Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework

The diurnal cycle of convection and precipitation is an important atmospheric feature. It also poses a great challenge to global numerical atmospheric modeling. Over continental East Asia, most global models cannot well capture the nocturnal and early morning peaks of summer rainfall. This problem m...

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Main Authors: Yi Zhang, Haoming Chen, Dan Wang
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/2/53
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spelling doaj-1312e62ae4e34c8798bf543f863a8d992020-11-25T00:31:05ZengMDPI AGAtmosphere2073-44332019-01-011025310.3390/atmos10020053atmos10020053Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling FrameworkYi Zhang0Haoming Chen1Dan Wang2State Key Laboratory of Severe Weather (LaSW), Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081, ChinaState Key Laboratory of Severe Weather (LaSW), Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081, ChinaNumerical Weather Prediction Center, National Meteorological Center, China Meteorological Administration, Beijing 100081, ChinaThe diurnal cycle of convection and precipitation is an important atmospheric feature. It also poses a great challenge to global numerical atmospheric modeling. Over continental East Asia, most global models cannot well capture the nocturnal and early morning peaks of summer rainfall. This problem may lead to dry biases and limit the modeling skills. This study investigates this problem using a global multiscale modeling framework (Super-Parameterized CAM5; SPCAM5). The nocturnal and early morning peaks, which are almost absent in CAM5 and a coarser-resolution SPCAM5, can be successfully captured by SPCAM5 with a moderate increase in the horizontal resolution. On the lee side of the Tibetan Plateau, SPCAM5 generates robust eastward propagating rainfall signals, which correspond to the moving convective systems, as revealed by the heating and drying profiles. Over the eastern plain of China, the early morning peaks become more evident, corresponding to a stratiform-type heating structure in the midlevel. A sensitivity experiment with altered grid-scale forcing also suggests the important preconditioning role of the vertical moisture advection in regulating the early morning peaks. These results highlight the added value of representing multiscale processes to the successful simulation of the diurnal cycle over continental East Asia.https://www.mdpi.com/2073-4433/10/2/53global weather and climate modelsconvection and precipitationdiurnal cyclenumerical modeling of the atmosphere
collection DOAJ
language English
format Article
sources DOAJ
author Yi Zhang
Haoming Chen
Dan Wang
spellingShingle Yi Zhang
Haoming Chen
Dan Wang
Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
Atmosphere
global weather and climate models
convection and precipitation
diurnal cycle
numerical modeling of the atmosphere
author_facet Yi Zhang
Haoming Chen
Dan Wang
author_sort Yi Zhang
title Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
title_short Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
title_full Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
title_fullStr Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
title_full_unstemmed Robust Nocturnal and Early Morning Summer Rainfall Peaks over Continental East Asia in a Global Multiscale Modeling Framework
title_sort robust nocturnal and early morning summer rainfall peaks over continental east asia in a global multiscale modeling framework
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2019-01-01
description The diurnal cycle of convection and precipitation is an important atmospheric feature. It also poses a great challenge to global numerical atmospheric modeling. Over continental East Asia, most global models cannot well capture the nocturnal and early morning peaks of summer rainfall. This problem may lead to dry biases and limit the modeling skills. This study investigates this problem using a global multiscale modeling framework (Super-Parameterized CAM5; SPCAM5). The nocturnal and early morning peaks, which are almost absent in CAM5 and a coarser-resolution SPCAM5, can be successfully captured by SPCAM5 with a moderate increase in the horizontal resolution. On the lee side of the Tibetan Plateau, SPCAM5 generates robust eastward propagating rainfall signals, which correspond to the moving convective systems, as revealed by the heating and drying profiles. Over the eastern plain of China, the early morning peaks become more evident, corresponding to a stratiform-type heating structure in the midlevel. A sensitivity experiment with altered grid-scale forcing also suggests the important preconditioning role of the vertical moisture advection in regulating the early morning peaks. These results highlight the added value of representing multiscale processes to the successful simulation of the diurnal cycle over continental East Asia.
topic global weather and climate models
convection and precipitation
diurnal cycle
numerical modeling of the atmosphere
url https://www.mdpi.com/2073-4433/10/2/53
work_keys_str_mv AT yizhang robustnocturnalandearlymorningsummerrainfallpeaksovercontinentaleastasiainaglobalmultiscalemodelingframework
AT haomingchen robustnocturnalandearlymorningsummerrainfallpeaksovercontinentaleastasiainaglobalmultiscalemodelingframework
AT danwang robustnocturnalandearlymorningsummerrainfallpeaksovercontinentaleastasiainaglobalmultiscalemodelingframework
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