Water cycle

Water cycle


The water cycle has no beginning or end. The sun, which drives the water cycle, heats the water of the ocean. Part of that water evaporates as water vapor. Ice and snow flow directly into water vapor. Upstream air streams carry water vapor and evaporate the steam (soils from the soil and plants) into the upper atmosphere. The water vapor is condensed into clouds at cold temperatures in the sky. Air currents circulate around the globe, cloud particles collide, grow and fall from the sky as precipitation. Some of these are part of the snow, and they accumulate frozen water for thousands of years in the appearance of snow and glaciers.

In warm summers, such as spring, it melts snow and flows on land. Most of the rainfall is back to the ocean or land, and the surplus floods over land as a result of gravity. A part of this excess flows into the valleys' rivers, and these streams of water flow toward the ocean. This excess and groundwater leak are stored in lakes as fresh water. This irrigation does not always flow into a river. Some of it is leaking into the ground. This part of the water that drains will fill the aquifers again. These aquifers retain overwhelming amounts of fresh water for a long period of time. Part of the spill is deposited near the surface of the earth, and the groundwater leak back to surface water again, and some of the underground water flows through the surface of the ground. This will restart the water cycle.


Different in the water cycle


Rainfall is the condensation of water vapor falling on Earth's surface. The most abundant rainfall is rain, but it also receives ice, rain, fog, and heavy rain. At maximum rains, 505,000km3 of earth receives the water, and that 398,000 km3 of that water falls to the ocean.

Canal interlocking is the evaporation that flows down on the leafy branches of the triangle and evaporates back into the atmosphere. Snow melting is the production of water. Water flows are various methods of water flowing over the earth. This includes both the flow of the surface and the flow of streams. This flows into any activity, such as seepage into the ground, evaporation, storage of lakes and reservoirs or for the exploitation of agriculture and other human uses. Leakage means the surface water flowing into the ground. The water is either in soil water or in ground water.

Submersion flows are flowing underground as run-in zones or as aquifers. Subsurface water returns to the top or pumping, or flows to the oceans. Graduction, influenced by it, re-emerges from a lower level than the water leaked. Groundwater flow is slow, and the time taken to recharge is also slow. Therefore, the aquifers exist for thousands of years. Evaporation is the addition of water that flows on the surface of the earth from the liquid phase to the atmosphere and joins the atmosphere.

The power for evaporation is primarily due to solar radiation. Evaporation also includes the transpiration from plants. The annual total evaporation amounts to 505,000 km3, of which 434,000 km3 is the ocean. Overturning is a variation of the water (ice or ice) to the water vapor.

Adulthood is the movement of water through solid, liquid, or gaseous atmospheres. Without evaporation, the steam that evaporates from the oceans will not be able to return to the surface as rain.

Condensation is the formation of clouds or mist resulting in the formation of water vapor in the air, or water vapor in the air.


The water cycle changes over time.


water cycle is the process that describes the movement of water through the hydrosphere. But a large portion of the water is stored for a long time without moving to the water cycle. Most of this water is stored in the oceans. It is estimated that 332,500,000 gallons (1,386,000Km3) of water are stored in oceans, 321,000,000 gallons (1,338,000,000Km3) of water, or 95% of the total. About 90% of the water vapor supplied to the water cycle is supplied by oceans.

In cold climates, there is more snow and glacier in the glaciers, and part of the global water supply turns into ice, reducing the amount of water that flows to the other part of the water cycle. The weather is not so hot in warm weather. The ice age was 1/3 of the world's land cover, and the ocean currents were about 400 feet (122 m) below the present size. About 3 million years ago, at Earth's last hot stage, the sea level was 18 feet (5'5 meters). About 3 million years ago, the ocean was above 165 feet (50 m) above. Scientists unanimously accepted the 2007 Intergovernmental Panel on Climate Change (IPCC) Policies for the Climate Change Situation that the water cycle is growing throughout the 21st century. But this does not mean that this idea is increasing in all parts of the world. In the dry season, relative to vertical regions, a decline in rainfall can be shown in the 21st century. This can lead to drought, and the likelihood of drought will increase. These dry spheres are more potent in polarized subtropical zones (eg, the Mediterranean region, South Africa, South Australia, and the Southwestern United States). Presently, westerly weather forecasts are expected to increase. This large-scale climate model was the result of research conducted in several international research centers according to the IPCC's 4th assessment. Presently, westerly weather forecasts are expected to increase. This large-scale climate model was the result of research conducted in several international research centers according to the IPCC's 4th assessment. Presently, westerly weather forecasts are expected to increase. This large-scale climate model was the result of research conducted in several international research centers according to the IPCC's 4th assessment.

Glacial melting is also an example of a change in the water cycle. The depth of the glaciers from the rainfall is not sufficient to restore the flood by pouring and melting. The glacial melting has been widespread since the 1850s.

water cycle is powered from solar energy. 86% of global evaporation reduces the temperature of the ocean due to steam cooling. When evaporation stops cooling, the greenhouse effect can increase the surface heat of 67 ° C, making the world warmer.

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