天空色彩
天空因散射光的波谱差异而显露的色彩。不同的色彩对应了不同的散射光光谱。干洁天气，大气以分子散射为主，对太阳辐射的短波成分散射能力较强，天空成湛蓝色，随太阳高度增高还可能向紫色偏移。大气中水汽增加或大气混浊度变大时，大颗粒气溶胶散射占主导地位，散射光与波长的关系降低，天空呈现灰白色。
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contributed at 2011-12-26
Classification(s)
●
Earth System(in Chinese) Meteorological climatology
Detailed Description
| English |
|---|
| Name | sky colour |
| Chinese |
|---|
| Name | 天空色彩 |
| Description | 天空因散射光的波谱差异而显露的色彩。不同的色彩对应了不同的散射光光谱。干洁天气，大气以分子散射为主，对太阳辐射的短波成分散射能力较强，天空成湛蓝色，随太阳高度增高还可能向紫色偏移。大气中水汽增加或大气混浊度变大时，大颗粒气溶胶散射占主导地位，散射光与波长的关系降低，天空呈现灰白色。 |
How to Cite
NNU_Group (2011). 天空色彩, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/3e70b5b0-1b98-434f-9bf8-1fe2004ef53d
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