Abstract
The influence of ENSO events on winter precipitation anomalies in the Philippines has been well known since decades, but whether this effect is different between months needs further exploration. In this study, the monthly variations of precipitation over the Philippines in winter during the mature phases of ENSO events are investigated with datasets of reanalysis and observations from 1979 to 2019. Results indicate that only the eastern Pacific (EP) El Niño shows different influences on the Philippines winter precipitation among different months. In December during mature EP El Niño events, precipitation deficiency is not significant over the whole Philippines, whereas in January and February, precipitation decreases significantly over the southern Philippines as well as the areas to the southeast of the Philippines. Besides, the correlation between consecutive dry days over the southeast Philippines and ENSO is significantly positive in January and February but not in December. The eastward propagation of EP El Niño–related anomalous anticyclone over the western North Pacific (WNPAC) from December to February is proved responsible for the changed relationship between EP El Niño and precipitation. In December, the center of the WNPAC is located to the southeast of the Indo-China Peninsula, inducing weak lower-level wind anomalies and, consequently, weak vertical movement and water vapor transport anomalies over the Philippines, which exerts limited influence on the local precipitation. In January and February, by contrast, the center of WNPAC is located to the southeast of the Philippines, and therefore the southern Philippines is occupied by anticyclonic moisture transports and downward vertical motions, favoring less precipitations and larger than normal consecutive dry days over there.
Highlights
El Niño–Southern Oscillation (ENSO) is characterized by anomalous sea surface temperature (SST) in the tropical Pacific Ocean, exerting significant influence on global climate
Based on multiple datasets of reanalysis and observation, this study reveals a sub-seasonal variation of the El Niño–related precipitation anomalies over the Philippines from December to February
In the December during eastern Pacific (EP) El Niño mature phase, precipitation anomalies are relatively weak over the Philippines and its surrounding areas
Summary
El Niño–Southern Oscillation (ENSO) is characterized by anomalous sea surface temperature (SST) in the tropical Pacific Ocean, exerting significant influence on global climate. Precipitation datasets used in this study are derived from the Climate Prediction Center Merged Analysis of Precipitation (CMAP) with a horizontal resolution of 2.5 ° × 2.5 °over both land and ocean (https://psl.noaa.gov/data/gridded/data.cmap.html), which have been proven predominant in the tropical areas (Xie and Arkin, 1997). The monthly Climatic Research Unit (CRU) Time-Series version 4.04 land precipitation data (https:// crudata.uea.ac.uk/cru/data/hrg/) with a finer horizontal resolution of 0.5 ° × 0.5 ° (Harris et al, 2020) are employed to validate the CMAP results and eliminate the uncertainty brought from data Both datasets cover the study period of 1979–2019. The two-tailed Student’s t-test is used to test the significance of the difference and correlation between two samples, with the significance level set as 0.05 in the current study
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