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Tropical cyclone characteristics associated with extreme precipitation in the northern Philippines
Author(s) -
Racoma Bernard Alan B.,
Klingaman Nicholas P.,
Holloway Christopher E.,
Schiemann Reinhard K. H.,
Bagtasa Gerry
Publication year - 2022
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.7416
Subject(s) - landfall , climatology , precipitation , tropical cyclone , typhoon , environmental science , intensity (physics) , monsoon , meteorology , geology , geography , physics , quantum mechanics
The Philippines is exposed to tropical cyclones (TCs) throughout the year due to its location in the western North Pacific. While these TCs provide much‐needed precipitation for the country's hydrological cycle, extreme precipitation from TCs may also cause damaging hazards such as floods and landslides. This study examines the relationship between TC extreme precipitation and TC characteristics, including movement speed, intensity and season, for westward‐moving TCs crossing Luzon, northern Philippines. We measure extreme precipitation by the weighted precipitation exceedance (WPE), calculated against a 95th percentile threshold, which considers both the magnitude and spatial extent of TC‐related extreme precipitation. WPE has a significant, moderate positive relationship with TC intensity with a non‐significant, weak negative relationship with movement speed. When TCs are classified by intensity 1 day before landfall (or pre‐landfall), Typhoons (1‐min maximum sustained wind speed ≥64 knots) tend to yield higher WPE than non‐Typhoons (<64 knots). On the other hand, when TCs are classified by pre‐landfall speed, slow TCs (movement speed <11.38 knots) tend to yield higher WPE than fast TCs (movement speed ≥11.38 knots). However, the relationship between pre‐landfall TC intensity and WPE is more pronounced during June–September while there is no significant difference between the WPE of the southwest monsoon (June–September) and northeast monsoon (October–December) seasons. These results suggest that it is important to consider the pre‐landfall cyclone movement speed, intensity and season to anticipate extreme precipitation of incoming TCs. A decision table considering these factors is devised to aid in TC extreme precipitation forecasting.