作者: Yuanyuan Guo , Zhiping Wen , Renguang Wu , Riyu Lu , Zesheng Chen
DOI: 10.1175/JCLI-D-14-00674.1
关键词: Anomaly (natural sciences) 、 Atmospheric sciences 、 Precipitation 、 Baroclinity 、 Geology 、 Climatology 、 Troposphere 、 Boreal 、 Atmospheric circulation 、 Rossby wave 、 Subtropics
摘要: AbstractThe leading mode of boreal winter precipitation variability over the tropical Pacific for period 1980–2010 shows a west–east dipole pattern with one center western North (WNP) and Maritime Continent other equatorial central (CP). Observational evidence that East Asian upper-tropospheric subtropical westerly jet (EAJ) has significant correlation anomalies WNP CP have distinct influence on variation EAJ. A series numerical experiments based linear baroclinic model are performed to confirm heating associated perturbations The results indicate heat source can excite northward-propagating Rossby wave train in upper troposphere Asia facilitate poleward eddy momentum...