On the Arctic Boundary Layer : From Turbulence to Climate
The boundary layer is the part of the atmosphere that is in direct contact with the ground via turbulent motion. At mid-latitudes the boundary layer is usually one or a few kilometers deep, while in the Arctic it is much more shallow, typically a few hundred meters or less. The reason is that here t...
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| Format: | Doctoral Thesis |
| Language: | English |
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Stockholms universitet, Meteorologiska institutionen (MISU)
2007
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| Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-6585 http://nbn-resolving.de/urn:isbn:91-7155-373-8 |