1) Spatial background fields during the Plum Rains
梅雨期高空背景场
3) Meiyu precipitation
梅雨期雨量
1.
Correlation and moving correlation analysis are used in this paper in order to find out the relation between the total precipitation in the Yangtze-Huaihe River valley during Meiyu period (Meiyu precipitation) and the sea surface temperature (SST) in the Pacific Ocean from the previous winter to Meiyu period.
运用相关分析和滑动相关方法,分析了江淮流域5个代表站1903-2000年梅雨期雨量的变化特征及其与太平洋海温的相关关系及年代际差异。
4) Meiyu period
梅雨期
1.
A Lagrangian Diagnosis on a Block Case during the 1991 Meiyu Period in the Changjiang-Huaihe Region;
1991年江淮梅雨期一个阻塞个例的Lagrange诊断分析
2.
On the basis of the daily precipitation of the Meiyu period at 44 stations in the Changjiang-Huaihe region from 1954 to 2003,the temporal evolution and spatial distribution characters of torrentialrain(≥50 mm/d) are investigated in terms of fuzzy cluster method and empirical orthogonal function(EOF) decomposition.
利用江淮地区44个站1954—2003年近50 a逐日降水资料,采用模糊聚类和经验正交函数分解(EOF)方法分析了江淮梅雨期暴雨的时空变化特征。
3.
The water vapor transport model at the regional boundary in the Meiyu period is put forward through diagnostic analysis.
通过诊断分析,提出梅雨期中国区域边界水汽输送特征模型,即高原中部区域西边界与低纬南海、西太平洋南边界为水汽输送流入主体,西太平洋东边界为水汽“流出”主体。
5) Mei-yu period
梅雨期
1.
Based on 1959—2000 daily precipitation data of 76 stations in the Changjiang-Huaihe area of China,the Changjiang-Huaihe area is divided into four regions with different spatial features of rainfall in Mei-yu period by use of REOF decomposition.
应用1959—2000年江淮地区76站逐日降水资料,对梅雨期月降水量进行REOF分解。
2.
Using the June and July maximum temperature data at 64 observational stations from 1961 to 2001,the Changjiang-Huaihe valley s maximum temperature field in the Mei-yu period is divided objectively into 3 subdivisions by using the rotated empirical orthogonal function(REOF) method.
利用江淮地区64个测站1961—2001年6—7月最高气温资料,采用旋转经验正交展开(REOF)方法对江淮地区梅雨期最高气温场进行客观分区,并分析了各区域最高气温的长期演变趋势。
6) plum rain period forecasting
梅雨期预报
补充资料：梅雨
| 梅雨 春末夏初 (5月底～7月初)中国长江 、淮河流域和日本南部的连阴雨天气。由极地冷气团和副热带暖气团在这一带交绥所致。因空气潮湿 ，衣物容易发霉 ，又时值梅子黄熟，故称梅雨，又称霉雨和黄梅雨。梅雨时日又称黄梅天、黄梅季。由于各年冷暖气流的强弱和进退迟早不同，梅雨期出现的早晚、长短和雨量的多寡变化较大。梅雨适时适量有利于农作物生长；若雨期过长或过短，雨量过多或过少，则可引起旱涝灾害。 |
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