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Meteorological data and information on condensation nuclei (CN) levels were collected from the peak area of Mount Kenya over a short period in July 1977. The relationship between CN, vertical temperature structure and wind speed is examined. A schematic model of the behavior of haze layers near the top of the mountain is suggested.
Meteorological data and information on condensation nuclei (CN) levels were collected from the peak area of Mount Kenya over a short period in July 1977. The relationship between CN, vertical temperature structure and wind speed is examined. A schematic model of the behavior of haze layers near the top of the mountain is suggested.
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|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 246 | 65 | 28 |
| PDF Downloads | 36 | 7 | 1 |
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