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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Online Access: | https://doi.org/10.1002/asl.1023 |
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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 |
work_keys_str_mv |
AT siyuansun rossbywavepacketsintheuppertroposphereandtheirassociationswithclimatologicalsummertimedailyprecipitationinmlryrofchina AT zhaoyongguan rossbywavepacketsintheuppertroposphereandtheirassociationswithclimatologicalsummertimedailyprecipitationinmlryrofchina |
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1724170042491273216 |