Air relative humidity (RH) was 43～ 91% in general.
地温(Ts)变化范围13～27.5℃，相对湿度(RH)43～91%。
参考来源 - 日光温室黄瓜光能利用与光合效率调节机理的研究Air temperature, relative humidity and wind speed above the 2/3 height of plant were simulated better than the low layers.
模型较好的模拟了冠层2/3高度以上的气温、相对湿度和风速,越接近地面,模拟结果越差。
参考来源 - 农田冠层能量平衡和小气候要素的特征与模拟·2,447,543篇论文数据，部分数据来源于NoteExpress
以上来源于: WordNet
N the mass of water vapour present in the air expressed as a percentage of the mass that would be present in an equal volume of saturated air at the same temperature 相对湿度 → compare absolute humidity
The assumption of constant relative humidity is important, because water vapor in the atmosphere is another efficient absorber of radiation at infrared wavelength.
相对湿度恒定的假设是重要的，因为大气中的水蒸气是红外波长辐射的另一种有效吸收剂。
Because warm air can hold more moisture than cool air, the relative humidity will be constant only if the amount of water vapor in the atmosphere increases as the temperature rises.
因为温暖的空气比冷空气能容纳更多的湿气，所以只有当大气中的水蒸气量随着温度的升高而增加时，相对湿度才会保持不变。
Relative humidity is expressed as percentage.
相对湿度采用百分数表示。
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