蒸发散 Evapotranspiration
(重定向自Potential evapotranspiration)
蒸发散,又称蒸散、蒸散量等,包括了地表水分蒸发与植物体内水分的蒸腾。它是维持陆面水分平衡的一个重要组成部分,也是维持地表能量平衡的主要部分。
计算蒸散的模型有:
- 鲍恩比能量平衡法(BREB法)
- 空气动力学方法
- Penman Monteith公式
- 涡旋相关法
单词 | Potential evapotranspiration |
释义 |
Potential evapotranspiration
中文百科
蒸发散 Evapotranspiration(重定向自Potential evapotranspiration)
蒸发散,又称蒸散、蒸散量等,包括了地表水分蒸发与植物体内水分的蒸腾。它是维持陆面水分平衡的一个重要组成部分,也是维持地表能量平衡的主要部分。 计算蒸散的模型有:
英语百科
Evapotranspiration 蒸发散(重定向自Potential evapotranspiration)
![]() ![]() ![]() ![]() Evapotranspiration (ET) is the sum of evaporation and plant transpiration from the Earth's land and ocean surface to the atmosphere. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy inte****tion, and waterbodies. Transpiration accounts for the movement of water within a plant and the subsequent loss of water as vapor through stomata in its leaves. Evapotranspiration is an important part of the water cycle. An element (such as a tree) that contributes to evapotranspiration can be called an evapotranspirator. |
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