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The extreme Northeast China cold vortex activities in the late spring of 2021 and possible causes involved

Jie WU Ying LIU Yong-Sheng LI Jin-Qing ZUO Yu NIE Qing-Quan LI Shuai ZHANG Dong-Qian WANG

气候变化研究进展(英文版)2022,Vol.13Issue(6):787-796,10.
气候变化研究进展(英文版)2022,Vol.13Issue(6):787-796,10.

The extreme Northeast China cold vortex activities in the late spring of 2021 and possible causes involved

The extreme Northeast China cold vortex activities in the late spring of 2021 and possible causes involved

Jie WU 1Ying LIU 2Yong-Sheng LI 1Jin-Qing ZUO 2Yu NIE 3Qing-Quan LI 1Shuai ZHANG 2Dong-Qian WANG1

作者信息

  • 1. CMA Climate Studies Key Laboratory&CMA-NJU Joint Laboratory for Climate Prediction Studies,National Climate Center China Meteorological Administration(CMA),Beijing 100081,China
  • 2. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Information Science&Technology,Nanjing 210044,China
  • 3. Heilongjiang Climate Center Harbin 150030,China
  • 折叠

摘要

关键词

Northeast China cold vortex(NCCV)/Wave train/La Nina event/Snow depth/Barotropic energy conversion

Key words

Northeast China cold vortex(NCCV)/Wave train/La Nina event/Snow depth/Barotropic energy conversion

引用本文复制引用

Jie WU,Ying LIU,Yong-Sheng LI,Jin-Qing ZUO,Yu NIE,Qing-Quan LI,Shuai ZHANG,Dong-Qian WANG..The extreme Northeast China cold vortex activities in the late spring of 2021 and possible causes involved[J].气候变化研究进展(英文版),2022,13(6):787-796,10.

基金项目

This study was jointly sponsored by the National Natural Science Foundation of China(41905067,42175052),the Na-tional Key Research and Development Program(2021YFA0718000),the Innovative Development Special Project of China Meteorological Administration(CXFZ2021Z011,CXFZ2021Z010 and CXFZ2022J039),and the science funding from Beijing Meteorological Service(BMBKJ202003005).The computations were conducted on the Shuguang-PI high-per-formance computing platform from the China Meteorological Administration,which is gratefully acknowledged for the generous provision of computational resources.The atmo-spheric circulation and moisture data are from the NCEP/NCAR Reanalysis data(https://psl.noaa.gov/data/gridded/data.ncep.reanalysis.pressure.html).The CPC Merged Analysis of Pre-cipitation(CMAP)dataset are downloaded from https://psl.noaa.gov/data/gridded/data.cmap.html.The ERA5 dataset is download from https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-land-monthly-means?tab=form.NOAA_OI_SST_V2 data provided by the NOAA/OAR/ESRL PSL,Boulder,Colorado,USA,from their Web site at https://psl.noaa.gov/data/gridded/data.noaa.oisst.v2.html.The NCDC snow depth dataset is provided by the Cold and Arid Regions Sciences Data Center at Lanzhou(http://westdc.westgis.ac.cn).The authors also thank Nanjing Hurricane Translation for reviewing the English language quality. (41905067,42175052)

气候变化研究进展(英文版)

OACSCDSCI

1674-9278

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