1) northwest monsoon
西北季风
2) northwestern margin of East Asian monsoon region
季风区西北缘
3) The northwest influence region of East Asian summer monsoon
东亚夏季风西北影响区
4) muerto
墨西哥夏季的强北风
5) WNPSM
西北太平洋夏季风
1.
Meiyu and tropic cyclone directly influence on the variation of MWL,and it is indicated by Wilcoxon test that the change of MWL is closely correlated to western north pacific summer monsoon(WNPSM),while the correlation is not significant between minimum water level and WNPSM.
梅雨和热带气旋影响次数直接影响太湖最高水位的变化;Wilcoxon检验表明最高水位变化与西北太平洋夏季风指数之间联系密切,而最低水位与其关系则不明显。
6) northeast monsoon
东北季风
1.
Combining the wind satellite data, we analyze the effect of the northeast monsoon on the form and development of the thermal fronts.
结合风场的卫星遥感资料 ,分析了东北季风对南海北部陆架温度锋的影响 ,表明东北季风风速的增加有利于温度锋强度的增强。
2.
In this article we made a statistical research on strong northeast monsoon along the coast of Guangdong province caused by cold air during the decade from 1988 to 1997.
通过对1988～1997年十年中冷空气造成的广东沿海强东北季风过程的统计研究,挑选出多个与强东北季风相关程度较高的因子作最优因子组合,分月份、分时次共设计了24条概率预报方程,从而建立起冬春季强东北季风概率预报方法,因子结构合理,处理技术科学,所有计算过程完全客观定量。
3.
The statistical analysis of climatological data concerning the strong northeast monsoon caused by cold air during the decade from 1988 to 1997 along the coast of Guangdong province reveals that the monthly change of the northeast monsoon is clear, and its interannual change is reducing.
通过对 1988～ 1997年冷空气造成的广东沿海强东北季风过程的气候统计分析 ,发现广东的强东北季风有明显的月分布规律 ,而年际变化有逐渐减少的趋势 ;强东北季风与地面因子相关程度较高 ,而与 85 0hPa要素相关性较低 ;同时发现地面冷高压中心位置聚合度较高 ,但不同月份、不同时次 ,其中心位置有明显差
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
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