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Hydrosphere

earth science Maturity 9-11 Next article →

The hydrosphere is the combined body of water found on, under, and above the surface of a planet. On Earth, this system includes oceans, seas, lakes, rivers, and streams. It also encompasses groundwater, soil moisture, and permafrost within the Earth's crust. Even the water vapor, droplets, and crystals in the air are part of this system.

Ocean world Earth
Ocean world Earth

Because water covers approximately 71% of Earth's surface, our home is often called the blue planet. This massive system is essential for regulating life and maintaining the stability of our environment.

Water moves through a continuous process known as the water cycle. This cycle transfers water between different reservoirs, such as the atmosphere, oceans, and groundwater. Solar energy, provided as heat and light, drives much of this movement. Gravity also plays a vital role in moving water back to the surface. Most evaporation occurs from the oceans, returning water to the atmosphere. Water can also move through sublimation, which is evaporation directly from snow and ice. Additionally, trees release water through tiny pores called stomata in a process called transpiration. Hydrologists use the term evapotranspiration to describe these three processes—evaporation, sublimation, and transpiration—working together.

Watercyclesummary
Watercyclesummary

The hydrosphere contains water in several distinct states and locations. Saltwater is the most abundant, accounting for 97.5% of all water on Earth. Fresh water makes up only 2.5% of the total volume. This fresh water is not evenly distributed. About 68.9% is locked away as ice and permanent snow in places like the Arctic and Antarctic. Another 30.8% exists as fresh groundwater. Only 0.3% of the world's fresh water is found in easily accessible forms, such as lakes and rivers. The total mass of the hydrosphere is approximately 1.4 × 10^18 tonnes.

History shows that the hydrosphere has been a changing part of Earth for about 4 billion years. The word itself was brought into English in 1887. It is a translation of the German term *hydrosphäre*, which was introduced by Eduard Suess. Scientists believe the oceans formed as the early Earth cooled. Initially, the atmosphere was thin and rich in hydrogen and helium. As the planet cooled, water vapor released from volcanoes and the cooling Earth condensed. This vapor fell as rain, filling depressions on the surface to create the oceans. This process likely occurred around 4,000 million years ago.

Understanding the scale of the hydrosphere requires looking at specific measurements. There are an estimated 1.386 billion cubic kilometers of water on Earth. The oceans cover about 361 million square kilometers of the surface. The average salinity of these oceans is about 35 grams of salt per kilogram of seawater. The turnover of water is also a massive process. Every year, 577,000 km³ of water evaporates from the ocean and land. This is balanced by 577,000 km³ of precipitation falling back to Earth. This movement ensures that water is constantly migrating through the system.

The hydrosphere is part of a closed system. This means that while water moves and changes form, the total amount of water on Earth has almost certainly not changed since geological times. Water is neither created nor destroyed; it only migrates between reservoirs. This system is deeply connected to the biosphere, where the first life forms began in the oceans. Early organisms did not breathe oxygen, but later, the evolution of cyanobacteria changed everything. These organisms began converting carbon dioxide into food and oxygen, which fundamentally altered the composition of the atmosphere.

Ocean world Earth
Ocean world Earth

Human activity now has a significant impact on these natural cycles. Infrastructure like dams can block and redirect the natural pathways of rivers. Many rivers are no longer free-flowing due to the use of levees and hydropower. Humans also withdraw water from aquifers at an unprecedented rate. For example, the Ogallala Aquifer in the United States is being depleted faster than it can be replenished. If such sources run dry, it can lead to massive economic losses. Furthermore, human-caused pollution and climate change continue to alter the chemistry and patterns of the hydrosphere.

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