| 1. | Characteristics of winter atmospheric teleconnection patterns in northern hemisphere and their effects on climate in china
北半球冬季大气环流遥相关型特征与我国区域气候 |
| 2. | We divided the global june - august precipitation field into 34 subareas and pointed out that there exists evident teleconnection among the june - august precipitation in these subareas
用reof方法将全球陆地6 - 8月降水场分成34个大尺度降水分区。 |
| 3. | There is teleconnection relations between shandong summer rainfall and the convective activities happening in tropical areas in spring and summer accomplished by rossby waves
通过分析强弱季风年春、夏季热带地区olr场的分布特征，发现热带地区的对流活动与山东夏季降水之间存在着遥相关关系。 |
| 4. | 3 ) the teleconnection between winter sst of north pacific and summer precipitation is the areas of equator east pacific and black current with the areas of middle and lower reaches of yangtze river and hetao
3 )冬季太平洋sst与我国东部夏季极端降水量的遥相关型主要表现在，赤道东太平洋及黑潮海域的冬季海温与长江中下游地区和河套地区的遥相关型。 |
| 5. | This paper is concerned with the time - spatial characteristics of summer extreme precipitation over eastern china and with the teleconnection between summer extreme precipitation and sst of the north pacific and soi , based on the daily rainfall data of 59 stations from 1951 to 2000
本文利用我国东部( 105e ~ 0以东) 59个测站1951 - 2000年的夏季逐日降水资料对我国东部夏季降水极值的时空特征及其与北太平洋海温和南方涛动指数( soi )的遥相关进行研究。 |
| 6. | Longitude circulations exist in the soohpa height fields in wet . springs and latitude circulations exist in dry springs . the composite : differences of the atmospheric circulation exist in wet springs and dry springs , which appears to be the eu teleconnection pattern of the general circulation
结果表明，山东省春季涝年与旱年的环流形势存在明显的差异：异常多雨年，贝加尔湖以西的广大中高纬地区高度场降低，我国东部到日本的高度场明显升高，亚洲中高纬地区呈现纬向环流。 |
| 7. | Results show , 1 ) the teleconnection between extreme precipitation of ease china and the same season sst of north pacific is mainly in nino area ( nino 1 - 2 area most ) ; the plus connection area between nino1 area and the next summer extreme precipitation is in middle and lower reaches of yangtze river
结果表明， 1 )我国东部夏季极端降水量空间分布与同期太平洋sst的遥相关型主要集中在整个nino海区(以nino1 - 2区为最) ； nino1区与次年夏季极端降水量的相关主要表现在与长江中下游区的正相关型。 |
| 8. | Based on the empirical orthogonal function ( eof ) , the characteristics of large scale variations of precipitation anomaly during rainy season ( from jun to aug ) in south - west china for the period 1961 1995 is analyzed , and the teleconnection distribution charac - teristics between sea surface temperature ( sst ) over india ocean and precipitation during rainy season in south - west china were studied by using the method of cca
用自然正交函数展开方法对1961 1995年西南汛期( 6 8月)降水大尺度变化特征进行分析，并在此基础上用典型相关分析方法研究了1 8月印度洋海温距平场与西南汛期降水场的遥相关分布特征。 |
| 9. | As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
结果发现当黑潮海温冷异常时，后期夏季大陆热低压加深，东亚夏季风偏强。中纬度阻塞高压减弱，东亚地区纬向环流发展，在东亚-西太平洋地区激发“ - + - ”的东亚遥相关型，从而西太平洋副高强度偏弱，面积偏小，位置偏东、偏北，东亚梅雨锋也偏弱，季风槽则变强，位置偏北。同时南亚高压偏弱，位置偏北、偏东，易形成东部型。 |
| 10. | The positive and negative anomaly centers at 500hpa level formed the anomaly " wave train " from lower latitude to higher latitude over east asia . the teleconnection pattern called east asia - pacific pattern ( eap ) plays important roles in the summer rainfall in shandong area . study shows that weaker okhotsk sea high , northward location of subtropical high and stronger indian low , are likely to lead to more rain in shandong province in summer
分析对比旱涝年不同层次高度场以及高低层散度场，结果发现，在春夏季旱涝年，高度场几个主要的距平中心以及115 130 e区域高( 200hpa )低( 925hpa )层散度场基本呈现出反位相分布特征，北半球夏季存在的东亚-太平洋遥相关型( eap型)对山东夏季降水产生重要影响。 |
