term paper on water cycle

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The Water Cycle, Essay Example

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Water is an important element for the survival of living things.  The hydrologic cycle refers to the precipitation and evaporation of water from the atmosphere and back to the earth. Water on earth is mostly found in the ocean, which covers over 70% of the earth’s surface and is the source for the major reservoir.  In fact, the oceans contain about 97% of the earth’s available water. The hydrologic cycle is driven through solar energy, which causes the water to evaporate into the atmosphere and return to the earth’s surface in the form of precipitation via gravity. Water that falls onto the land can be absorbed through living organisms, such as plants.  Water molecules taken up by plants are returned to the atmosphere in form of evaporation from leaves. Other water molecules are absorbed into the water and undergo photosynthesis through combining with carbon dioxide resulting in high energy molecules referred to as glucose. These glucose molecules are then further broken down during cellular respiration of living organisms into water and carbon dioxide and released back into the atmosphere.

The patterns of both precipitation and evaporation result in the distribution of plants on the earth’s surface.  For instance, this change in hydrologic cycle can be observed in different types of habitats, such as the desert or rain forest.  In deserts, there is a decrease observed in living communities due to the decrease in biological productivity from the lack of water. On the other hand in rain forests, there is an abundance of water resulting in an increased biological productivity.  In these habitats, therefore, different types of plant species and abundance occur. Changes in the hydrologic cycle could results in changes of plant communities in these areas, which thereby effect the distribution of plants on earth.

Living organisms in an ecosystem require both energy and nutrients in order to maintain life activities essential to living organisms, such as growth, development and reproductions. Plants are key to the cycle of energy and nutrients within an ecosystem.  The plants capture sunlight and convert the sunlight into chemical energy through the process of photosynthesis. The energy captured through the plants is transferred through the food chain starting with the herbivores. The herbivores eat plants and obtain energy.  Carnivore animals eat the herbivores to obtain energy. Scavengers obtain energy from left over animal remains.  Finally, decomposers obtain energy through decaying material. Sunlight provides the energy that powers life. Nutrients and C N P H20 enter the ecosystem via the non-living components of the planet, such as the atmosphere, earth, or ocean.  Solar energy continually bombards the earth and provides a limitless source of energy.  This flow of energy is limitless since the energy provided from the sun is limitless.  However, the nutrients essential for living organisms is limited.  For instance, the earth only contains a certain amount of available Carbon, Phosphorus, or Nitrogen. The process of photosynthesis provides 1/7 th of the available carbon. Therefore, if cellular respiration were to discontinue and carbon dioxide was not released into the atmosphere, energy for life would also discontinue, as the availability of Carbon would decrease or end for the uptake of plants.  Therefore, the flow of energy and the cycling of nutrients play major roles in the populations within an ecosystem.

The differences in ecosystems depend of two different types of factors. These are abiotic and biotic factors.  The abiotic factors refer to components such as non-living things such as water and light.  The biotic factors are the living community of organisms. Different habitats are comprised of different abiotic and biotic factors.  In a swamp, the most important abiotic factor is water. The water in a swamp has a huge biotic community for micro biotic organisms, such as animal and plant-like protists, fish, plants, insects, amphibians, and reptiles.  Birds and mammals also utilize the swamps as well. All of the biotic community comprises the biotic factors.

Matter and energy flow through an ecosystem when organisms feed on one another, making up the food chain. Food producers are the first chain, such as plants and algae that capture sunlight and convert chemical energy to food via photosynthesis. After the food producers, are the consumers. Consumers consume food producers; therefore, they eat the plant material. Next are the second order consumers, third order consumers and decomposers.

Pyramids were developed to illustrate the energy flow through an ecosystem with the producers on the bottom, consumers, 2 nd order consumers, and third order consumers at the top. This pyramid showed that 16% of the energy is passed on to the consumers, 11% to the secondary consumers, and only 5% to the third order consumers.

The Carbon cycle moves through ecosystems starting with air, since it contains carbon dioxide.  Plants absorb carbon dioxide and break it down to glucose and oxygen. Carbon dioxide also diffuses into water for aquatic plants.  Some of the Carbon atoms are used to build body tissue and other molecules are returned back to the atmosphere. Carbon is also released back to the environment through the burning of wood or fossil fuels. Decomposers also return Carbon to the atmosphere as well. All of these components affect the carbon cycle.

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water cycle

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• NASA - Global Precipitation Measurement - The Water Cycle
• U.S. Geological Survey - The Water Cycle
• Chemistry Libretexts - Water Cycle
• Northwest River Forecast Center - The Water Cycle
• NeoK12 - Educational Videos and Games for School Kids - Water Cycle
• Pennsylvania State University - Department of Energy and Mineral Engineering - Understanding water cycle
• UCAR Center for Science Education - The Water Cycle
• water cycle - Children's Encyclopedia (Ages 8-11)
• water cycle - Student Encyclopedia (Ages 11 and up)

water cycle , cycle that involves the continuous circulation of water in the Earth - atmosphere system. Of the many processes involved in the water cycle, the most important are evaporation , transpiration , condensation , precipitation , and runoff . Although the total amount of water within the cycle remains essentially constant, its distribution among the various processes is continually changing.

A brief treatment of the water cycle follows. For full treatment, see hydrosphere: The water cycle .

Evaporation , one of the major processes in the cycle, is the transfer of water from the surface of the Earth to the atmosphere. By evaporation, water in the liquid state is transferred to the gaseous , or vapor, state. This transfer occurs when some molecules in a water mass have attained sufficient kinetic energy to eject themselves from the water surface. The main factors affecting evaporation are temperature , humidity , wind speed, and solar radiation . The direct measurement of evaporation, though desirable, is difficult and possible only at point locations. The principal source of water vapor is the oceans , but evaporation also occurs in soils , snow , and ice . Evaporation from snow and ice, the direct conversion from solid to vapor, is known as sublimation. Transpiration is the evaporation of water through minute pores, or stomata, in the leaves of plants . For practical purposes, transpiration and the evaporation from all water, soils, snow, ice, vegetation, and other surfaces are lumped together and called evapotranspiration , or total evaporation.

Water vapor is the primary form of atmospheric moisture. Although its storage in the atmosphere is comparatively small, water vapor is extremely important in forming the moisture supply for dew , frost , fog , clouds , and precipitation. Practically all water vapour in the atmosphere is confined to the troposphere (the region below 6 to 8 miles [10 to 13 km] altitude).

The transition process from the vapor state to the liquid state is called condensation . Condensation may take place as soon as the air contains more water vapour than it can receive from a free water surface through evaporation at the prevailing temperature. This condition occurs as the consequence of either cooling or the mixing of air masses of different temperatures. By condensation, water vapor in the atmosphere is released to form precipitation .

Precipitation that falls to the Earth is distributed in four main ways: some is returned to the atmosphere by evaporation, some may be intercepted by vegetation and then evaporated from the surface of leaves , some percolates into the soil by infiltration, and the remainder flows directly as surface runoff into the sea. Some of the infiltrated precipitation may later percolate into streams as groundwater runoff. Direct measurement of runoff is made by stream gauges and plotted against time on hydrographs.

Most groundwater is derived from precipitation that has percolated through the soil. Groundwater flow rates, compared with those of surface water, are very slow and variable, ranging from a few millimeters to a few meters a day. Groundwater movement is studied by tracer techniques and remote sensing.

Ice also plays a role in the water cycle. Ice and snow on the Earth’s surface occur in various forms such as frost, sea ice , and glacier ice. When soil moisture freezes, ice also occurs beneath the Earth’s surface, forming permafrost in tundra climates . About 18,000 years ago glaciers and ice caps covered approximately one-third of the Earth’s land surface. Today about 12 percent of the land surface remains covered by ice masses.

Geography Notes

Water cycle: term paper on water cycle | atmosphere | geography.

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After reading this term paper you will learn about the composition of water cycle present in the atmosphere.

The water cycle is a process where water evaporates from the sea, condenses as clouds, falls as rain and flows into the seas and oceans through rivers and streams and again evaporates due to heat in the air.

i. When rain falls on the ground, some water percolates into the soil and adds to the underground water table. This water from the soil is later used by plants and animals which is released back into the atmosphere either in the form of vapor or liquid.

ii. When water flows through the rocks, it dissolves the deposited soluble minerals. Thus, rivers carry more minerals from the land to the sea which are used by the marine organisms.

iii. When the snow on the ice caps of the mountains melts, the water flows down into the streams and rivers, and thus enter the water cycle.

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Term Paper , Geography , Atmosphere , Water Cycle , Term Paper on Water Cycle

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The Process of the Water Cycle Research Paper

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Introduction

Water cycle process, works cited.

Nature comprises many processes that recycle various elements to avoid human wastage. Nature does not waste any of its elements and recycles them all including water, air and organic fertility. Recycling of natural elements occurs in order to maintain ecological balance for survival of all living species.

However, human beings have meddled with nature so much that problems such as depletion of ozone layer and global warming are inflicting the human race adversely (Kalman and Sjonger 11). An example of a process in which nature recycles one of its constituent elements is the water cycle. By definition, the water cycle is a continuous movement of water between the earth surface and the atmosphere (Kalman and Sjonger 11).

The water moves from water bodies such as oceans and rivers into the atmosphere and vice versa. It involves several states of matter including solid, gas and liquid in which water changes its form in an unending cycle of precipitation (Kalman and Sjonger 2). The cycle involves several steps that include evaporation, precipitation, run-off and percolation. Each of these steps plays a role in continuing the water cycle.

The water cycle is important in maintaining the right amount of water in nature. In addition, it facilitates the storage of underground water that is used when there is no precipitation (Olien 8). There are several steps involved in the water cycle.

They include evaporation, condensation, precipitation, infiltration, sub-surface flow and run-off (Olien 8). In all these steps, water is converted into different states of matter including liquid, gas and solid. Heat exchange is one of the processes that are involved in all the steps. In each of these steps, heat is either lost or gained.

Evaporation

This is the process by which water changes from liquid form to gaseous form (Olien 9). It is the primary process that drives the movement of water from water bodies into the atmosphere in form of water vapor. The main water bodies include oceans, sea, lakes, rivers, dams, streams and ponds.

They provide approximately 90% of the vapor in the atmosphere. The other 10% comes from plants through the process of transpiration (Olien 9). Evaporation takes place when heat from solar energy heats up water in water bodies and causes it to change from liquid to gas. On the other hand, evapotranspiration is the process of water release from the surface of plants and soil due to evaporation (Olien 10).

Transpiration contributes a very low percentage of water vapor in the water cycle. Evaporation is the main process that drives the water cycle. Afterwards, the water vapor rises to the atmosphere and the next step of condensation begins. Research has established that after water molecules rises into the atmosphere, they spend approximately 10 days before being released as precipitation.

Condensation

This is the process by which water vapor changes from vapor into liquid, and is the reverse process of evaporation (Olien 11). Condensation plays a significant part in the water cycle because it results in the formation of clouds. After clouds are formed, they possess the ability to produce precipitation.

Precipitation is the main route through which water returns to the earth surface after the process of evaporation (Olien 11). In times when clouds are not visible, water is still present but in the form of vapor and small water droplets.

Clouds are formed from the combination of these water droplets with atmospheric elements such as dust, smoke and salt. They form tiny cloud droplets that enlarge into clouds as more droplets combine with atmospheric elements. Cloud droplets have different sizes that range from 10 microns to 5 millimeter (Olien 12).

This process takes place in the higher parts of the atmosphere because the weather conditions found there encourage condensation. This is because temperatures are cooler than the lower parts of the atmosphere. As water droplets coalesce, clouds and precipitation may form at the same time. Precipitation refers to clouds in either liquid or solid form falling to the surface of the earth from the clouds (Olien 13).

Precipitation

Precipitation refers to the process by which water is discharged from the atmosphere in a liquid or solid form into the surface of the earth, be it land or water surface (Kalman and Sjonger 16). Precipitation is released from the atmosphere in many forms that include snow, hail, freezing rain, sleet or rain.

It is the main channel that returns water into the surface of the earth. In most cases, precipitation is released as rain. Some precipitation is released from the atmosphere in form of snow, which accumulates in certain places on the ground to form glaciers and icecaps. When temperatures rise during spring, they melt and the water flows back into water bodies.

These structures store water for long periods. Clouds comprise water vapor, which accumulates over a long period to form precipitation (Kalman and Sjonger 16). Precipitation happens when these droplets gain a fall velocity that is greater than the cloud updraft speed. This takes a long time because a single raindrop is made by a combination of millions of tiny cloud droplets.

Surface run-off

This is the runoff of precipitation on the surface of the earth (Kalman and Sjonger 18). When rain hits an impervious surface on the ground, it flows over the surface. This water then flows back into water bodies and evaporates to continue the cycle. It flows into lakes, rivers and streams, from which t floes into the oceans.

Approximately, a complete water cycle takes 9 days. During runoff, water may infiltrate the ground, evaporate or flow back into water bodies. Only about 30% of precipitation that falls from the atmosphere flows back into the oceans. The other 70% evaporates, infiltrates the ground or is transpired (Olien 20). Human beings can also divert surface runoff to desired places for use in agriculture.

Infiltration

This refers to the process of water movement from the earth surface into the ground. A small portion of infiltrated water is held by the shallow soil layer from which it flows horizontally and vertically through the soil layer into the atmosphere (Olien 21). Some water seeps through the ground surface and flows into streams while the rest infiltrates further into the ground and replenishes the ground-water aquifers.

If these aquifers are porous, then people can drill water holes into the aquifers to draw water for domestic and agricultural uses (Kalman and Sjonger 23). Water that infiltrates into the ground stays there for some time before seeping into streams or moving vertically to the surface from where it evaporates.

Ground water storage and discharge

Some water infiltrates into the deep regions of the earth surface and is stored there for long periods. Despite being trapped in the depths of the earth, the water moves slowly since it is part of the water cycle. Ground water is stored in structures known as aquifers. To participate effectively in the water cycle, ground water seeps through the ground and enters the main water bodies by horizontal movement.

The structure of quifers and confining soil and rock layers are the main factors that determine the speed of groundwater movement. In addition, the movement of the water depends on the permeability and porosity of the soil constituents that hold the water. Because of gravity, groundwater moves further downwards into the ground surface and may never move back to the water cycle. It remains trapped in the ground for thousands of years.

Nature comprises many processes that recycle various elements for reuse. Nature has no wastage and recycles all elements including water, air and organic fertility. An example of a process in which nature recycles one of its constituent element is the water cycle. By definition, water cycle is a continuous movement of water between the earth surface and the atmosphere.

The water moves from water bodies found on the surface of the earth to the atmosphere and vice versa. Steps involved in the water cycle include evaporation, condensation, precipitation, infiltration, sub-surface flow and run-off. In all these steps, water is converted into different states of matter including liquid, gas and solid. Water evaporates from the surface of the earth, moves into the atmosphere as vapor and condenses to form clouds.

These clouds fall back to the earth surface as precipitation in form of rain, sleet or snow. Some water seeps through the ground surface and flows into streams while the rest infiltrates further into the ground and replenishes the ground-water aquifers. It stays there for some time before seeping into streams or moving vertically to the surface from where it evaporates.

The water cycle is important in maintaining the right amount of water in nature. In addition, it facilitates the storage of underground water that is used when there is no precipitation or during droughts. Some water infiltrates into the deep regions of the earth surface and is stored there for long periods. Despite being trapped in the depths of the earth, the water moves slowly since it is part of the water cycle.

Kalman, Bobbie and Sjonger, Rebecca. The Water Cycle . New York: Crabtree Publishing Company, 2006. Print.

Olien, Rebecca. The Water Cycle . New York: Capstone, 2005. Print.

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What Is the Water Cycle?

Water can be found all over Earth in the ocean, on land and in the atmosphere. The water cycle is the path that all water follows as it moves around our planet.

Credit: NASA/JPL-Caltech Data source: NASA's Earth Observatory

On Earth, you can find water in all three states of matter: solid , liquid and gas . Liquid water is found in Earth’s oceans, rivers, lakes, streams—and even in the soil and underground. Solid ice is found in glaciers , snow, and at the North and South Poles . Water vapor—a gas—is found in Earth’s atmosphere.

How does water travel from a glacier to the ocean to a cloud? That’s where the water cycle comes in.

The Water Cycle

Credit: NASA/JPL-Caltech

The Sun’s heat causes glaciers and snow to melt into liquid water. This water goes into oceans, lakes and streams. Water from melting snow and ice also goes into the soil. There, it supplies water for plants and the groundwater that we drink.

Snow falling on a glacier during winter months usually replaces any water that melts away in the summer. However, due to Earth’s overall warming , most glaciers today are losing more ice than they regain, causing them to shrink over time.

How does water get into the atmosphere? There are two main ways this happens:

• Heat from the Sun causes water to evaporate from oceans, lakes and streams. Evaporation occurs when liquid water on Earth’s surface turns into water vapor in our atmosphere.
• Water from plants and trees also enters the atmosphere. This is called transpiration .

Warm water vapor rises up through Earth’s atmosphere. As the water vapor rises higher and higher, the cool air of the atmosphere causes the water vapor to turn back into liquid water, creating clouds. This process is called condensation .

When a cloud becomes full of liquid water, it falls from the sky as rain or snow—also known as precipitation . Rain and snow then fill lakes and streams, and the process starts all over again.

Clouds, like these over the savannah in Nairobi, Kenya, form when water vapor in the atmosphere condenses back into liquid water. Credit: Department of State

Why Do We Care About the Water Cycle?

We care about the water cycle because water is necessary for all living things. NASA satellites orbiting Earth right now are helping us to understand what is happening with water on our planet.

Water in the Soil

Humans need water to drink, and to water the plants that grow our food. NASA has a satellite called SMAP —short for Soil Moisture Active Passive —that measures how much water is in the top 2 inches (5 cm) of Earth’s soil . This can help us understand the relationship between water in the soil and severe weather conditions, such as droughts.

Water in the Atmosphere

NASA’s CloudSat mission studies water in our atmosphere in the form of clouds. CloudSat gathers information about clouds and how they play a role in Earth’s climate. Also, the international satellite called the Global Precipitation Measurement Mission (GPM) observes when, where and how much it rains and snows on Earth.

Water in the Oceans

As Earth’s climate becomes warmer, land ice at the North and South Poles starts melting. The water then flows into the ocean, causing sea level to rise. NASA’s Jason-3 mission—short for Joint Altimetry Satellite Oceanography Network-3 —orbits Earth collecting information about sea level and ocean temperature. This helps track how the ocean responds to Earth’s changing climate.

NASA is also tracking how Earth’s water moves all around our planet. This is the work of the GRACE-FO —or Gravity Recovery and Climate Experiment-Follow On —mission. It tracks the movement of water from one month to the next, and can even measure changes in deep groundwater hundreds of feet below Earth’s surface.

NASA’s Aqua satellite also collects a large amount of information about Earth’s water cycle, including water in the oceans, clouds, sea ice, land ice and snow cover.

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Water Cycle

What is the water cycle.

Water cycle, also known as the hydrologic cycle, involves a series of stages that show the continuous movement and interchange of water between its three phases – solid, liquid, and gas, in the earth’s atmosphere. The sun acts as the primary source of energy that powers   the   water cycle on earth. Bernard Palissy discovered the modern theory of the water cycle in 1580 CE.

Steps of the Water Cycle: How does it Work

1. Change from Liquid to Gaseous Phase – Evaporation and Transpiration

The heat of the sun causes water from the surface of water bodies such as oceans, streams, and lakes to evaporate into water vapor in the atmosphere. Plants also contribute to the water cycle when water gets evaporated from the aerial parts of the plant , such as leaves and stems by the process of transpiration.

2. Change from Solid to Gaseous Phase – Sublimation

Due to dry winds, low humidity, and low air pressure, snow present on the mountains change directly into water vapor, bypassing the liquid phase by a process known as sublimation.

3. Change from Gaseous to Liquid Phase – Condensation

The invisible water vapor formed through evaporation, transpiration, and sublimation rises through the atmosphere, while cool air rushes to take its place. This is the process of condensation that allows water vapor to transform back into liquid, which is then stored in the form of clouds.

Sometimes, a sudden drop in atmospheric temperature helps the water vapors to condense into tiny droplets of water that remain suspended in the air. These suspended water droplets get mixed with bits of dust in the air, resulting in fog.

4. Change from Gaseous to Liquid and Solid Phase – Precipitation and Deposition         

Wind movements cause the water-laden clouds   to collide and fall back on the earth’s surface through precipitation, simply known as rain. The water that evaporated in the first stage thus returns into different water bodies on the earth’s surface, including the ocean, rivers, ponds, and lakes. In regions with extremely cold climate with sub-zero temperatures, the water vapor changes directly into frost and snow bypassing the liquid phase, causing snowfall in high altitudes by a process known as the deposition. 

5. Return of the water back into the underground reserve – Runoff, Infiltration, Percolation, and Collection

The water that falls back on the earth’s surface moves between the layers of soil and rocks and is accumulated as the underground water reserves known as aquifers. This process is further assisted by earthquakes, which help the underground water to reach the mantle of the earth. Some amount of precipitated water flows down the sides of mountains and hills to reach the water bodies, which again evaporates into the atmosphere. During volcanic eruptions, the underground water returns to the surface of the earth, where it mixes with the surface water bodies in order to continue the cycle.

Video: Water Cycle Explained

Why is the water cycle important.

The most crucial and direct impacts of the above process on earth include:

• Making fresh water available to plants and animals, including humans, by purifying the groundwater on earth. During the water cycle, the water evaporates, leaving behind all the sediments and other dust particles. Similarly, for the sustenance of marine life, the saline range of all salt water bodies is kept within a certain permissible limit through infiltration. 
• Allowing even distribution of water on all surfaces of the earth. Water is temporarily stored as clouds in the atmosphere, whereas surface water bodies such as rivers and oceans, together with underground water, form the major permanent water reserves. 
• Causing a cooling effect on earth due to evaporation of water from surface water bodies, which help to form clouds that eventually precipitate down in the form of rain. This way water cycle affects the weather and climate of the earth.
• Ensuring some other biogeochemical cycles , including those concerning oxygen and phosphorus, to continue in nature.
• Cleaning the atmosphere by taking-away dust particles, shoot, and bacteria , thus acting as a means to purify the air we breathe.

Human Impact on Water Cycle

Human activities adversely affect the water cycle in the two following ways:

a) Deforestation : Plants play an important role in the water cycle by preventing soil erosion and thus helps to increase the groundwater level of the earth. Also, plants contribute by absorbing water from the soil, which is then released back to the atmosphere during transpiration. Deforestation adversely affects both the above processes, thus breaking the flow of the water cycle.

b) Pollution : Burning of fossil fuels acts as the major source of air pollution releasing toxic gases into the atmosphere, leading to the formation of smog and acid rain . Water from farmlands run off to the nearest water bodies carrying chemicals such as insecticides and pesticides along with them, thus causing water pollution. The presence of excessive contaminants in the atmosphere and water bodies decreases the evaporation and condensation on earth, thus adversely affecting the water cycle.

Ans. Cellular respiration is the process by which organisms take up oxygen in order to breathe and digest food. Water is utilized for breaking large molecules that release energy in the form of ATP , while in a subsequent step the water molecules are released back into the cell, which in turn returns to the atmosphere, thus affecting the water cycle.

Ans. Rivers contain more water than streams and thus contribute more to the formation of water vapor through evaporation compared to a stream.

• Water Cycle – Britannica.com
• The Water Cycle – Khanacademy.org
• Water Cycle – Noaa.gov
• What Is The Hydrologic Cycle? – Worldatlas.com
• What is the Water Cycle? – Earth.com
• The Water Cycle – Coastgis.marsci.uga.edu

Article was last reviewed on Wednesday, May 17, 2023

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One response to “Water Cycle”

The first part of the water cycle is of course evaporation and transportation, but I don’t want to focus on that, I want to focus on the 2nd step which is sublimation. Sublimation is when snow or hail, or sleet falls down on a mountain and it quickly turns into water vapor by passing the liquid phase.Now lets skip to the last phase which is RIPC

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The Water Cycle

The new water cycle diagram is now available.

The water cycle describes where water is on Earth and how it moves. Human water use, land use, and climate change all impact the water cycle. By understanding these impacts, we can work toward using water sustainably. 

•   Water Science School HOME   •   Water Cycle Diagrams   • Glossary of Water Cycle Terms   • Water Pools and Fluxes Data Tables

What is the water cycle? 

The water cycle describes where water is on Earth and how it moves. Water is stored in the atmosphere, on the land surface, and below the ground. It can be a liquid, a solid, or a gas. Liquid water can be fresh or saline (salty). Water moves between the places it is stored. Water moves at large scales, through watersheds, the atmosphere, and below the Earth's surface. Water moves at very small scales too. It is in us, plants, and other organisms. Human activities impact the water cycle, affecting where water is stored, how it moves, and how clean it is.  

Pools store water 

Oceans store 96% of all water on Earth. Ocean water is saline, meaning it’s salty. On land, saline water is stored in saline lakes. The rest of the water on Earth is fresh water. Fresh water is stored in liquid form in freshwater lakes , artificial reservoirs, rivers , and wetlands. Water is stored in solid, frozen form in ice sheets and glaciers, and in snowpack at high elevations or near Earth's poles. Water vapor is a gas and is stored as atmospheric moisture over the ocean and land. In the soil, frozen water is stored as permafrost and liquid water is stored as soil moisture. Deeper below ground, liquid water is stored as groundwater in aquifers. Water in groundwater aquifers is found within cracks and pores in the rock.   

Fluxes move water between pools 

As it moves, water can change form between liquid, solid, and gas. Circulation mixes water in the oceans and transports water vapor in the atmosphere. Water moves between the atmosphere and the surface through evaporation , evapotranspiration , and precipitation . Water moves across the surface through snowmelt , runoff , and streamflow . Water moves into the ground through infiltration and groundwater recharge. Underground, groundwater flows within aquifers. Groundwater can return to the surface through natural discharge into rivers, the ocean, and from springs .   

What drives the water cycle? 

Water moves naturally and because of human actions. Energy from the sun and the force of gravity drive the continual movement of water between pools. The sun’s energy causes liquid water to evaporate into water vapor. Evapotranspiration is the main way water moves into the atmosphere from the land surface and oceans. Gravity causes water to flow downward on land. It causes rain, snow, and hail to fall from clouds.    

Humans alter the water cycle 

In addition to natural processes, human water use affects where water is stored and how water moves. We redirect rivers. We build dams to store water. We drain water from wetlands for development. We use water from rivers, lakes, reservoirs, and groundwater aquifers. We use that water to supply our homes and communities . We use it for agricultural irrigation and grazing livestock. We use it in industrial activities like thermoelectric power generation , mining , and aquaculture . 

We also affect water quality. In agricultural and urban areas, irrigation and precipitation wash fertilizers and pesticides into rivers and groundwater . Power plants and factories return heated and contaminated water to rivers. Runoff carries chemicals, sediment , and sewage into rivers and lakes. Downstream from these sources, contaminated water can cause harmful algal blooms , spread diseases, and harm habitats for wildlife.   

The water cycle and climate change 

Climate change is actively affecting the water cycle. It is impacting water quantity and timing. Precipitation patterns are changing. The frequency, intensity, and length of extreme weather events, like floods or droughts , are also changing. Ocean sea levels are rising, leading to coastal flooding. Climate change is also impacting water quality. It is causing ocean acidification which damages the shells and skeletons of many marine organisms. Climate change increases the likelihood and intensity of wildfires , which introduces unwanted pollutants from soot and ash into nearby lakes and streams.   

What determines water availability? 

Humans and other organisms rely on water for life. The amount of water that is available depends on how much water there is in each pool (water quantity). Water availability also depends on when and how fast water moves (water timing) through the water cycle. Finally, water availability depends on how clean the water is (water quality). By understanding human impacts on the water cycle, we can work toward using water sustainably.    

Read more about the components of the water cycle in more detail: 

Atmosphere   ·  Condensation   ·  Evaporation   ·  Evapotranspiration   ·  Freshwater lakes and rivers   ·  Groundwater flow   ·  Groundwater storage   ·  Ice and snow   ·  Infiltration   ·  Oceans   ·  Precipitation   ·  Snowmelt   ·  Springs   ·  Streamflow   ·  Sublimation   ·  Surface runoff  

Home / Essay Samples / Environment / Nature / Water Cycle

Essays on Water Cycle

Understanding the water cycle: a fundamental process.

The water cycle, also known as the hydrologic cycle, is a fundamental and intricate process that regulates the continuous movement and distribution of water on Earth. This essay aims to present an argumentative analysis of the water cycle, its components, and its significance in sustaining...

The Importance of the Water Cycle

The water cycle, a continuous and essential natural process, plays a pivotal role in sustaining life on Earth. This essay presents an argumentative analysis of the significance of the water cycle, emphasizing its crucial role in supporting ecosystems, driving weather patterns, nourishing agriculture, and meeting...

Salt as a Method of Water Conservation: Archaea in Salt Water Lakes

Salt lakes are a harsh environment which has highly saline conditions who grow in extremophiles including a diverse group of halophiles. Halophiles are live in the deep sea, salt mines, and crystalized ponds also. This type of microorganisms has variation in the fluidity of membrane...

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