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A simple analytical model relates the seasonal excursion of the Intertropical Convergence Zone to seasonal changes in hemispheric forcing. The maximum value of the excursion increases with the seasonal heating change; it decreases with the equator-pole heating difference and with the heat storage capacity of the system as indicated by the lag of the response after the forcing.
A simple analytical model relates the seasonal excursion of the Intertropical Convergence Zone to seasonal changes in hemispheric forcing. The maximum value of the excursion increases with the seasonal heating change; it decreases with the equator-pole heating difference and with the heat storage capacity of the system as indicated by the lag of the response after the forcing.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 125 | 43 | 5 |
| PDF Downloads | 68 | 28 | 2 |
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