Alwin Andriel L. Bathan , Lyndon Mark P. Olaguera , Faye Abigail T. Cruz , Jose Ramon T. Villarin , Joel T. Maquiling , Maria Obiminda L. Cambaliza , John A. Manalo , Jun Matsumoto
{"title":"热带气旋、西南季风和热带气旋增强西南季风对菲律宾西海岸降雨变率的影响","authors":"Alwin Andriel L. Bathan , Lyndon Mark P. Olaguera , Faye Abigail T. Cruz , Jose Ramon T. Villarin , Joel T. Maquiling , Maria Obiminda L. Cambaliza , John A. Manalo , Jun Matsumoto","doi":"10.1016/j.atmosres.2025.108273","DOIUrl":null,"url":null,"abstract":"<div><div>This study investigates the processes driving interannual variability of rainfall over the western coast of the Philippines during the peak southwest monsoon (SWM) months (July–September) from 1961 to 2022. Specifically, it describes how tropical cyclones (TC), SWM, and TC-enhanced SWM influence SWM rainfall variability. Rainfall measurements from 11 stations along the western coast of the Philippines were classified into three types: direct TC rainfall (P<sub>D</sub>), indirect TC rainfall (P<sub>I</sub>), and SWM rainfall (P<sub>SM</sub>). The yearly contributions of P<sub>D</sub>, P<sub>I</sub>, and P<sub>SM</sub> to SWM rainfall were estimated to be 15.4 %, 33.1 %, and 51.5 %, respectively. Furthermore, four rainfall variability types were found depending on the characteristics of each year's rainfall anomalies: enhanced P<sub>D</sub> but suppressed P<sub>SM</sub> (D+S-), suppressed P<sub>D</sub> but enhanced P<sub>SM</sub> (D-S+), enhanced P<sub>I</sub> but suppressed P<sub>SM</sub> (I+S-), and suppressed P<sub>I</sub> but enhanced P<sub>SM</sub> (I-S+). Composite analysis using ERA5 data revealed the presence of anomalous winds and circulations unique to each type that causes variations in the TC tracks and the monsoon flow, which accounts for the rainfall variability. Notable ones are the anomalous anticyclone over Taiwan in the D+S- case, which pushes TCs closer to the Philippines, and the anomalous anticyclone east of the Philippines in the I+S- case, which enhances the trade winds.</div></div>","PeriodicalId":8600,"journal":{"name":"Atmospheric Research","volume":"326 ","pages":"Article 108273"},"PeriodicalIF":4.4000,"publicationDate":"2025-06-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Influence of tropical cyclones, southwest monsoon, and tropical cyclone-enhanced southwest monsoon on rainfall variability over the western coast of the Philippines\",\"authors\":\"Alwin Andriel L. Bathan , Lyndon Mark P. Olaguera , Faye Abigail T. Cruz , Jose Ramon T. Villarin , Joel T. Maquiling , Maria Obiminda L. Cambaliza , John A. Manalo , Jun Matsumoto\",\"doi\":\"10.1016/j.atmosres.2025.108273\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>This study investigates the processes driving interannual variability of rainfall over the western coast of the Philippines during the peak southwest monsoon (SWM) months (July–September) from 1961 to 2022. Specifically, it describes how tropical cyclones (TC), SWM, and TC-enhanced SWM influence SWM rainfall variability. Rainfall measurements from 11 stations along the western coast of the Philippines were classified into three types: direct TC rainfall (P<sub>D</sub>), indirect TC rainfall (P<sub>I</sub>), and SWM rainfall (P<sub>SM</sub>). The yearly contributions of P<sub>D</sub>, P<sub>I</sub>, and P<sub>SM</sub> to SWM rainfall were estimated to be 15.4 %, 33.1 %, and 51.5 %, respectively. Furthermore, four rainfall variability types were found depending on the characteristics of each year's rainfall anomalies: enhanced P<sub>D</sub> but suppressed P<sub>SM</sub> (D+S-), suppressed P<sub>D</sub> but enhanced P<sub>SM</sub> (D-S+), enhanced P<sub>I</sub> but suppressed P<sub>SM</sub> (I+S-), and suppressed P<sub>I</sub> but enhanced P<sub>SM</sub> (I-S+). Composite analysis using ERA5 data revealed the presence of anomalous winds and circulations unique to each type that causes variations in the TC tracks and the monsoon flow, which accounts for the rainfall variability. Notable ones are the anomalous anticyclone over Taiwan in the D+S- case, which pushes TCs closer to the Philippines, and the anomalous anticyclone east of the Philippines in the I+S- case, which enhances the trade winds.</div></div>\",\"PeriodicalId\":8600,\"journal\":{\"name\":\"Atmospheric Research\",\"volume\":\"326 \",\"pages\":\"Article 108273\"},\"PeriodicalIF\":4.4000,\"publicationDate\":\"2025-06-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Atmospheric Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0169809525003655\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"METEOROLOGY & ATMOSPHERIC SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169809525003655","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
Influence of tropical cyclones, southwest monsoon, and tropical cyclone-enhanced southwest monsoon on rainfall variability over the western coast of the Philippines
This study investigates the processes driving interannual variability of rainfall over the western coast of the Philippines during the peak southwest monsoon (SWM) months (July–September) from 1961 to 2022. Specifically, it describes how tropical cyclones (TC), SWM, and TC-enhanced SWM influence SWM rainfall variability. Rainfall measurements from 11 stations along the western coast of the Philippines were classified into three types: direct TC rainfall (PD), indirect TC rainfall (PI), and SWM rainfall (PSM). The yearly contributions of PD, PI, and PSM to SWM rainfall were estimated to be 15.4 %, 33.1 %, and 51.5 %, respectively. Furthermore, four rainfall variability types were found depending on the characteristics of each year's rainfall anomalies: enhanced PD but suppressed PSM (D+S-), suppressed PD but enhanced PSM (D-S+), enhanced PI but suppressed PSM (I+S-), and suppressed PI but enhanced PSM (I-S+). Composite analysis using ERA5 data revealed the presence of anomalous winds and circulations unique to each type that causes variations in the TC tracks and the monsoon flow, which accounts for the rainfall variability. Notable ones are the anomalous anticyclone over Taiwan in the D+S- case, which pushes TCs closer to the Philippines, and the anomalous anticyclone east of the Philippines in the I+S- case, which enhances the trade winds.
期刊介绍:
The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.