1.
Simulation of air temperature and precipitation over Qinghai-Xizang Plateau with RegCM3 model
RegCM3模式对青藏高原温度和降水的模拟及检验
2.
Studies on the Characters of Air Temperature over the Tibetan Plateau in the Globe Climatic Background in Recent 50 Years;
近50年全球气候背景下青藏高原温度变化特征分析
3.
Primary Analyses of Teleconnection Relationship between the Qinghai-Xizang Plateau Air Temperature and the Indian Ocean SST
青藏高原气温与印度洋海温遥相关的初步研究
4.
Seed germination responses of Hippophae neurocarpa endemic to the Qinghai-Tibetan Plateau to temperature
青藏高原特有植物肋果沙棘种子萌发对不同温度的响应
5.
Eurasian temperature-Loess plateau-Qingzang plateau element is 23 species(10.6%);
欧亚温带—黄土高原—青藏高原成分23种,占10.6%;
6.
RELATIONSHIP BETWEEN SURFACE TEMPERATURE DISTRIBUTION CHARACTERISTICS OF TIBETAN PLATEAU AND SEA SURFACE TEMPERATURE (SST) OF TROPICS AND SOUTHERN OSCILLATION
青藏高原地面气温的分布特征及其与南方涛动、热带有关海域海表温度的关系
7.
Comparison of NCEP/NCAR Reanalysis Data and Radiosonde Data about Temperature and Geopotential Height of Upper Air over the Tibetan Plateau
青藏高原地区上空NCEP/NCAR再分析温度和位势高度资料与观测资料的比较分析
8.
Variation of Summer Air Temperature on the East Side of Qinghai-Xizang Plateau and Its Probable Causes
青藏高原东侧地区夏季气温变化及其可能成因
9.
Study on the Temporal and Spatial Characters of Air Temperature Variation on Qinghai-Xizang Plateau During the Period of Using Instruments;
器测时期青藏高原气温变化的时空规律研究
10.
Analyses on Variety Characteristics of Temperature in Qinghai-Tibet Plateau in Recent 50 Years;
青藏高原近50年来气温变化特征的研究
11.
Simulation of Summer Air Temperature and Precipitation over Tibetan Plateau with Regional Climate Model(RegCM3)
RegCM3模式对青藏高原夏季气温和降水的模拟
12.
Anomaly Features of Temperature over Qinghai-Xizang Plateau in Summer and Pacific SSTA in Winter and Its Correlation Analysis
夏季青藏高原气温与冬季北太平洋海温的异常特征及其相关分析
13.
Analysis on the Topographic Gradient and Geographical Meaning of Mt.Konggur,in the Northern Edge of Qinghai-Tibet Plateau
青藏高原北缘公格尔山地区地形梯度的剖析
14.
The Moho Depth of Qinghai-Tibet Plateau Revealed by Seismic Detection
由地震探测揭示的青藏高原莫霍面深度
15.
Assessment of Land Degradation on Qinghai-Tebet Plateau
青藏高原土地退化类型及其退化程度评价
16.
Because of its high elevation, the Qinghai-Tibet Plateau area, a special alpine-cold zone, has low temperatures all year round.
西南的青藏高原全年气温较低，是中国特殊的高寒地区。
17.
Periodic fluctuation features of air temperature,precipitation,and aboveground net primary production of alpine meadow ecosystem on Qinghai-Tibetan Plateau
青藏高原高寒草甸气温、降水和地上净初级生产力变化的周期特征
18.
REVEALING THE MYSTERIES OF THE QINGHAI-XIZANG (TIBET) PLATEAU-BRIEF REVIEW ON“THE GEOLOGICAL EVOLUTION OF TIBET”--REPORT OF THE 1985 ROYAL SOCIETY-ACADEMIA SINICA GEO TRAVERSE OF THE QINGHAI-XIZANG PLATEAU
揭开青藏高原的奥秘——简评《青藏高原地质演化》