辐散风和瞬变的涡度通量的异常对定常波年际异常的强迫作用  

THE FORCING OF ANOMALOUS DIVERGENT WIND AND TRANSIENT VORTICITY FLUXES TO THE ANOMALY OF STATIONARY WAVES

作　　者：耿全震[1] 黄荣辉[1] 

机构地区：[1]中国科学院大气物理研究所,国家气候中心

出　　处：《气象学报》1996年第2期132-141,共10页Acta Meteorologica Sinica

基　　金：国家重大项目

摘　　要：研究了１９８２／１９８３年１２—２月对流层上层由辐散风和瞬变的涡度通量所产生的涡度源异常对定常波异常的强迫作用。结果表明，瞬变的涡度通量辐合的异常有抵消或耗散辐散风产生的涡度源异常的趋势；定常波的异常是在这两种强迫力的共同作用下维持的。同时还表明，对１９８２／１９８３年的情况，热带和赤道中东太平洋上的涡度源异常以及中纬度北太平洋上的涡度源异常都对太平洋／北美地区的大气环流异常起了重要的作用。he forcings of anomalous divergent wind and transient vorticity fluxes to the anomaly of stationary waves of DJF 1982/1983 are studied. The results show that the anomaly of the transient vorticity flux convergence tends to cancel or dissipate the anomaly of the vorticity sources generated by divergent wind. The stationary wave anomalies are maintained by both of these forcings.It is also found that,for the DJF 1982/1983 case,both of the vorticity source anomaly over tropical and equatorial easternPacific and that over midlatitude north Pacific are important to maintain the atmospheric circulation anomaly over Pacific/North America region.

关 键 词：辐散风 涡度通量 定常波 强迫作用 年际异常 

分 类 号：P433[天文地球—大气科学及气象学] P425.42