1Analysis of Climatic Changes of Cloud Layers Vertical Structure in Atmospheric Layer below 250 hPa in Antarctica.
Cloudiness plays very important role in distribution of solar radiation and precipitation at the earth surface. Forming of different cloudiness types is viewing complex thermodynamic processes in different atmospheric layers. So knowledge of vertical structure
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.533.3983 http://www.cpc.ncep.noaa.gov/products/outreach/proceedings/cdw27_proceedings/ichernykh_2002.pdf |
| Summary: | Cloudiness plays very important role in distribution of solar radiation and precipitation at the earth surface. Forming of different cloudiness types is viewing complex thermodynamic processes in different atmospheric layers. So knowledge of vertical structure |
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