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The saturation deficit, a moisture parameter which is used in quantitative precipitation forecasting and which is a measure of the mean relative humidity in the layer 1000–500 mb., is related to both satellite-viewed cloud cover and cloud conditions. The results are presented in the form of contingency tables. The positive correlation found between cloud cover and saturation deficit is greatly improved when a distinction is made between deep and shallow cloud conditions.
The saturation deficit, a moisture parameter which is used in quantitative precipitation forecasting and which is a measure of the mean relative humidity in the layer 1000–500 mb., is related to both satellite-viewed cloud cover and cloud conditions. The results are presented in the form of contingency tables. The positive correlation found between cloud cover and saturation deficit is greatly improved when a distinction is made between deep and shallow cloud conditions.
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| Full Text Views | 36 | 17 | 0 |
| PDF Downloads | 21 | 13 | 1 |
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