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  2. Biotic pump - Wikipedia

    en.wikipedia.org/wiki/Biotic_pump

    This causes low pressure to form over this region causing greater moist air than the areas with less rain being evaporated. This causes the moisture in the air to go from an area of high pressure to an area of low pressure. Factors like full sunshine in forested areas and deserts can affect the transfer of moisture in the air.

  3. 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 ...

  4. 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.

  5. Guttation - Wikipedia

    en.wikipedia.org/wiki/Guttation

    The water will accumulate in the plant, creating a slight root pressure. The root pressure forces some water to exude through special leaf tip or edge structures, hydathodes or water glands, forming drops. Root pressure provides the impetus for this flow, rather than transpirational pull. Guttation is most noticeable when transpiration is ...

  6. Evapotranspiration - Wikipedia

    en.wikipedia.org/wiki/Evapotranspiration

    Evapotranspiration (ET) refers to the combined processes which move water from the Earth's surface (open water and ice surfaces, bare soil and vegetation) into the atmosphere. [ 2 ] : 2908 It covers both water evaporation (movement of water to the air directly from soil, canopies , and water bodies) and transpiration (evaporation that occurs ...

  7. Hydraulic redistribution - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_redistribution

    Hydraulic redistribution is a passive mechanism where water is transported from moist to dry soils via subterranean networks. [1] It occurs in vascular plants that commonly have roots in both wet and dry soils, especially plants with both taproots that grow vertically down to the water table, and lateral roots that sit close to the surface.

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

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

    “A real Christmas tree can absorb up to 2 liters of water every day, so be sure to top it up with fresh water frequently,” say the experts at Christmas Tree Direct. And “there is no need to ...

  9. Aerial root - Wikipedia

    en.wikipedia.org/wiki/Aerial_root

    The surface of these roots is covered with porous lenticels, which lead to air-filled spongy tissue called aerenchyma. This tissue facilitates the diffusion of gases throughout the plant, as oxygen diffusion coefficient in air is four orders of magnitude greater than in water. [2] Pneumatophores of mangrove plant