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  4. Impacts of the Kuroshio intrusion through the luzon strait on the local precipitation anomaly
 
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Impacts of the Kuroshio intrusion through the luzon strait on the local precipitation anomaly

Journal
Remote Sensing
Journal Volume
13
Journal Issue
6
Date Issued
2021
Author(s)
Fang W.-P
Wu D.-R
Zheng Z.-W
Gopalakrishnan G
Ho C.-R
Zheng Q
Huang C.-F
Ho H
CHEN-FEN HUANG  
DOI
10.3390/rs13061113
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85103110941&doi=10.3390%2frs13061113&partnerID=40&md5=c1daff75deee81b1d28e33b2d8001f50
https://scholars.lib.ntu.edu.tw/handle/123456789/606345
Abstract
The Kuroshio Current has its origin in the northwestern Pacific, flowing northward to the east of Taiwan and the northern part of Luzon Island. As the Kuroshio Current flows northward, it quasi-periodically intrudes (hereafter referred to as Kuroshio intrusion (KI)) into the northern South China Sea (SCS) basin through the Luzon Strait. Despite the complex generation mechanisms of KI, the purpose of this study is to improve our understanding of the effects of KI through the Luzon Strait on the regional atmospheric and weather variations. Long-term multiple satellite observations, including absolute dynamic topography, absolute geostrophic currents, sea surface winds by ASCAT, multi-scale ultra-high resolution sea surface temperature (MURSST) level-four analysis, and research-quality three-hourly TRMM multi-satellite precipitation analysis (TMPA), was used to systematically examine the aforementioned scientific problem. Analysis indicates that the KI is interlinked with the consequential anomalous precipitation off southwestern Taiwan. This anomalous precipitation would lead to ~560 million tons of freshwater influx during each KI event. Subsequently, independent moisture budget analysis suggests that moisture, mainly from vertical advection, is the possible source of the precipitation anomaly. Additionally, a bulk formula analysis was applied to understand how KI can trigger the precipitation anomaly through vertical advection of moisture without causing an evident change in the low-level flows. These new research findings might reconcile the divisiveness on why winds are not showing a synchronous response during the KI and consequential anomalous precipitation events. ? 2021 by the authors. Licensee MDPI, Basel, Switzerland.
Subjects
Atmospheric re-sponses
Kuroshio intrusion
Luzon Strait
Precipitation
South China Sea
Winds
Advection
Budget control
Lutetium compounds
Moisture
Ocean currents
Surface waters
Topography
Absolute dynamic topography
Geostrophic currents
Northern South China Sea
Precipitation anomalies
Precipitation events
Satellite precipitation
Sea surface temperature (SST)
Ultrahigh resolution
Quality control
SDGs

[SDGs]SDG13

[SDGs]SDG14

Type
journal article

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