Examining the Predictability of the Stratospheric Sudden Warming of January 2013 Using Multiple NWP Systems

Examining the Predictability of the Stratospheric Sudden Warming of January 2013 Using Multiple NWP Systems
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DOI:
10.1175/mwr-d-15-0010.1
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发表时间:
2016-04
影响因子:
3.2
通讯作者:
O. Tripathi;M. Baldwin;A. Charlton-Perez;M. Charron;J. Cheung;S. Eckermann;E. Gerber;D. Jackson;Y. Kuroda;A. Lang;J. McLay;R. Mizuta;C. Reynolds;G. Roff;M. Sigmond;S. Son;T. Stockdale
O. Tripathi;M. Baldwin;A. Charlton-Perez;M. Charron;J. Cheung;S. Eckermann;E. Gerber;D. Jackson;Y. Kuroda;A. Lang;J. McLay;R. Mizuta;C. Reynolds;G. Roff;M. Sigmond;S. Son;T. Stockdale
中科院分区:
地球科学2区
文献类型:
--
作者:
O. Tripathi;M. Baldwin;A. Charlton-Perez;M. Charron;J. Cheung;S. Eckermann;E. Gerber;D. Jackson;Y. Kuroda;A. Lang;J. McLay;R. Mizuta;C. Reynolds;G. Roff;M. Sigmond;S. Son;T. Stockdale

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AbstractThe first multimodel study to estimate the predictability of a boreal sudden stratospheric warming (SSW) is performed using five NWP systems. During the 2012/13 boreal winter, anomalous upward propagating planetary wave activity was observed toward the end of December, which was followed by a rapid deceleration of the westerly circulation around 2 January 2013, and on 7 January 2013 the zonal-mean zonal wind at 60°N and 10 hPa reversed to easterly. This stratospheric dynamical activity was followed by an equatorward shift of the tropospheric jet stream and by a high pressure anomaly over the North Atlantic, which resulted in severe cold conditions in the United Kingdom and northern Europe. In most of the five models, the SSW event was predicted 10 days in advance. However, only some ensemble members in most of the models predicted weakening of westerly wind when the models were initialized 15 days in advance of the SSW. Further dynamical analysis of the SSW shows that this event was characterized ...