Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations

Ocean variability plays an essential role in the climate system at different time scales through air–sea interactions. Recent studies have addressed the importance of the ocean mixed layer in cooling feedback to tropical cyclones (TCs). However, using constant sea surface temperature (SST) in short-...

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Main Authors: Diah Valentina Lestari, Xiaoming Shi
Format: Article
Language:English
Published: MDPI AG 2021-09-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/9/1138
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spelling doaj-ca0f47a023db4ff6be8f3bee6c97b7142021-09-25T23:43:15ZengMDPI AGAtmosphere2073-44332021-09-01121138113810.3390/atmos12091138Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature VariationsDiah Valentina Lestari0Xiaoming Shi1Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Hong Kong, ChinaDivision of Environment and Sustainability, The Hong Kong University of Science and Technology, Hong Kong, ChinaOcean variability plays an essential role in the climate system at different time scales through air–sea interactions. Recent studies have addressed the importance of the ocean mixed layer in cooling feedback to tropical cyclones (TCs). However, using constant sea surface temperature (SST) in short-range weather forecasts remains common, especially in high-resolution regional models. This study investigates the role of subsurface ocean mixing in the short-range forecast of non-TC extreme rainfall with the Weather Research and Forecast (WRF) model. In the simulations of 26 heavy rainfall cases, we found that using a one-dimensional mixed layer model leads to a 15% enhancement (reduction) of rainfall maximum in six (two) cases compared to using constant SST. When the initial depth of the mixed layer model is perturbed by the amount of daily variability, 13 cases exhibit larger than 15% increases or decreases. A detailed analysis of one case suggests that the radiative process dominates the overall response of SST. The warming and moistening of boundary layer air cause significant strengthening of updrafts in convection. Although the SST change in most cases due to varying mixed layer model setups is less than 0.5 K, convective motions in some cases are surprisingly sensitive to small changes.https://www.mdpi.com/2073-4433/12/9/1138ocean mixed layerprecipitationshort-range forecastWRF-ARW
collection DOAJ
language English
format Article
sources DOAJ
author Diah Valentina Lestari
Xiaoming Shi
spellingShingle Diah Valentina Lestari
Xiaoming Shi
Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
Atmosphere
ocean mixed layer
precipitation
short-range forecast
WRF-ARW
author_facet Diah Valentina Lestari
Xiaoming Shi
author_sort Diah Valentina Lestari
title Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
title_short Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
title_full Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
title_fullStr Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
title_full_unstemmed Sensitivity of the Short-Range Precipitation Forecast in South China Region to Sea Surface Temperature Variations
title_sort sensitivity of the short-range precipitation forecast in south china region to sea surface temperature variations
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2021-09-01
description Ocean variability plays an essential role in the climate system at different time scales through air–sea interactions. Recent studies have addressed the importance of the ocean mixed layer in cooling feedback to tropical cyclones (TCs). However, using constant sea surface temperature (SST) in short-range weather forecasts remains common, especially in high-resolution regional models. This study investigates the role of subsurface ocean mixing in the short-range forecast of non-TC extreme rainfall with the Weather Research and Forecast (WRF) model. In the simulations of 26 heavy rainfall cases, we found that using a one-dimensional mixed layer model leads to a 15% enhancement (reduction) of rainfall maximum in six (two) cases compared to using constant SST. When the initial depth of the mixed layer model is perturbed by the amount of daily variability, 13 cases exhibit larger than 15% increases or decreases. A detailed analysis of one case suggests that the radiative process dominates the overall response of SST. The warming and moistening of boundary layer air cause significant strengthening of updrafts in convection. Although the SST change in most cases due to varying mixed layer model setups is less than 0.5 K, convective motions in some cases are surprisingly sensitive to small changes.
topic ocean mixed layer
precipitation
short-range forecast
WRF-ARW
url https://www.mdpi.com/2073-4433/12/9/1138
work_keys_str_mv AT diahvalentinalestari sensitivityoftheshortrangeprecipitationforecastinsouthchinaregiontoseasurfacetemperaturevariations
AT xiaomingshi sensitivityoftheshortrangeprecipitationforecastinsouthchinaregiontoseasurfacetemperaturevariations
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