30,043
Great Slave Canada fresh water 27,200 1,580

[1] National Geographic. (n. d.). Lake.

[2] Lane, R. K. Lakes. (n. d.). Encyclopedia Britannica.

[3] USGS. (n. d.). Lakes and reservoirs.

[4] Dwyer, C. (n. d.). The 10 largest lakes of the world. When on Earth.


Aug. 8, 2016
Wikipedia precipitation
CC BY-SA 4.0

Precipitation refers to water released from clouds in the form of rain, freezing rain, sleet, snow or hail. It is the primary connection in the water cycle that provides for the delivery of atmospheric water to the Earth. Most precipitation falls as rain.[1]

Weather and humidity are related. Warm air can hold more water vapor than cool air. This means that if a parcelan air bubble that keeps its shape as it rises or sinks in the atmosphere of cool air and a parcel of warm air have the same amount of water vapor, the cool parcel has a higher relative humiditythe amount of water vapor present in air as a percentage of the amount needed for atmospheric saturation at the same temperature than the warm parcel.[10]

Upper atmosphere moisture cools quickly, forming large clouds that spread under low pressure conditions. Rapid upward air flow from Earth's surface creates low-pressure areas near the ground. Cool air fills the low pressure areas, producing precipitation.[11]

Clouds contain water vapor and cloud droplets, small drops of condensed water. The droplets are too small to fall as precipitation, but large enough to form visible clouds, which continuously evaporate and condense. Most of the condensed water doesn't fall as precipitation because the fall speed isn't high enough to overcome cloud updrafts.upward air movement[1]

The first stage in precipitation occurs when tiny water droplets adhere to condensation nuclei,tiny suspended particles, either solid or liquid, upon which water vapor condensation begins in the atmosphere which serve as the basis for raindrops.[1]

If the particles grow large enough, they produce raindrops with fall velocities which exceed cloud updraft speeds. Millions of tiny cloud droplets are needed to produce a single raindrop.[1]

Another more efficient mechanism is known as the Wegener-Bergeron-Findeisen process,a process of ice crystal growth that occurs in mixed phase clouds which leads to the rapid growth of ice crystals using water vapor in clouds. These crystals may fall as snow, or melt and fall as rain.[1]

Cloud chart
Cloud chart
National Oceanic and Atmospheric Administration
NWS Cloud Chart
public domain
Acid rain results when sulfur dioxidea colorless pungent toxic gas formed by burning sulfur in air and nitrogen oxidesa group of highly reactive gases, including nitrogen dioxide, nitrous acid and nitric acid in the atmosphere are transported by wind and air currents. These chemicals react with water to form sulfuric and nitric acids, which then fall as acid rain.[8]

SO2sulfur dioxide + OHhydroxideHOSO2hydroxysulfonyl radical

HOSO2hydroxysulfonyl radical + O2oxygenHO2water + SO3sulfur trioxide

SO3 (g)sulfur trioxide gas + H2O (l)waterH2SO4 (aq)sulfuric acid

NO2nitrogen dioxide + OHhydroxideHNO3nitric acid

Small amounts of sulfur dioxide and nitrogen oxides come from erupting volcanoes, but most is the result of burning fossil fuels by electric power generators, vehicles, manufacturing, oil refineries and other industries.[8]

Acid rain water leachesdrain away from soil, ash or other material by water aluminum from soil particles which flow into streams and lakes. Some plants and animals can tolerate acidic waters and moderate amounts of aluminum, but others can't live in low pHused to specify how acidic or alkaline a water-based solution is, acidic solutions have lower pH, and alkaline solutions have higher pH conditions. At pH 5 most fish eggs cannot hatch, frogs can't survive below pH 4 and the mayflies frogs eat don't survive below ph 5.5.[9]

Acid rain also kills trees, other plants and animals because it removes soil minerals and nutrients required for growth.[9]

At high elevations, acid foga thick cloud of tiny water droplets suspended in the atmosphere near Earth's surface and clouds remove nutrients from trees, leaving them with brown or dead leaves and needles. Unable to absorb sunlight, the trees are weakened and less able to withstand freezing temperatures.[9]

Melting snow and heavy rain can cause episodic acidification, creating short-term ecosystem stress.[9]

Acid rain causes coastal water nitrogen pollution, partially responsible for declining fish and shellfish populations.[9]

South Asia's monsoonsa seasonal change in prevailing wind direction that often results in weeks or months of rainy weather begin on India's west coast, with spring wind changes that push moist air from the Arabian Sea Arabian Sea
Arabian Sea
Oct. 12, 2012
Wikipedia Arabian Sea
public domain
toward land.[6]

Some farms experience temporary droughts, while others get too much rain, too quickly. In 2022, monsoon rains in Pakistan left much of the country underwater and killed more than 1,500 people. In India's technology capital, Bengaluru, September monsoon rains required workers to commute by boat.[6]

Right whales are threatened in part by ice melting where?
Climate change has made monsoons unpredictable for about 1.8 billion people, a quarter of Earth's population. Because warm air holds more moisture than cool air, atmospheric moisture collects in warm air, creating longer dry spells. When it rains the moisture falls in a short time in delugeswhen land is overflowed by significant precipitation amounting to normal weekly or monthly rains.[6]

To counteract the effects of climate change villagers dug long trenches by hand along hillsides to catch rain. The trenches prevent rain from running into streams. Instead, the water flows into local wells, providing a water supply after the monsoons have ended.[6]

In most years, Pacific winter storms deliver about 48 cubic miles of mountain snow, which remains frozen until the spring. During hot and dry months, melted snow flows into rivers, lakes, reservoirs and underground aquifers. Twenty-five million people depend on this water for irrigation, food and hydroelectric power.[7]

In 2015 California experienced a dry snow drought, when a high-pressure air mass called a ridiculously resilient ridgelarge high-pressure mass that remains over the U.S. West Coast for prolonged periods and that diverts storms winter storms, intensifying drough blocked winter snow storms, leaving only 25% of normal snowfall, and creating the state's worst recorded snow drought.[7]

Washington and Oregon experienced a wet snow drought. The Pacific Northwest had a relatively wet winter in 2015, but warm temperatures produced rain, rather than snow. Water that would have melted during the spring flowed directly into rivers, lakes and streams, and was no longer available during hot, dry months.[7]

Residents of Rolwaling, Nepal are threatened by floods caused by what?
Climate change and global warming are increasing both dry and wet snow droughts. In 2022 California and Oregon mountains had about half as much snow as is typical and Washington had about 75% of its normal snowfall.[7]

Fog is found in coastal zones around the planet. Its most noticeable human impact is on transportation, because shipping, road traffic and air travel and freight delays cost billions of dollars per year.[2]

But fog is also essential for plants and animals and agriculture and human health.

Along Chile's coast, cold ocean water rises to the surface carrying nutrients to wave tops where they form fog droplet nuclei that condense and then floats over land. Fog transports these nutrients from the ocean to the forests.[2]

Advection fog in San Francisco
Advection fog in San Francisco
B. Inaglory
Sep. 26, 2009
Wikipedia fog
CC BY-SA 3.0
Ocean bacteria, viruses and other organisms can be found in Italy's mountains. They have been transported by fog droplets from the sea onto land.[2]

Fog is the main source of moisture in the Namib Desert in Southwest Africa where it sustains vegetation providing metabolic fuel for 48 species, including the tenebrionid beetle Tenebrionid darkling beetle at Dar es Salaam, TanzaniaTenebrionid darkling beetle at Dar es Salaam, Tanzania
M. M. Karim
Jan. 1, 2009
Wikipedia darkling beetle
GNU Free Documentation License 1.2
that captures and drinks fog.[2]

Plant material and decomposition matter provide water best when they have been wet, which usually will be from fog[5]

While persistent fog can destroy food crops, it can benefit others, including artichoke and pumpkin fields in California's central coast, where fog creates the right light, temperature and moisture conditions for crop growth.[2]

America's most famous fog occurs in California, near the Golden Gate Bridge.[2] In June, July and August, most of the Northern Hemisphere, including California, endures high summer temperatures. But the average daily high in San Francisco is below 70oF (21oC), cooler than any major continental U.S. city.[3]

Anecdotal evidence from shoreline residents and scientists idicate that fog along that state's coast and the Santa Cruz region is diminishing. The reasons for the decline aren't clear, but climate change and increasing temperatures may explain why the fog, sustaining California's redwoods, is slowly disappearing. Redwoods and Torrey pines are showing signs of distress.[2]

One study demonstrated that fog has decreased about 30% in the past 60 years along the west coast. In the 1950s, coastal California got about 12 hours of fog per day during fog season. That has now been reduced to about 9 hours per day.[2]

Fog also reduces air temperature. One study that analyzed reduced fog showed a disproportionately high number of excessive heat deaths in coastal zones when fog is reduced. Those used to cooler temperatures because of fog may not know how to prepare themselves to deal with excess heat.[2]

Studies in Sao Paulo and Los Angeles demonstrate that human emissions produced fog near industrial centers. Pollution control efforts have reduced this reflective fog loaded with industrial pollution, which is more reflective than clean haze. The reduction of smog allows more warming, further diminishing fog.[2]

Icy fog, called pogonipa dense winter fog containing frozen particles that is formed in deep mountain valleys of the western U.S. by the Shoshone, forms in some high valleys of the Western U.S. This fog forms only in conditions cold enough to threaten respiratory health. Indigenous people and settlers recognized and feared this fog.[2]

Water harvested from fog is becoming increasingly important for people in arid, subtropical areas that are drying out with global warming.[2]

Fog collection in Alto Patache, Atacama Desert, Chile
Fog collection in Alto Patache, Atacama Desert, Chile
N. Saffie
Jul. 5, 2013
Wikipedia fog collection
CC BY-SA 2.0
As greenhouse gases trap more solar energy on the planet's surface, ocean currents are shifting poleward and the tropics and subtropics are expanding, The position and direction of winds that affect fog formation and persistence are changing, threatening fog-dependent ecosystems, including the biodiverse mountain forests of Mexico, Costa Rica and Hawaii.[2]

These forests and special plant communities might be the most vulnerable because rising temperatures could quickly push their fog belt upward, exposing sensitive cloud forests with many species that can only survive in fog zones.[2]

Fog nets can capture between 200 and 400 liters of fresh water per day, providing a reliable water source. More than 2,000 have been installed across Peru, Bolivia, Colombia and Mexico. Fog collected in the Peruvian provinces of Cusco, Tacna and Arequipa is clean, and the water it creates can be used by humans.[4]

In 2009, German conservationists planted she-oak trees in Peru to create a natural fog-catching system to replicate ancient water-capturing methods that collected water dripping from fog-covered plants. In Lima, Peru, one of the world's most polluted cities, fog nets pick up pollution. The condensed water can be used for crops and animals, but not for human consumption.[4]

In Morocco, lack of water has affected rural Amazigh communities, creating a daily burden for women, who spent more than three hours per day carrying water from communal wells to their homes. They now use fog nets. Similar fog harvesting successes have helped residents of Namibia, Bolivia and Chile.[4]

Water purification techniques may make polluted fog water fit to drink. Fog collection may provide reliable water for drought-stricken communities. But while new technologies are being brought to bear on the problem the basic techniques of fog catching go back centuries.[4]


Cloudy with a 20% chance of uncertainty
S. Kobilka
Aug. 8, 2022
Embedded video, no copy made
[1] USGS. (n. d.). Precipitation and the water cycle.

[2] Berwyn, B., Hasemyer, D., & Pickett, M. (Oct. 10, 2021). With a warming climate, coastal fog around the world is declining.

[3] Branch, J., Riggio, N., & Reinhard, S. (Sep. 14, 2022). The elusive future of San Francisco's fog. The New York TImes.

[4] Trevino, M. T. (Feb. 23, 2020). The etherial art of fog catching.

[5] Mitchell, D., et al. (Jan. 17, 2020). Fog and fauna of the Namib Desert: past and future. Ecosphere.

[6] Fountain, H. (Oct. 4, 2022). South Asia's monsoon is inextricably linked, culturally and economically, to much of Asia. Climate change is making it increasingly violent and erratic. The New York Times.

[7] Nichols, J. (Oct. 12, 2022). The problem with snow drought. Parched.

[8] Environmental Protection Agency. (Jun. 24, 2022). What is acid rain?

What is the weight of one gallon of water?
[9] Environmental Protection Agency. (Jun. 24, 2022). Effects of acid rain.

[10] National Oceanic and Atmospheric Administration. (n. d.). Discussion of humidity.,

[11] GoWeather. (Mar. 2, 2021). What is humidity and how does humidity affect weather.


Groundwater contamination by nitrates
Groundwater contamination by nitrates
Groundwater Quality
public domain
Falling rain and melting snow seep into Earth's cracks and crevices to form and recharge groundwater. The ground becomes saturated at the water table.the level below which the ground is saturated with water When that occurs, groundwater seepage can sometimes be seen when water-bearing layers emerge on the land surface in both rural and urban settings.[1]

Water in aquifersa body of permeable rock which can contain or transmit groundwater reaches the surface through springs, is discharged into lakes and streams, or extracted from man-made or artesian wells. In areas where material above the aquifer is permeable, pollutants can readily sink into groundwater supplies.[1]

Groundwater is used for drinking by more than 50% of the U.S. population, but the most substantial use of groundwater is crop irrigation.[1]

In some areas of the world people face serious water shortages because groundwater is used faster than it can be recharged. In other areas groundwater is polluted by human activities related to landfills, septic tanks,a tank used to hold domestic water wastes leaky underground gas tanks and from overuse of fertilizers and pesticides. If groundwater becomes polluted, it will no longer be safe to drink.[1]

Some of the substances introduced into groundwater include antimony,a lustrous gray metalloid, found in nature mainly as the sulfide mineral stibnite arsenic,a solid chemical element that is used especially in wood preservatives, alloys, and semiconductors and is extremely toxic in both pure and combined forms cadmium,a soft, malleable, bluish white metal found in zinc ores chromium,a blue-white metallic element found naturally only in combination and used especially in alloys and in electroplating copper,a highly conductive metallic chemical element that is easily formed into sheets and wires cyanide,a large group of poisonous chemical compounds used to make plastics and to extract and treat metals lead,a soft, dense, malleable metal with a relatively low melting point mercury,a silver-white poisonous heavy metallic element that is liquid at ordinary temperatures used in batteries, in dental amalgam, and in scientific instruments nitrate,usually combined with sodium or potassium and used as a fertilizer nitrite,a salt or ester of nitrous acid silver,a malleable, polishable, metallic chemical element, has the highest thermal and electric conductivity of any substance, used in jewelry, tableware, electronics, and as an antimicrobial and sulfatea salt of sulfuric acid, containing the anion SO from a variety of industrial processes. Others, including aluminum,a silver-white malleable, conductive, light metallic chemical element that resists weathering, and is the most common metal in Earth's crust barium,a silver-white metallic element used in drilling fluid and vacuum tubes, and as a contrast agent in medical imaging beryllium,a steel-gray, light, brittle chemical element that occurs naturally in beryl used as a hardening agent in alloys iron,a strong, hard magnetic silvery-gray metal used as a material for construction and manufacturing, especially in the form of steel manganese,a grayish-white, hard, brittle metallic element that resembles iron but is not magnetic and is used in alloys, batteries, and plant fertilizers nickel,a silver-white hard malleable, ductile, metallic element capable of a high polish and resistant to corrosion used in alloys and as a catalyst selenium,a photosensitive element that occurs in crystalline and amorphous forms, obtained as a by-product in copper refining, used in glass, semiconductor devices and alloys sodium,a silver-white, soft, waxy, ductile, chemically-active element that occurs abundantly in nature thalliuma soft poisonous metallic element that physically resembles lead, occurs sparsely in a number of common ores, used in the form of compounds especially in photosensitive devices and zinca bluish-white, ductile metallic element when pure and heated, brittle at ordinary temperatures, an essential micronutrient for both plants and animals, used especially in alloys and as a protective coating in galvanizing iron and steel occur naturally and mix with groundwater.[2]


[1] Groundwater Foundation. (2020). What is groundwater?

[2] USGS. Rivers, streams and creeks.

Weather Events

El Niño affects changes in phytoplankton
El Niño affects changes in phytoplankton
Jan. 1, 1998
Wikipedia El Niño
public domain
South American fishermen first noticed periods of unusually warm water in the Pacific Ocean in the 1600s, calling them El Niñothe cycle of warm and cold sea surface temperature of the tropical central and eastern Pacific Ocean accompanied by high air pressure in the western Pacific and low air pressure in the eastern Pacific de Navidad because these events peaked in December, when trade winds weaken and warm water is pushed eastward, toward the west coast of the Americas.[1]

El Niño has a significant affect on weather. The warmer waters cause the Pacific jet streama narrow band of strong westerly air currents that circles the Earth several miles above its surface to move southward, resulting in warmer and dryer areas in the northern U.S. and Canada. In the U.S. Gulf Coast and Southeast El Niño produces wetter weather and flooding.[1]

El Niño also affects Pacific coast marine life. During normal conditions, upwelling brings water from the deep ocean to the surface. This water provides a lot of nutrients but during El Niño upwelling weakens or stops, decreasing phytoplanktonplankton consisting of microscopic plants populations off the coast, affecting fish that serve as part of the food chain.[1]

El Niño is characterized by

El Niño and La Niña influence
El Niño and La Niña influence
National Oceanic and Atmospheric Administration
May 11, 2022
public domain
La Niñaan oceanic and atmospheric phenomenon that is the colder counterpart of El Niño is also sometimes called El Viejo, anti-El Niño, or simply "a cold event." La Niña has the opposite effect of El Niño. During La Niña events, trade winds are stronger than usual, pushing more warm water toward Asia. Off the west coast of the Americas, upwelling increases, bringing cold, nutrient-rich water to the surface.[1]

This cold water in the Pacific pushes the jet stream northward, leading to lead to drought in the southern U.S. and heavy rains and flooding in the Pacific Northwest and Canada.[1]

During a La Niña year, winter temperatures are warmer than normal in the South and cooler than normal in the North. La Niña can also lead to a more severe hurricane season.[1]

La Niña is characterized by

Over the last 50 years oceans have absorbed more than 90% of the heat generated by human-produced global warming. Rising sea level temperatures increase hurricane energy, slow atmospheric circulation, and cause hurricanes to move more slowly over land.[2]


[1] National Oceanic and Atmospheric Administration. (Oct. 5, 2017). What is eutrophication? National Ocean Service.

[2] Denchak, M. (Jun. 26, 2022). Hurricanes and climate change: Everything you need to know. NRDC.

[3] National Oceanic and Atmospheric Administration. (May 11, 2022). El Niño & La Niña (El Niño-Southern Oscillation).


Global drought frequency and duration increased by about a third since 2000. More than 2.3 billion people around the world are currently facing water stress.[1]

Where are ridiculously resilient ridges found?
A United Nations report concluded that from 1970 to 2019, weather, climate and water hazards accounted for 50% of disasters and 45% of disaster-related deaths, primarily in developing countries. Droughts only represent 15% of natural disasters killing 650,000 people in that time period.[2]

More than 10 million have died due to major drought events over the past 100 years. By 2050 drought could affect more than 75% of the world's population.[2] As many as 5.7 billion people could live in areas with water shortages for at least one month a year and more than 215 million people could be displaced from their homes.[1]

Drought and high temperatures created devastating 2020 bushfires in Tuggeranong, Australia
Drought and high temperatures created devastating
2020 bushfires in Tuggeranong, Australia
Nick D.
Jan. 29, 2020
Wikipedia drought
CC BY-SA 4.0
Drought inflicts severe burdens on women and girls in emerging and developing countries, affecting their education levels, nutrition, health, sanitation and safety. Almost 160 million children are exposed to severe and prolonged droughts. By 2040 one in four children will likely be living in areas with extreme water shortages.[3]

Women who carry out agricultural responsibilities are often not recognized as farmers. This limits their income and technology and ability to access sustainability practices.[4]

Some women have been successful. In India, women developed an underground rainwater catchment system. In Benin, West Africa, a solar power system irrigates fields so women don't have to collect and transport water from rivers and aquifers.[4]

Drought has been declared in parts of England. The first six months of 2022 were the driest since 1976. The National Drought Group estimates that by 2050 some rivers could have only 20% of their current water supplies. Temperatures could increase by 7Co due to climate change. (Degree changes are noted as Co or Fo while specific temperatures are noted as oC or oF.) In July 2022, U.K. temperatures were above 40oC for the first time.[1]

The Italian government declared a state of emergency in five regions in July 2022 because of a drought, the worst in 70 years. About a third of Italy's 17 million citizens live around the Po River, with more than half of the nation's pigs and cattle. The drought has threatened olive oil and risotto rice supplies, significantly raising their prices.[1]

France is experiencing its worst drought since in 1958, and is dealing with national water use restrictions. The country's corn harvest is expected to be 20% lower than in 2021.[1]

Portugal recorded its hottest July ever, with 99% of the country suffering severe or extreme drought. Average temperatures were just over 40oC, almost three degrees higher than the usual July average.[1]

The Netherlands is one of the world's flattest and most densely populated countries, and the world's second leadeing exporter of farm products. Climate change has produced hot, dry summers, reducing fresh water Alpine snowmelt that normally flows into the Rhine River. As less fresh water flows down the Rhine toward the North Sea, seawater moves landward, toward clean home and farm water supplies.[17]

In August 2022, the Rhine's flow was at a record low, forcing farmers in Enshede to illegally siphon water from ponds. As a result, city planners approved construction of ditches in grassy areas to catch rainwater. Concrete tiles and other paved surfaces were removed to expose water-absorbing soil and brooks and streams were reshaped reduce runoff.[17]

Some Dutch water boards have been helping growers dry out fields since the Middle Ages. Now they are assisting farmers in keeping their land wet by using efficient drip irrigation.[17]

Around 75% of Romania is affected by drought. The country's cereal crop is expected to decrease by 30 million metric tons.[1]

Climate change and drought foring hard choices across California
May 9, 2022
Embedded video, no copy made
Drought has devastating effects on ecosystems But there are solutions


A dry lakebed in California in its worst megadrought in 1,200 years
A dry lakebed in California in its
worst megadrought in 1,200 years
Mar. 15, 2009
Wikipedia climate change in the U.S.
public domain
[1] World Economic Forum. (Aug. 12, 2022). Droughts are getting worse around the world, here's why and what needs to be done.

[2] United Nations. (May 12, 2022). World 'at a crossroads' as droughts increase nearly a third in a generation.

[3] Algur, K. D., Patel, S. K., & Chauhan, S. (2021). The impact of drought on the health and livelihoods of women and children in India: A systematic review. Children and Youth Services Review, Elsevier, 122(C).

[4] Schonhardt, S. (May 10, 2022). Scientific American.

[5] King-Okumu, C., et al. (2019). How can we stop the slow-burning systemic fuse of loss and damage due to land degradation and drought in Africa? Current Opinion in Environmental Sustainability, 50, pp. 289-302.

[6] WRI. (2017). Can we restore 350 million hectares by 2030?

[7] Vizcarra, N. (Sep. 10, 2020). Africa's great green wall is officially 4% - and unofficially 18% - complete. Global Landscapes Forum: Landscape News.

[8] Quesnel, K. J., & Ajami, N. K. (Oct. 25, 2017). ScienceAdvances.

[9] Hoegh-Guldberg, O., et al. (2018). Impacts of 1.5oC global warming on natural and human systems. In V. Masson-Delmotte, et a., (Eds.), Global warming of 1.5oC: An IPCC special report on the impacts of global warming of 1.5oC above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change. World Meteorological Organization Technical Document.

[10] Tsegai, D. & Brüntrup, M. (2019). Drought challenges and policy options: lessons drawn, and the way forward. Current Directions in Water Scarcity Research, 2, pp. 325-336. Elsevier.

[11] FAO & NEPAD. (Sep. 29, 2021). Review of forest and landscape restoration in Africa 2021. ReliefWeb.

What form of water is captured in large nets in dry climates?
[12] Stocker, B. D. et al. (Mar. 11, 2019). Drought impacts on terrestrial primary production underestimated by satellite monitoring. Nature Geoscience, 12(4), pp. 264-270.

[13] Nath, S., Shyanti, R. K., & Nath, Y. (2021). Influence of anthropocene climate change on biodiversity loss in different ecosystems. Global Climate Change, pp. 63-78. Elsevier.

[14] Peace, N. (Mar. 11, 2020). Impact of climate change on insect, pest, disease, and animal biodiversity. International Journal Environmental Science & Natural Resources Review article, 23(5).

[15] Wintle, B. A., Legge, S., & Woinarski, J. C. (2020). After the megafires: What next for Australian wildlife? Trends in Ecology & Evolution, 35(9), pp. 753-757.

[16] Brando, P.M., et al. (2020). The gathering firestorm in southern Amazonia. Science Advances, 6(2).

What four elements are involved in acid rain production?
[17] Zhong, R. (Oct. 18, 2022). They're 'world champions' of banishing water. Now, the Dutch need to keep it. The New York Times.


Flooded New Orleans after hurricane Katrina
Flooded New Orleans after hurricane Katrina
Sep. 11, 2005
Wikipedia flood
public domain
Humans continue to burn fossil fuels, increasing atmospheric greenhouse gases and atmospheric temperatures. Hot air holds more water vapor, causing an increase in rainstorm intensity.[1]

According to the National Climate Assessment, rain intensity increased significantly between 1958 and 2016. For each Celsius degree increase in Earth's temperature, the amount of atmospheric water vapor increases by around 7%.[1]

Floods occur when a lot of rain falls quickly and cannot soak into the ground because of saturation or impermeability.not allowing liquid or gas to go through Water pools on land surfaces or flows downhill, creating destructive and often deadly flash floods.[1]

Floods alter landscapes, erode riverbanks, increase sedimentation, clog rivers, displace and smother fish and other aquatic life when their habitats are washed away.[3]

Floodwater can be contaminated with agricultural pesticides, industrial chemicals, debris and sewage. Floods are the primary cause of weather-related infectious disease outbreaks, increasing the chance of spreading waterborne diseases including hepatitis Aa highly contagious liver infection caused by the hepatitis A virus and intestinal infection caused by Vibrio cholerae bacteria[3]

Receding floodwater creates stagnant water pools leaving a breeding ground for mosquitoes, which can transmit malaria.a serious and sometimes fatal disease caused by a mosquito parasite Flood events also lead to an increase in some forms of zoonosisa disease which can be transmitted to humans from animals, such as leptospirosisan infectious bacterial disease that occurs in rodents, dogs, and other mammals and can be transmitted to humans.[3]

Researchers calculated that floods also affect the U.S. housing market. They found that residential properties at risk of flooding were overvalued by between $121 billion and $127 billion. Most were found in coastal counties with no flood risk disclosure laws, in those where there was little concern about climate change, in low-income communities and in cities and towns highly dependent on property taxes.[4]

SeaWiFS satellite image of Okawango Delta, with national borders added
SeaWiFS satellite image of Okawango Delta,
with national borders added
NASA/Goddard Spaceflight Center
Mar. 28, 1999
Wikipedia Okavango Delta
public domain
The effects of seasonal floods isn't always negative. Floods transport nutrients, including nitrogen, phosphorus and organic material. When water recedes, the nutrients remain as natural fertilizer improving soil quality and increasing plant growth productivity. Ancient civilizations rose near productive, seasonally-flooded rivers such as the Nile.[3]

Floods replenish underground water sources. Floodwater is absorbed by the ground, percolating through soil and rock, reaching underground aquifers, which supply clean fresh water to springs, wells, lakes and rivers.[3]

Small seasonal floods help native fish outcompete invasive species. Sediment deposited during floods serves as fish nurseries for small fish, and the nutrients they bring support aquatic food webs by boosting productivity.[3]

Approximately 40% of world species rely on wetlands, which filter water, mitigate flooding and act as carbon sinks. The Okavango Delta in Botswana is a UNESCO World Heritage Site and one of the world's largest, most important wetland habitats. The river captures rainfall from the Angolan highlands, causing flooding that replenishes wetlands during the dry season, providing a Kalahari Desert oasis.[3]

Floods can trigger breeding events and migration. In 2016, thousands of water birds flocked to the Macquarie Marshes in New South Wales, Australia. Flooding had filled their wetland habitat for the first time in years, triggering a mass breeding event.[3]

In Cambodia, monsoon rains cause the annual Mekong River flood pulse migration. The floodwaters caused the Tonle Sap river, connecting to the Mekong River to Tonle Sap lake, to reverse its flow. Floodwater entering the lake starts fish migrations, supporting one of the world's most productive fisheries.[3]

The Macquarie marshes are an important area for white-necked herons
The Macquarie marshes are an important area
for white-necked herons
G. Fergus
Jul. 14, 2006
Wikipedia Macquarie Marshes
CC BY-SA 2.5
River floods occur when a river or stream overflows its banks onto normally dry land. This type of flood is most common in late winter and early spring as the result of heavy rainfall, rapid snow melt or ice jams. Approximately 41 million U.S. residents are at risk from flooding along rivers and streams.[2]

Coastal flooding results from coastal storms, including hurricanes or nor'eastersa storm that travels along the Eastern Seaboard and brings winds from the northeast that create destructive storm surges, walls of water moving from ocean onto land.[2]

Higher sea level produces shallow floods known as nuisance or sunny day floods. These floods wash over roads and into storm drains during high tide.[2]

Urban flooding refers to flooding that occurs when rainfall, rather than a body of water, exceeds stormwater drain capacity, usually in densely populated areas.[2]

Because the National Weather Service issues flood watches and warnings, local weather services can notify citizens and the media.[1]

Flooding can be mitigated by undeveloped land areas, forests, wetlands and retention ponds.[1]


[1] Hersher, R. (Aug. 3, 2022). How climate change drives inland floods. NPR.

[2] Denchak, M. (Apr. 10, 2019). Flooding and climate change: Everything you need to know. NRDC.

[3] National Geographic. (2022). The many effects of flooding.

[4] Gourevitch, J. D., et al. (Feb. 16, 2023). Unpriced climate risk and the potential consequences of overvaluation in US housing markets. Nature.


Boulton, C.A., Lenton, T.M., & Boers, N. (2022). Pronounced loss of Amazon rainforest resilience since the early 2000s. Nature Climate Change, 12, 271-278."

Tonlé Sap lake, river and drainage basin in Cambodia
Tonlé Sap lake, river
and drainage basin in Cambodia
Oct. 2, 2006
Wikipedia Macquarie Marshes
CC BY-SA 2.5
Chea, T., Berger, N., & Edelson, J. (Apr. 6, 2023). Dramatic photos show how storms filled California reservoirs. AP News.

Colorado River District. (2020). Acronyms.

Colorado River District. (2020). Glossary.

Colorado River District. (2020). Webinars.

Environmental Protection Agency. (Apr. 4, 2023). Annual allotment of federal funds for states, tribes, and territories.,national%20

Environmental Protection Agency. (Feb. 18, 2022). Drinking water rule quick reference guides.

Environmental Protection Agency. (Feb. 18, 2022). Regulatory and guidance information by topic: Water.

Environmental Protection Agency. (Feb. 23, 2016). Water trivia facts.

What is the smallest ocean?
Floodbase. (2023). Global flood database.

Hillhouse, G. (May 3, 2022). How wells and aquifers actually work. Practical Engineering.

Hillhouse, G. (Apr. 5, 2022). What sewage treatment and brewing have in common. Practical Engineering.

Horne, C. et al. (2017). Water for the environment. Elsevier Press. (2020). Marine life.

When was the International Geophysical Year?
Miller, C. (Nov. 28, 2022). Water as part of the climate solution. Inside Climate News.

NASA. (Aug. 28, 2015). NASA's earth minute: Greenland ice.

Newburger, E. (Dec. 30, 2022). EPA issues clean water rule that repeals Trump administration changes. CNBC.

NPR. (Apr. 19, 2023). How melting ice due to climate change is having far reaching effects.

Rivers, Streams and Creeks
public domain
Rayne, E. (Dec. 20, 2022). Megadrought on Earth affected gravity waves at the edge of space.

Richtel, M. (Jan. 18, 2023). Bomb cyclone? Or just windy with a chance of hyperbole? The New York Times.

Seametrics. (2018). 100 amazing water facts you should know.

Singh, P. (Feb. 2, 2023). Relative humidity calculator.

Smithsonian Institution. (Apr. 2018). The census of marine life.

World`s most important water use?
Tollefson, J. (Dec. 16, 2022). Billion-dollar NASA satellite launches to track Earth's water. Nature.

UCI News. (Feb, 23, 2023). UC Irvine researchers create e. coli-based water monitoring technology.

Utah Division of Water Rights. (n. d.). Glossary of water words.

What is the major source of acid rain?
Utah Geological Survey. (n. d.). Groundwater resources/hydrology publications.

Utah State University. (n. d.). Utah water research laboratory. (n. d.). Safe water protects and saves lives.

Water Project. (Aug. 31, 2016). Facts about water: Statistics of the water crisis.

Water covers what percent of Earth`s surface?
WaterUseItWisely. (2020).

Wikipedia. (Oct. 16, 2020). Water.

Denise Meeks,