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湿数（しっすう）は、気温から露点温度を引いた数値。
, 습수(濕數, dew point depression, T-Td)는 대기의 특정 … 습수(濕數, dew point depression, T-Td)는 대기의 특정 높이에서 온도와 이슬점 온도 간의 차이이다. 일정한 온도에서 차이가 작을수록 수분은 더 많이 존재하게 되며, 즉 상대 습도는 더 높아지게 된다. 더 낮은 대류권에서 수분이 더 많으면(낮은 습수) 과 (lifted condensation levels, LCL)가 낮아진다. LCL의 높이는 극심한 뇌우를 조절하는데 중요한 역할을 한다. 대기에 수분량을 측정하는데 사용되는 습수는 농업과 삼림기상 부문에서, 특히 산불을 예측하는데 중요한 지표가 된다.수는 농업과 삼림기상 부문에서, 특히 산불을 예측하는데 중요한 지표가 된다.
, The dew point depression (T-Td) is the dif … The dew point depression (T-Td) is the difference between the temperature and dew point temperature at a certain height in the atmosphere. For a constant temperature, the smaller the difference, the more moisture there is, and the higher the relative humidity. In the lower troposphere, more moisture (small dew point depression) results in lower cloud bases and lifted condensation levels (LCL). LCL height is an important factor modulating severe thunderstorms. One example concerns tornadogenesis, with tornadoes most likely if the dew point depression is 20 °F (11 °C) or less, and the likelihood of large, intense tornadoes increasing as dew point depression decreases. LCL height also factors in downburst and microburst activity. Conversely, instability is increased when there is a mid-level dry layer (large dew point depression) known as a "dry punch", which is favorable for convection if the lower layer is buoyant. As it measures moisture content in the atmosphere, the dew point depression is also an important indicator in agricultural and forest meteorology, particularly in predicting wildfires.ogy, particularly in predicting wildfires.
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| rdfs:comment |
湿数（しっすう）は、気温から露点温度を引いた数値。
, The dew point depression (T-Td) is the dif … The dew point depression (T-Td) is the difference between the temperature and dew point temperature at a certain height in the atmosphere. For a constant temperature, the smaller the difference, the more moisture there is, and the higher the relative humidity. In the lower troposphere, more moisture (small dew point depression) results in lower cloud bases and lifted condensation levels (LCL). LCL height is an important factor modulating severe thunderstorms. One example concerns tornadogenesis, with tornadoes most likely if the dew point depression is 20 °F (11 °C) or less, and the likelihood of large, intense tornadoes increasing as dew point depression decreases. LCL height also factors in downburst and microburst activity. Conversely, instability is increased when there is a mid-level ty is increased when there is a mid-level
, 습수(濕數, dew point depression, T-Td)는 대기의 특정 … 습수(濕數, dew point depression, T-Td)는 대기의 특정 높이에서 온도와 이슬점 온도 간의 차이이다. 일정한 온도에서 차이가 작을수록 수분은 더 많이 존재하게 되며, 즉 상대 습도는 더 높아지게 된다. 더 낮은 대류권에서 수분이 더 많으면(낮은 습수) 과 (lifted condensation levels, LCL)가 낮아진다. LCL의 높이는 극심한 뇌우를 조절하는데 중요한 역할을 한다. 대기에 수분량을 측정하는데 사용되는 습수는 농업과 삼림기상 부문에서, 특히 산불을 예측하는데 중요한 지표가 된다.수는 농업과 삼림기상 부문에서, 특히 산불을 예측하는데 중요한 지표가 된다.
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| rdfs:label |
湿数
, 습수
, Dew point depression
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