Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8894527 | Journal of Hydrology | 2018 | 45 Pages |
Abstract
In general, and across all scales, we find that there are mainly two cycles of maximum TC-rainfall: one diurnal cycle with peaks atâ¯â¼10 andâ¯â¼22â¯h (local time), and one semi-diurnal cycle with peaks atâ¯â¼2 andâ¯â¼5â¯h (local time). Although in a smaller proportion, the latter exhibits a weak afternoon alternative, i.e., â¼14 andâ¯â¼18â¯h (local time).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Manuel F. Rios Gaona, Gabriele Villarini,