摘要
利用中国科学院大气物理研究所 9层大气环流模式 (IAP9L AGCM)对夏季气候进行了 30年 ( 1970～ 1999年 )集合回报试验 ,并采用统计学分析方法对跨季度夏季短期气候的可预测性问题进行了初步探讨 .结果表明 ,该模式对对流层中、高层大气环流的预测能力强于低层 ,位势高度场和表面气温的可预测性最大 ,而降水的可预测性则相对较小 .对流层中、高层位势高度场的可预测性基本呈带状分布 ,越靠近赤道可预测性越高 ;而降水的可预测性基本局限于赤道东太平洋及热带个别区域 .由此可见 ,降水的预测极为困难和复杂 。
This study examines the predictability of extraseasonal short term climate during boreal summer by statistic method. The results are based on ensembles of JJA simulation carried out with the 9 level Atmospheric General Circulation Model developed in the Institute of Atmospheric Physics (IAP9L AGCM) for the years 1970～ 1999. It follows that the ability of the model in predicting atmospheric general circulation in mid and upper troposphere is better than that in low level. Of all analyzed variables, the prediction skill of geopotential height and surface air temperature (precipitation) is the highest (lowest). The correlation coefficient of geopotential height in the mid and upper troposphere is somewhat more zonal in spatial distribution and generally drops off away from the equator, while the prediction skill for precipitation is almost limited in equatorial eastern Pacific and a few small regions in tropics. This is an indication that accurate forecasting of precipitation is extremely difficult and complicated. Moreover, it is of considerable importance to seeking for effective correction system and new physical prediction factors in the following studies.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2004年第1期19-24,共6页
Chinese Journal of Geophysics
基金
国家杰出青年基金项目 (4 0 12 5 0 14 )
中国科学院知识创新工程重要方向性项目(KZCX2 2 0 3 )
国家重点基础研究规划项目(G19980 40 90 5 )
关键词
气候预测
大气环流
集合回报
IAP9L-AGCM
IAP9L AGCM,Extraseasonal short term climate predictions, Ensemble hindcasting, Predictability
