梅雨

主要结果如下：（1）外植体采摘最佳时间为4-9月份（避开梅雨季节）。

The results were as follows : ( 1 ) April to September ( avoiding the mould rains season ) was the best period to pick the explants .

用模糊优先比预报梅雨年型

The method for forecasting plum rains by fuzzy preference ratio

梅雨季节东西容易发霉。

Things easily get mildewed in the rainy season .

应用湿Q矢量诊断梅雨锋暴雨

Using the Wet Q-vector to Diagnose a Process of Meiyu Front Heavy Rain

梅雨锋暴雨的Q矢量定性分析

Qualitative comparison and analysis of q - vector

一次梅雨锋暴雨过程Q1和Q2的结构

The structure of q_1 and q_2 during a heavy rain process on the Meiyu front

2007年湖北省梅雨期可降水量的GPS观测和分析

Investigation and analysis by global positioning system on precipitable water vapor during Meiyu period of 2007 year in Hubei Province

梅雨锋暴雨的Doppler雷达观测研究：边界层中尺度涡旋系统

A study of rain gushin the Mei Yu front with Doppler radar observations : mesoscale vortex system in the boundary layer

与南区梅雨期降水耦合正相关的南海和赤道东太平洋关键区海温异常分布实际上属于同一种海温分布型，但两个海温Key区所影响到的南区的范围是不相同的。

In fact , the two SST distributions mentioned above belong to the same SST distribution pattern , but the regions influenced by the two SST distribution are different from each other .

2002年6月21-23日梅雨锋上的MCS分析

Analysis of MCS developed along Mei-yii front during June 21 to 23 , 2003

AW模式对梅雨暴雨的预报试验

Predicting Experiments of Heavy Rainfall During Mei-Rain Season with AW Model

梅雨异常年份的东半球中低纬环流特征Java中的异常处理

Some characteristics of circulation over middle and low latitudes of eastern hemisphere during anomalous droughts and floods in 1981 and 1983 how to handle the exception in Java

江淮梅雨期降水不同尺度异常与SSTA的关系

Relationships between Different Multi-time Scales of Anomalous Precipitation in Jiang-Huai Mei-yu and SSTA

梅雨锋上MCS的发展、传播和CISK惯性重力波

Evolution and Propagation of the MCSs over Meiyu Fronts and Inertia-gravitational Wave-CISK

一次梅雨锋上MCS云微物理过程及降水形成机制

Study on cloud micro-physical processes and precipitation formative mechanisms of a mesoscale convective system in Meiyu front in June 2004

位势不稳定和条件性对称不稳定共存使得在θe高值区域的垂直上升运动和在θe面（梅雨锋区）上的斜上升运动得以产生和维持。

Potential instability that exists with conditional symmetrical stability make the vertical ascend movement in θ e big value area and slope ascend movement in θ e surface ( Meiyu front area ) produce and maintain .

梅雨锋上MCS的发展、传播以及与低层湿度锋相关联的CISK惯性重力波

Evolution and Propagation of MCSs over Meiyu Fronts and Inertia-Gravitational Wave-CISK Related to " Low-level Moisture Frontal Zone "

使用1998年夏季高分辨率的GAME再分析资料，通过计算热量和水汽收支，分析了江准梅雨的热力和动力特征。

By using the high-resolution GAME reanalysis data , the heat and moisture budgets during the period of HUBEX / GAME in the summer of 1998 are calculated for exploring the thermodynamic features of Meiyu over the Changjiang-Huaihe ( CH ) valley .

本论文的主要目的就是基于前人的研究成果及方法，研究江淮梅雨期的MCV。

The aim of this thesis is to investigate the MCV in mei-yu season based on the former researches and methods .

从湿Q矢量散度辐合场这个角度探讨了梅雨锋暴雨的内在机理，并给出了梅雨锋暴雨具体预报的新思路。

Based on the convergence field of wet Q-vector divergence , the intrinsic mechanism of Meiyu front heavy rain is discussed , and a new thinking for the forecast of Meiyu front heavy rain is given .

利用EOF和小波变换方法讨论了长江流域梅雨期降水的多时空尺度特征。

The multiple temporal and spatial scale characteristics of rainfall over the Yangtze River valley during the Meiyu period is studied by EOF and wavelet analysis .

其中20世纪70年代中期PDO出现暖位相增强的突变，长江中下游梅雨也在此时期转入增多的趋势。

When PDO occurred abrupt warming in meddle of 1970s in 20 century , the trend of the Meiyu enhanced than previous period .

与低层湿度锋耦合的带状CISK和暖切变型梅雨锋的产生

The Band of CISK Coupled with Low Level Moisture Fronts and the Genesis of Warm Shear Line-Type Meiyu Fronts

韩国现在已酷暑难当，但初夏的梅雨却没有如约而至。据韩国气象厅（KoreaMetrologicalAdministration）说，韩国今年5月初以来的降雨量创下1908年以来的同期最低水平。

Sizzling hot summer weather has arrived in South Korea , but the early summer rains have yet to come . According to the Korea Metrological Administration , rainfall since the beginning of May has been the lowest since 1908 .

分析了春季北极涛动（AO）指数的变化对梅雨ChangmaBaiu带夏季降水年际变化的影响。

The influence of spring Arctic Oscillation ( AO ) on the summer rainfall over Meiyu Changma Baiu regions is analyzed .

应用准静止卫星水汽图像导出的风（简称为水汽风）分析东亚梅雨锋云带内中尺度对流系统（MCS）在对流层上层的流出通道。

Winds obtained by tracking features in satellite water vapor imagery have been used to analyze the upper level outflow in the vicinity of mesoscale convection systems ( MCS ) along the Meiyu front .

关键区（143°E-160°E，27°N-39°N）10-11月海温与次年江淮南区梅雨期气温日较差存在较好的反相关关系。

There is a apparent negative correlation between the temperature daily range in south area of Changjiang-huaihe valley over Meiyu period and SSTA in the Key region ( 143 ° E 160 ° E , 27 ° N 39 ° N ) from November to December in former year .

为了验证VPP的结果，进行了模拟及实例反演，文中给出了两个反演实例，第一实例为梅雨锋过程，第二个为中尺度雹暴过程。

We validate VPP by experimental and real instance , the first is mei yu front process and the second is mesoscale hail storm .

在整个梅雨锋暴雨过程中，500hPa高度上的Qq矢量散度辐合场的辐合强度及其辐合中心位置对同时刻的降水强度及雨区位置有非常好的指示作用；

Throughout the Meiyu front rainstorm process , the convergence intensity and center of 500 hPa Qq divergence field are good indicators for the intensity and location of precipitation ;

FSW类型则主要受到梅雨锋面及西南气流影响，从风场分布可明显观察到沿著梅雨锋面的东南及西北侧皆有数个反气旋环流系统排列，使得锋面处的风切更为增强。

From the wind field , we can find that a series of anti-cyclones located to the southeastern and the northwestern sides along the Mei-Yu front , which make the frontal wind shear even enhanced .