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  2. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. [2] The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the environment. When it condenses, it releases energy and warms the environment.

  3. Streamflow - Wikipedia

    en.wikipedia.org/wiki/Streamflow

    Streamflow, or channel runoff, is the flow of water in streams and other channels, and is a major element of the water cycle.It is one runoff component, the movement of water from the land to waterbodies, the other component being surface runoff.

  4. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Since liquid water flows, ocean waters cycle and flow in currents around the world. Since water easily changes phase, it can be carried into the atmosphere as water vapour or frozen as an iceberg. It can then precipitate or melt to become liquid water again. All marine life is immersed in water, the matrix and womb of life itself. [7]

  5. Biotic pump - Wikipedia

    en.wikipedia.org/wiki/Biotic_pump

    Prior to the biotic pump theory, trees were thought to have a passive role in the water cycle. [5] By contrast those developing the biotic pump concept state that “forest and trees are prime regulators within the water, energy and carbon cycles.” [ 6 ] In areas were there is more rain is currently being evaporated (on land versus over the ...

  6. Subsurface flow - Wikipedia

    en.wikipedia.org/wiki/Subsurface_flow

    Subsurface flow, in hydrology, is the flow of water beneath Earth's surface as part of the water cycle. In the water cycle, when precipitation falls on the Earth's land, some of the water flows on the surface forming streams and rivers. The remaining water, through infiltration, penetrates the soil traveling underground, hydrating the vadose ...

  7. Evapotranspiration - Wikipedia

    en.wikipedia.org/wiki/Evapotranspiration

    The water balance equation relates the change in water stored within the basin (S) to its input and outputs: Δ S = P − E T − Q − D {\displaystyle \Delta S=P-ET-Q-D\,\!} In the equation, the change in water stored within the basin ( ΔS ) is related to precipitation ( P ) (water going into the basin), and evapotranspiration ( ET ...