1) west wind drift
西风漂流
1.
In view of the interdecadal time scale,the summer precipitation has obviously positive correlations with SST in west Pacific warm pool and equatorial eastern Pacific,while has negative correlations with SST in west wind drift and the area south to it.
在年代际尺度上,降水与西太平洋暖池区、赤道东太平洋的海温有明显的正相关,与西风漂流区及其以南的中太平洋海温则呈现反相关。
3) wind-induced currents
风漂流
1.
Different methods for computation of wind-induced currents in southern Yellow Sea in summer;
夏季南黄海风漂流的不同计算方法的对比分析
4) break adrift
使随风漂流
5) sag to leeward
向下风漂流
6) 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 。
补充资料：西风漂流
在盛行西风吹送下所形成的洋流。自西向东流动。在北半球为北大西洋暖流和北太平洋暖流。在南半球，各大洋西风漂流连在一起，形成横亘太平洋、大西洋、印度洋环绕全球的洋流。
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