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  2. Biotic pump - Wikipedia

    en.wikipedia.org/wiki/Biotic_pump

    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 ocean), the atmospheric volume decreases at a much quicker rater. This causes low pressure to form ...

  3. Transpiration - Wikipedia

    en.wikipedia.org/wiki/Transpiration

    Drier surroundings give a steeper water potential gradient, and so increase the rate of transpiration. Wind: In still air, water lost due to transpiration can accumulate in the form of vapor close to the leaf surface. This will reduce the rate of water loss, as the water potential gradient from inside to outside of the leaf is then slightly less.

  4. Transpirational cooling (biological) - Wikipedia

    en.wikipedia.org/wiki/Transpirational_cooling...

    In the tallest trees, such as Sequoia sempervirens, the water rises well over 100 metres from root-tip to canopy leaves. Such trees also exploit evaporation to keep the surface cool. Water vapour from evapotranspiration mixed with air moves upwards to the point of saturation and then, helped by the emissions of cloud condensation nuclei, forms ...

  5. Precipitation - Wikipedia

    en.wikipedia.org/wiki/Precipitation

    The main ways water vapor is added to the air are: wind convergence into areas of upward motion, [12] precipitation or virga falling from above, [24] daytime heating evaporating water from the surface of oceans, water bodies or wet land, [25] transpiration from plants, [26] cool or dry air moving over warmer water, [27] and lifting air over ...

  6. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    Water returns to the land surface at lower elevation than where it infiltrated, under the force of gravity or gravity induced pressures. Groundwater tends to move slowly and is replenished slowly, so it can remain in aquifers for thousands of years. Transpiration: The release of water vapor from plants and soil into the air.

  7. Vapour-pressure deficit - Wikipedia

    en.wikipedia.org/wiki/Vapour-pressure_deficit

    Vapour pressure-deficit, or VPD, is the difference (deficit) between the amount of moisture in the air and how much moisture the air can hold when it is saturated. Once air becomes saturated, water will condense to form clouds, dew or films of water over leaves. It is this last instance that makes VPD important for greenhouse regulation. If a ...

  8. Do Christmas Trees Need Water? Everything to Know - AOL

    www.aol.com/christmas-trees-water-everything...

    800-290-4726 more ways to reach us. Sign in. Mail. 24/ ... Christmas trees will need water to keep them looking their best and to ensure that they last ... it's vital to give it a drink as soon as ...

  9. Evapotranspiration - Wikipedia

    en.wikipedia.org/wiki/Evapotranspiration

    Transpiration: the movement of water from root systems, through a plant, and exit into the air as water vapor. This exit occurs through stomata in the plant. Rate of transpiration can be influenced by factors including plant type, soil type, weather conditions and water content, and also cultivation practices. [ 6 ] :