Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China

Abstract Using the NCEP/NCAR reanalysis and station observations in China during 1979–2018, features of propagation of baroclinic wave packets in the upper troposphere and their relationships with precipitation over the middle and lower reaches of the Yangtze River (MLRYR) in daily climatology are i...

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Main Authors: Siyuan Sun, Zhaoyong Guan
Format: Article
Language:English
Published: Wiley 2021-04-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.1023
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spelling doaj-b5cf894e64ad48648bcc107001a384eb2021-04-02T09:00:37ZengWileyAtmospheric Science Letters1530-261X2021-04-01224n/an/a10.1002/asl.1023Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of ChinaSiyuan Sun0Zhaoyong Guan1Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD), Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), International Joint Laboratory on Climate and Environment Change (ILCEC) Nanjing University of Information Science and Technology Nanjing ChinaCollaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD), Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), International Joint Laboratory on Climate and Environment Change (ILCEC) Nanjing University of Information Science and Technology Nanjing ChinaAbstract Using the NCEP/NCAR reanalysis and station observations in China during 1979–2018, features of propagation of baroclinic wave packets in the upper troposphere and their relationships with precipitation over the middle and lower reaches of the Yangtze River (MLRYR) in daily climatology are investigated after having components with periods longer than 9 days filtered out. It is demonstrated that in the filtered daily climatology, the baroclinic wave packets still exist. The wave packet migrates eastward on the northern sides of the westerly jet stream axis whereas it does not move explicitly in the southern side of the axis in the upper troposphere. The filtered daily precipitation over MLRYR is mainly affected by the wave packets in the region south of the westerly jet axis. These results are very meaningful for better understanding behaviors of Rossby waves in daily climatology and the causes of daily precipitation variations in MLRYR.https://doi.org/10.1002/asl.1023boreal summerChinadaily climatologyprecipitationwave packet
collection DOAJ
language English
format Article
sources DOAJ
author Siyuan Sun
Zhaoyong Guan
spellingShingle Siyuan Sun
Zhaoyong Guan
Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
Atmospheric Science Letters
boreal summer
China
daily climatology
precipitation
wave packet
author_facet Siyuan Sun
Zhaoyong Guan
author_sort Siyuan Sun
title Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
title_short Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
title_full Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
title_fullStr Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
title_full_unstemmed Rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in MLRYR of China
title_sort rossby wave packets in the upper troposphere and their associations with climatological summertime daily precipitation in mlryr of china
publisher Wiley
series Atmospheric Science Letters
issn 1530-261X
publishDate 2021-04-01
description Abstract Using the NCEP/NCAR reanalysis and station observations in China during 1979–2018, features of propagation of baroclinic wave packets in the upper troposphere and their relationships with precipitation over the middle and lower reaches of the Yangtze River (MLRYR) in daily climatology are investigated after having components with periods longer than 9 days filtered out. It is demonstrated that in the filtered daily climatology, the baroclinic wave packets still exist. The wave packet migrates eastward on the northern sides of the westerly jet stream axis whereas it does not move explicitly in the southern side of the axis in the upper troposphere. The filtered daily precipitation over MLRYR is mainly affected by the wave packets in the region south of the westerly jet axis. These results are very meaningful for better understanding behaviors of Rossby waves in daily climatology and the causes of daily precipitation variations in MLRYR.
topic boreal summer
China
daily climatology
precipitation
wave packet
url https://doi.org/10.1002/asl.1023
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