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Nocturnal radiation reversal is essentially an unsteady, advective effect. It requires that clouds or fog drift over a previously cooled surface. In the case of higher clouds, reversal can occur only with a sufficiently intense surface temperature inversion.
Statistics of authentic cases of reversal occurring at Aspendale, Australia (38°02′S, 138°06′E), are given and related to other meteorological variables.
Nocturnal radiation reversal is essentially an unsteady, advective effect. It requires that clouds or fog drift over a previously cooled surface. In the case of higher clouds, reversal can occur only with a sufficiently intense surface temperature inversion.
Statistics of authentic cases of reversal occurring at Aspendale, Australia (38°02′S, 138°06′E), are given and related to other meteorological variables.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 41 | 18 | 2 |
| PDF Downloads | 41 | 28 | 1 |
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