高原季风,plateau monsoon英语短句,例句大全

高原季风,plateau monsoon
1)plateau monsoon高原季风
1.Analysis shows that the Asian monsoon system can be categorized into three relatively independent sub-systems,including South Asian monsoon,East Asian monsoon,and plateau monsoon.亚洲季风系统中存在着3个相对独立的子系统:南亚季风、东亚季风和高原季风。
2.By using NCEP/NCAR data from May to June 1958—1999, compositing and comparing methods, the anomaly circulations of QinghaiXizang Plateau monsoon and East Asian monsoon are analyzed.利用NCEP/NCAR1958—1999年5～6月各标准等压面层网格点资料,采用合成法和对比分析等方法,对初夏青藏高原季风和东亚季风环流异常进行了分析。

英文短句/例句

1.The relationships between Plateau Monsoon and 500 hPa Westerly Activities In Mid-latitude高原季风对500hPa中纬度西风带活动的影响
2.Relationship between a New Plateau Monsoon Index and Summer Precipitation in Sichuan Basin and Analysis of Circulation Features一个新的高原季风指数与四川盆地夏季降水的关系
3.Analysis of linkage between NDVI variability in Tibetan Plateau and South Asian summer monsoon青藏高原冬季植被变化与南亚夏季风关系分析
4.The Definition of Plateau Summer Monsoon Index and Analysis on Its Characteristics高原夏季风指数的定义及其特征分析
5.The Holocene East Asian Monsoon Record from Tenger Nuur of Monsoon Boundary in the Southern Mongolia Plateau;蒙古高原南部季风边缘区腾格淖尔记录的全新世东亚季风变化
6.Seasonal and Interannual Variability of the Pre-monsoon Circulation to the South of Tibetan Plateau in Spring and Relation between Pre-monsoon Circulation and East Asian Summer Monsoon;春季青藏高原南侧前季风环流圈的季节和年际变化及与东亚夏季风的关系
7.THE INFLUENCE OF ANOMALOUS DIABATIC HEATING OVER TIBETAN PLATEAU IN SPRING ON THE ASIAN TROPICAL CIRCULATION AND MONSOON ONSET春季青藏高原加热异常对亚洲热带环流和季风爆发的影响
8.Variation of Winter Temperature in China and Its Responding to the Anomalies in East Asian Winter Monsoon and Surface Heating Field over Qinghai-Xizang Plateau我国冬季气温异常对东亚季风和高原加热场的响应
9.A Study on Monsoon Circulations of Drought and Wet Years on the East Side of Qinghai-Xizang Plateau in Early Summer青藏高原东侧初夏旱涝的季风环流分析
10.Study on the Relationship between Frozen-thaw Process over Qinghai-Tibet Plateau and East Asian Summer Monsoon;青藏高原冻融过程与东亚夏季风关系的研究
11.Seeks: Explodes a gap the Himalaya Mountains to let the Indian Ocean warm wet monsoon blow the Qinghai-Tibet Plain.牟：把喜马拉雅山炸个缺口让印度洋暖湿季风吹进青藏高原。
12.Influences of Snow Cover over the Tibetan Plateau on Asian Summer Monsoon青藏高原积雪对亚洲夏季风影响的诊断及数值研究
13.Lake sediments responded for the ancient monsoonal change of the late Quaternary Period in the Inland of Qinghai-Xizang Plateau;青藏高原腹地湖泊沉积对第四纪晚期古季风变化的响应
14.EVOLUTION OF THE SOUTHWEST MONSOON ON ORBITAL TIME-SCALE REVEALED BY A LOESS-PALEOSOL SEQUENCE ON THE SOUTHEASTERN MARGIN OF THE QINGHAI-TIBETAN PLATEAU FOR THE LAST 1.16 Ma青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化
15.Late Quaternary Weathering and Erosion of the Eastern Tibetan Plateau and the Mekong Basin and East Asian Monsoon Evolution Recorded by the Sediments from the South China Sea青藏高原东部和湄公河盆地晚第四纪风化剥蚀与东亚季风演化在南海中的记录
16.Correlation between Indian Ocean Summer Monsoon and Stable Carbon Isotopic Composition from Mono-species Plant Cellulose in the Holocene;单种属泥炭纤维素碳稳定同位素组成与全新世青藏高原东部西南季风变化
17.Role of Western Pacific Ocean-Indian Ocean-Tibetan Plateau Climate System in the South China Sea Summer Monsoon;西太平洋—印度洋—青藏高原气候系统在南海夏季风爆发过程中的作用
18.Process of monsoon variations of the northeastern Qinghai-Xizang Plateau from the loess record of Lonxi Basin since the last interglacial epoch;陇西黄土沉积记录反映的末次间冰期以来青藏高原东北部季风的演化过程

相关短句/例句

Plateau-Monsoon高原-季风
3)Plateau summer monsoon高原夏季风
1.(1) The Plateau summer monsoon characteristics calculated by PMI of 1997 and 1998 show that: Its strength is very different in the different phases,so this paper divide it to three phases(intensive and permanent and weakly days)and discussing it s.采用1996—2005年NCEP/NCAR 600 hPa逐日再分析资料,利用高原季风指数定义和波包传播的诊断方法(WPD),研究了高原夏季风强弱年(1998年和1997年)不同发展阶段的波包传播特征。
4)plateau monsoon system高原季风系统
5)Plateau monsoon index(PMI)高原季风指数
1.Using the daily NCEP/NCAR reanalysis of 600 hPa geopotential height field from 1996 to 2005 and the concept of Plateau monsoon index(PMI) and method of WPD investigate the different wave-packet characteristics in different stages of the strong/weak(1998/1997) year.采用1996—2005年NCEP/NCAR 600 hPa逐日再分析资料,利用高原季风指数定义和波包传播的诊断方法(WPD),研究了高原夏季风强弱年(1998年和1997年)不同发展阶段的波包传播特征。
6)Altitude higher area summer Season高原夏季