Article ID Journal Published Year Pages File Type
8894527 Journal of Hydrology 2018 45 Pages PDF
Abstract
In general, and across all scales, we find that there are mainly two cycles of maximum TC-rainfall: one diurnal cycle with peaks at ∼10 and ∼22 h (local time), and one semi-diurnal cycle with peaks at ∼2 and ∼5 h (local time). Although in a smaller proportion, the latter exhibits a weak afternoon alternative, i.e., ∼14 and ∼18 h (local time).
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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