Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall

The moisture transport by tropical cyclones is characterized by high intensity and altitude, which may affect the microphysical processes of heavy rainfall triggered by tropical cyclones. In this study, we used the Weather Research and Forecasting (WRF) model to conduct numerical simulations on a he...

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Main Authors: Tianao Liu, Yilun Chen, Shumin Chen, Weibiao Li, Aoqi Zhang
Format: Article
Language:English
Published: Elsevier 2023-09-01
Series:Weather and Climate Extremes
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2212094723000403
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author Tianao Liu
Yilun Chen
Shumin Chen
Weibiao Li
Aoqi Zhang
author_facet Tianao Liu
Yilun Chen
Shumin Chen
Weibiao Li
Aoqi Zhang
author_sort Tianao Liu
collection DOAJ
description The moisture transport by tropical cyclones is characterized by high intensity and altitude, which may affect the microphysical processes of heavy rainfall triggered by tropical cyclones. In this study, we used the Weather Research and Forecasting (WRF) model to conduct numerical simulations on a heavy rainfall event near the Yangtze River Delta induced by Super Typhoon Mangkhut (2018). The vertical distribution of water vapor was modified to highlight the impact of moisture transport at various heights. The results showed that the distribution and intensity of the rainfall event changed with the transport height of water vapor. Ensuring that the water vapor content in the column kept constant, the total amount of precipitation in the region was greatest when the transport occurred primarily at low levels, and smallest when the transport occurred primarily at mid-levels. Detailed analysis of cloud water, rainwater, and frozen hydrometeors showed that liquid- (ice-) phase processes were the dominant microphysical processes when the transport height is low (mid-to-low). The deposition and riming processes contributed to heavy precipitation when the transport height was at the mid-to-upper levels. Our findings underscore the influence of moisture transport with high intensities and altitudes by tropical cyclones on microphysical processes, ultimately leading to changes in the distribution and intensity of heavy rainfall. Therefore, when analyzing heavy precipitation events, particular attention should be given to the moisture transport at the mid-to-upper levels.
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spelling doaj.art-3d33343610ff4f6ab31da4941c41cd492023-08-29T04:17:27ZengElsevierWeather and Climate Extremes2212-09472023-09-0141100587Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfallTianao Liu0Yilun Chen1Shumin Chen2Weibiao Li3Aoqi Zhang4Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, 519082, China; Corresponding author.The moisture transport by tropical cyclones is characterized by high intensity and altitude, which may affect the microphysical processes of heavy rainfall triggered by tropical cyclones. In this study, we used the Weather Research and Forecasting (WRF) model to conduct numerical simulations on a heavy rainfall event near the Yangtze River Delta induced by Super Typhoon Mangkhut (2018). The vertical distribution of water vapor was modified to highlight the impact of moisture transport at various heights. The results showed that the distribution and intensity of the rainfall event changed with the transport height of water vapor. Ensuring that the water vapor content in the column kept constant, the total amount of precipitation in the region was greatest when the transport occurred primarily at low levels, and smallest when the transport occurred primarily at mid-levels. Detailed analysis of cloud water, rainwater, and frozen hydrometeors showed that liquid- (ice-) phase processes were the dominant microphysical processes when the transport height is low (mid-to-low). The deposition and riming processes contributed to heavy precipitation when the transport height was at the mid-to-upper levels. Our findings underscore the influence of moisture transport with high intensities and altitudes by tropical cyclones on microphysical processes, ultimately leading to changes in the distribution and intensity of heavy rainfall. Therefore, when analyzing heavy precipitation events, particular attention should be given to the moisture transport at the mid-to-upper levels.http://www.sciencedirect.com/science/article/pii/S2212094723000403Heavy precipitationTransport height of water vaporNumerical modelsMicrophysical processesTropical cyclones
spellingShingle Tianao Liu
Yilun Chen
Shumin Chen
Weibiao Li
Aoqi Zhang
Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
Weather and Climate Extremes
Heavy precipitation
Transport height of water vapor
Numerical models
Microphysical processes
Tropical cyclones
title Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
title_full Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
title_fullStr Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
title_full_unstemmed Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
title_short Mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
title_sort mechanisms of the transport height of water vapor by tropical cyclones on heavy rainfall
topic Heavy precipitation
Transport height of water vapor
Numerical models
Microphysical processes
Tropical cyclones
url http://www.sciencedirect.com/science/article/pii/S2212094723000403
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