The equatorial stratospheric semiannual oscillation and time-mean winds in QBOi models

被引:20
作者
Smith, A. K. [1 ]
Holt, L. A. [2 ]
Garcia, R. R. [1 ]
Anstey, J. A. [3 ]
Serva, F. [4 ]
Butchart, N. [5 ]
Osprey, S. [6 ]
Bushell, A. C. [7 ]
Kawatani, Y. [8 ]
Kim, Y. -H. [9 ]
Lott, F. [10 ]
Braesicke, P. [11 ]
Cagnazzo, C. [4 ]
Chen, C. -C. [1 ]
Chun, H. -Y. [12 ]
Gray, L. [6 ]
Kerzenmacher, T. [11 ]
Naoe, H. [13 ]
Richter, J. [1 ]
Versick, S. [11 ]
Schenzinger, V. [14 ]
Watanabe, S. [8 ]
Yoshida, K. [13 ]
机构
[1] Natl Ctr Atmospher Res, Atmospher Chem Observat & Modeling, 3450 Mitchell Lane, Boulder, CO 80301 USA
[2] Northwest Res Associates, Boulder, CO USA
[3] Canadian Ctr Climate Modelling & Anal, Victoria, BC, Canada
[4] Natl Res Council ISMAR CNR, Inst Marine Sci, Rome, Italy
[5] MOHC, Exeter, Devon, England
[6] Univ Oxford, NCAS, Oxford, England
[7] Met Off, Exeter, Devon, England
[8] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Yokohama, Kanagawa, Japan
[9] Ewha Womans Univ, Seoul, South Korea
[10] LMD, Paris, France
[11] KIT, Karlsruhe, Germany
[12] Yonsei Univ, Seoul, South Korea
[13] Mission Res Inc, Tsukuba, Ibaraki, Japan
[14] Univ Vienna, Vienna, Austria
基金
英国自然环境研究理事会; 新加坡国家研究基金会; 美国国家科学基金会;
关键词
equatorial wind; QBO; SAO; semiannual oscillation; stratosphere; QUASI-BIENNIAL OSCILLATION; GRAVITY-WAVE PARAMETERIZATION; ZONAL WIND; SYNCHRONIZATION; CLIMATOLOGY; MESOSPHERE; IMPACT; SAO;
D O I
10.1002/qj.3690
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Quasi-Biennial Oscillation initiative (QBOi) is a model intercomparison programme that specifically targets simulation of the QBO in current global climate models. Eleven of the models or model versions that participated in a QBOi intercomparison study have upper boundaries in or above the mesosphere and therefore simulate the region where the stratopause semiannual oscillation (SAO) is the dominant mode of variability of zonal winds in the tropical upper stratosphere. Comparisons of the SAO simulations in these models are presented here. These show that the model simulations of the amplitudes and phases of the SAO in zonal-mean zonal wind near the stratopause agree well with the information derived from available observations. However, most of the models simulate time-average zonal winds that are more westward than determined from observations, in some cases by several tens of m center dot s(-1). Validation of wave activity in the models is hampered by the limited observations of tropical waves in the upper stratosphere but suggests a deficit of eastward forcing either by large-scale waves, such as Kelvin waves, or by gravity waves.
引用
收藏
页码:1593 / 1609
页数:17
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