| Autor: |
Yan-yu Yue, Yu Zhang, Jing Wang, Sheng-jie Niu, Feng Xu, Xu Dan, Li-juan Zhao |
| Rok vydání: |
2010 |
| Předmět: |
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| Zdroj: |
2010 Second IITA International Conference on Geoscience and Remote Sensing. |
| DOI: |
10.1109/iita-grs.2010.5602975 |
| Popis: |
The temperature is superadiabatic degressive at 70 meters below, and is approximate isothermal at 70–120 meters during fog process. The temperature inversion occurs apparently at night because that wind direction turns clockwise with high so that there is warming advection in boundary. In fog process, relative humidity increases with high in detection area and exceeds 85% above 80 meters, above of which increases relatively slowly . Relative humidity contour approximate exponentially distributed under 120 meter. Wind speed exceeds 10 meters per second above 120 meters height at boundary and linearly increases with height. Wind profiling has an approximate linear distribution at detection range during fog process. Wind direction is basically unchanged with high above 20 meters, which is the basic easterly wind or southeast wind so that it brings moisture vapor from the sea. Wind direction turns clockwise with high which led directly to the phenomenon of the atmospheric warming significantly at night. |
| Databáze: |
OpenAIRE |
| Externí odkaz: |
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