2023
DOI: 10.3390/rs15020340
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Investigating the Influence of Water Vapor on Heavy Rainfall Events in the Southern Korean Peninsula

Abstract: In this study, we examined the influence of water vapor on heavy rainfall events over the complex mountainous terrain of the southern Korean Peninsula using rawinsonde and global navigation satellite system (GNSS) datasets from a mobile observation vehicle (MOVE). Results demonstrated that the prevailing southeasterly winds enhanced precipitation on the leeward side of the mountainous region. The probability of severe rainfall increased in the highest precipitable water vapor (PWV) bin (>60 mm). A lead–lag … Show more

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Cited by 4 publications
(2 citation statements)
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“…The terrain of the study area is relatively flat, but micro-terrain features such as the northern mountainous region and the southern hills affect the formation, intensity, and spatial-temporal distribution of extreme rainfall to a certain degree by influencing atmospheric stability, wind fields, and water vapor transport, among other factors [90]. Mountains can affect the generation of extreme precipitation by lifting or blocking low-level airflow and inducing substantial rain when unstable airflow impacts the terrain [91,92]. Meanwhile, the terrain affects atmospheric water vapor transport, and upward airflow can cause convective precipitation, enhancing precipitation intensity.…”
Section: Discussionmentioning
confidence: 99%
“…The terrain of the study area is relatively flat, but micro-terrain features such as the northern mountainous region and the southern hills affect the formation, intensity, and spatial-temporal distribution of extreme rainfall to a certain degree by influencing atmospheric stability, wind fields, and water vapor transport, among other factors [90]. Mountains can affect the generation of extreme precipitation by lifting or blocking low-level airflow and inducing substantial rain when unstable airflow impacts the terrain [91,92]. Meanwhile, the terrain affects atmospheric water vapor transport, and upward airflow can cause convective precipitation, enhancing precipitation intensity.…”
Section: Discussionmentioning
confidence: 99%
“…To explore the temporal and spatial interaction characteristics of PWV and actual rainfall during typhoon 'Chandu' and three other typhoon events in Taiwan from 2015 to 2017, they were investigated using the PWV retrieved from the real-time precise point positioning technology or ground-based GPS data [22,23]. Kim et al found that the most intense rainfall events occurred after a rapid increase in PWV along with a strong southwesterly water-vapor flow during convective instability [24]. Zhao et al used the anomalous variations of the PWV inverted by ERA5 with other atmospheric parameters related to typhoons to analyze a typhoon-monitoring method with and without considering the typhoon's acceleration during the time of the maximum value of the PWV during the typhoon period [25].…”
Section: Introductionmentioning
confidence: 99%