1) Subtropical upper-tropospheric westerly jet
对流层上层西风急流
2) Tropospheric wind
对流层风
3) the tropospheric stream fields
对流层风场
4) convection air layer
对流通风层
5) westerly jet
西风急流
1.
Based on a new climate variability theory “Energy complement each other and balance between westerly jet in winter and subtropical high in summer ”presented by the author in this paper, the flood and drought prediction in China from 1997 to 2001 had been completed.
根据作者提出的气候变化理论“冬季西风急流与夏季副热带高压的能量互补与平衡”对1997～2001年夏季旱涝进行了预测试验。
2.
The significant impact of heating fields on the upper-tropospheric westerly jet has been revealed in much previous research,but little effort has been paid on differentiating the relative contribution of various heating fields over tropical and subtropical regions.
利用NCEP/NCAR月平均再分析资料,采用奇异值分解方法分析200 hPa纬向风场与东亚地表加热场的空间耦合变化特征,揭示影响东亚副热带西风急流位置及强度变化的加热关键区域。
3.
In this paper, westerly jet, storm track and baroclinic wave packets of upper troposphere in the Northern Hemisphere at summer of 1980?1998 are analyzed by using NCEP/NC.
分析了 1998年夏季北半球的西风急流、风暴轴、以及对流层上层的斜压波活动与气候平均情况的异同 ,并揭示了1998年夏季北半球斜压波活动传播的主要区域、斜压波活动的持续性、斜压波向东传播的速度以及斜压波传播时所具有的明显的下游效应 。
6) westerly jet stream
西风急流
1.
In this study,the monthly wind and temperature fields from ECMWF(European Center for Medium-Range Weather Forecasts) reanalysis dataset ERA40 are used to investigate the characteristics and variabilities of the East Asian-western Pacific westerly jet stream(WJS) in winter seasons.
利用ECMWF再分析资料ERA40中的逐月风场和温度场资料,对冬季位于东亚-西太平洋上空的西风急流(WJS)基本结构和异常特征进行了分析。
补充资料：上层建筑(见经济基础与上层建筑)
上层建筑(见经济基础与上层建筑)
superstructure
shongeeng)lonzbu上层建筑(superstrueture)层建筑。见经济基拙与上
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条