Does increasing model stratospheric resolution improve extended-range forecast skill?

被引:51
作者
Roff, Greg [1 ]
Thompson, David W. J. [2 ]
Hendon, Harry [1 ]
机构
[1] Ctr Australian Weather & Climate Res, Melbourne, Vic 3001, Australia
[2] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
关键词
SOUTHERN-HEMISPHERE; DOWNWARD PROPAGATION; PART I; TROPOSPHERE; WEATHER; PARAMETERIZATION; IMPACT;
D O I
10.1029/2010GL046515
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The effect of stratospheric resolution on extended-range forecast skill at high Southern latitudes is explored. Ensemble forecasts are made for two model configurations that differ only in vertical resolution above 100 hPa. An ensemble of twelve 30-day forecasts is made from mid-November for years 1979 to 2008. November is when the Southern Hemisphere stratosphere is most variable, and so this is when impacts on the Southern extratropical troposphere are expected to be greatest. As expected, the high resolution model is associated with better forecast skill in the stratosphere throughout the 30 day integration. Surprisingly, the high resolution model is also associated with significant forecast skill improvement (similar to 5%) in the troposphere similar to 3-4 weeks after the initialization date. The results suggest extended-range forecast skill can be improved in current forecast schemes by increasing model stratospheric resolution, improving representation of stratospheric dynamics and thermodynamics, and improving stratospheric initial conditions. Citation: Roff, G., D. W. J. Thompson, and H. Hendon (2011), Does increasing model stratospheric resolution improve extended-range forecast skill?, Geophys. Res. Lett., 38, L05809, doi: 10.1029/2010GL046515.
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页数:5
相关论文
共 28 条
[1]  
[Anonymous], INT GEOPHYS SER
[2]  
[Anonymous], 2008, 575 ECMWF
[3]   Stratospheric memory and skill of extended-range weather forecasts [J].
Baldwin, MP ;
Stephenson, DB ;
Thompson, DWJ ;
Dunkerton, TJ ;
Charlton, AJ ;
O'Neill, A .
SCIENCE, 2003, 301 (5633) :636-640
[4]   Propagation of the Arctic Oscillation from the stratosphere to the troposphere [J].
Baldwin, MP ;
Dunkerton, TJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D24) :30937-30946
[5]   Stratospheric harbingers of anomalous weather regimes [J].
Baldwin, MP ;
Dunkerton, TJ .
SCIENCE, 2001, 294 (5542) :581-584
[6]   The impact of the stratosphere on the troposphere during the southern hemisphere stratospheric sudden warming, September 2002 [J].
Charlton, AJ ;
O'Neill, A ;
Lahoz, WA ;
Massacand, AC ;
Berrisford, P .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2005, 131 (609) :2171-2188
[7]   Sensitivity of tropospheric forecasts to stratospheric initial conditions [J].
Charlton, AJ ;
O'Neill, A ;
Lahoz, WA ;
Massacand, AC .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2004, 130 (600) :1771-1792
[8]   Can knowledge of the state of the stratosphere be used to improve statistical forecasts of the troposphere? [J].
Charlton, AJ ;
O'Neill, A ;
Stephenson, DB ;
Lahoz, WA ;
Baldwin, MP .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2003, 129 (595) :3205-3224
[9]   Downward propagation and statistical forecast of the near-surface weather [J].
Christiansen, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D14) :1-10
[10]   Downward propagation from the stratosphere to the troposphere: A comparison of the two hemispheres [J].
Graversen, RG ;
Christiansen, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D24)