Water is always on the move. Rain falling today may have been water in a distant ocean days before. And the water you see in a river or stream may have been snow on a high mountaintop. Water is in the atmosphere, on the land, in the ocean, and underground. It moves from place to place through the water cycle.
Where's the water?
There are about 1.4 billion km3 of water (336 million mi3 of water) on Earth. That includes liquid water in the ocean, lakes, and rivers. It includes frozen water in snow, ice, and glaciers, and water that’s underground in soils and rocks. It includes the water that’s in the atmosphere as clouds and vapor.
If you could put all that water together – like a gigantic water drop – it would be 1,500 kilometers (930 miles) across.
The vast majority of the water on Earth, about 97% of it, fills the ocean. About 2% of the water on Earth is frozen in ice sheets near the poles and in glaciers. Most of the ice is in Antarctica, a smaller amount in Greenland in the Arctic, and a tiny fraction in mountain glaciers around the world. Most of the remaining 1% of Earth’s water is underground, in shallow aquifers, as soil moisture, or deep underground in rock layers. Only a small fraction of the water on Earth (0.03%) is in lakes, wetlands, and rivers.
Water's on the move.
As it moves through the water cycle, water often changes from a liquid, to a solid (ice), to a gas (water vapor). Water in oceans and lakes is typically liquid; but it is solid ice in glaciers, and often invisible water vapor in the atmosphere. Clouds are tiny droplets of liquid water or small ice crystals.
Water at the surface of the ocean, rivers, and lakes can become water vapor and move into the atmosphere with a little added energy from the Sun through a process called evaporation. Snow and ice can also become water vapor through a process called sublimation. And water vapor gets into the atmosphere from plants by a process called transpiration.
Because air is cooler at higher altitude in the troposphere, water vapor cools as it rises high in the atmosphere and transforms into water droplets by a process called condensation. The water droplets that form make up clouds. Water vapor can also condense into droplets near the ground, forming fog when the ground is cold. If the temperature is cold enough, ice crystals form instead of liquid water droplets.
If the droplets or ice crystals within clouds grow in size, they eventually become too heavy to stay in the air, falling to the ground as rain, snow, and other types of precipitation.
What happens to the rain and snow that fall?
Around the world, each year, about 505,000 km3 (121,000 mi3) of water falls as rain, snow, and other types of precipitation.
86% of those raindrops and snowflakes come from the ocean where 434,000 km3 (104,000 mi3) of water evaporates into the atmosphere each year. Water eventually returns to the ocean as precipitation that falls directly into the sea and as precipitation that falls on land and flows to the ocean through rivers.
Less water evaporates over the land than falls onto land as precipitation. Evaporation of water from the land happens directly from lakes, puddles, and other surface water. Also, water also makes its way into the atmosphere via a process called transpiration in which plants release water into the air from their leaves that was pulled up from the soil through roots. Collectively, the water evaporated from the land and from plants is called evapotranspiration.
Some of the snow and ice that falls as precipitation stays on the land as a part of icy mountaintop glaciers or the ice sheets that cover places like Greenland and Antarctica. Some of the precipitation seeps into the ground and joins the groundwater that is often tapped by wells to provide water to farms, towns, and cities.
How long does water stay in a place before it moves?
The length of time that particular water molecules stay in a part of the water cycle is quite variable, but water does stay in certain places longer than others.
A drop of water may spend over 3,000 years in the ocean before evaporating into the air, while a drop of water spends an average of just nine days in the atmosphere before falling back to Earth.
Water spends thousands to hundreds of thousands of years in the large ice sheets that cover Antarctica and Greenland. The oldest ice in Antarctica has been there for 2.7 million years. However, snow that falls in the winter may only stick around for a few days in mid-latitudes locations, where temperatures often rise above freezing causing the snow to melt, or up to six months closer to the Arctic, where temperatures stay below freezing all winter.
Water stays in soil for around one to two months although this varies greatly. Water that’s in soil moves into the atmosphere by evaporation and also by transpiration.
There are exceptions. For example, while water vapor spends relatively little time in the atmosphere, vapor that makes its way into the stratosphere, the layer of the atmosphere above the troposphere where weather typically forms, may remain there for a long time. Also, while water generally spends thousands of years in the ocean before moving on, water in warm, shallow coastal areas may evaporate and leave the ocean very quickly as compared with other areas of the ocean.
Climate change is affecting the water cycle.
Warming global temperatures increases the rate of evaporation and precipitation. The impacts are expected to increase over this century as climate warms. Some areas may experience heavier than normal precipitation, and other areas may become prone to droughts. Other parts of the water cycle - such as clouds, the ocean, glaciers and sea ice - are also affected by climate change.
- Learn more: The Water Cycle and Climate Change