Yao Tandong. The Dynamic Feature in Middle of the Qinghai-Xizang Plateau [M]. Beijing: Geology Press, 2002.
[姚檀栋。青藏高原中部冰冻圈动态特征[M]。北京：地质出版社，2002。]。
The uplifting of the Qinghai-Xizang Plateau has exerted great influence on regional differentiation of physical environments in West China.
近几百万年以来青藏高原的强烈隆升对中国西部地区自然环境地域分异的影响十分明显。
Wei Zhigang, Lü Shihua. 1995. Distribution of snow cover on the Qinghai-Xizang Plateau and its effect on surface albedo[J]. Plateau Meteor, 14(1):67-73.
韦志刚，吕世华.1995。青藏高原积雪的分布特征及其对地面反照率的影响[J]。高原气象，14（1）：67-73。
Completely different characteristics of pollen spectra are shown by the pollen records from the Southeast and the northwest of the Qinghai-Xizang Plateau.
全新世青藏高原的花粉记录，反映高原东南部和西北部截然不同的孢粉类型。
The Qiangtang Basin in the hinterland of the Qinghai-Xizang Plateau is interpreted as a reworked basin which has undergone multiple phases of tectonic reworking.
位于青藏高原腹地的羌塘盆地是经历了多期构造改造的改造型盆地。
Further analyses show the variation of earth rotation rate and sunspot cycle length have important role on the climate abrupt change in the Qinghai-Xizang Plateau.
进一步分析表明，地球自转速度和太阳黑子周期长度的变化对高原及北半球本世纪气候的突变和阶段性变化起着重要的作用。
The mass of the Qinghai-Xizang plateau is shortening in north-south and extending in east-west, and in the meanwhile there is evidently eastward side strike of some substance;
青藏高原主体在南北向缩短、东西向延伸的同时存在着明显向东的物质侧向滑移；
There are close relations between the losses of total ozone in spring and summer and the uplift of the second tropopause height in summer over the Qinghai-Xizang Plateau in recent 30 years.
近30年春、夏季高原臭氧总量亏损与夏季高原第二对流层顶高度的抬升存在着密切关系。
So a concept model has been get up by above research, this model explain that how the thermal in the Qinghai-Xizang Plateau effects on the water level in Qinghai Lake through basin climate change.
建立了青藏高原热力作用和气候变化的关系及其对青海湖水位下降趋缓(年际差增大)的概念模型。
The landforms evolvement of the Three Rivers Flow Area has relationship with the stagical rise of the Qinghai-Xizang plateau, and it respects to the landforms evolvement of the South and East Asia.
三江并流地带的地貌演化与青藏高原的阶段性隆升有关，而且与东南亚地貌演化关系也较为密切。
A strong cold wave entering Qinghai-Xizang Plateau during 8-10 January of 1983 is analys. Ed by the isentropic potential vorticity (IPV) maps.
用等熵位涡(IPV)图分析了1983年1月8—10日侵入青藏高原的一次较强冷空气过程。
This paper gives a brief account, of the principle, performance and usage of the three-component flux-gate magnetometer for electromagnetic deep sounding in Qinghai-Xizang plateau.
本文概述了为青藏科考大地电磁测深工作研制的三分量磁饱和式磁力仪的原理、性能、用途和野外使用情况。
Therefore, the changes of moisture and heat from frozen-thaw process in Qinghai-Xizang Plateau is an important outside heat source, which influences East Asia climate.
由此，青藏高原季节冻融过程引起的水热变化是影响东亚气候的一个重要外源。
Using the data of natural earthquakes, we have studied the characteristics of P-wave travel time in Qinghai-Xizang plateau and its vicinity.
本文利用天然地震资料，研究了青藏高原及其邻区的P波走时特征。
Dulong River watershed is situated in the northwest of Yunnan Province, and neighbors with Qinghai-Xizang Plateau and India in the north, neighboring with Burma in the west.
独龙江流域位于云南省的西北部，北与青藏高原相连，西与缅甸毗邻。
The physical factor fields and the behavial law of mesoscale geographical convergence over the northeast of Qinghai-Xizang Plateau are analysed.
青藏高原东北侧存在着中尺度地形绕流辐合现象。
Based on analysis, vegetation and distribution in Qinghai Lake region has a special pattern and coincides with the climate trends to colder and droughter with the uplift of Qinghai-Xizang Plateau.
植被东西方向的水平地带性并未表现出明显的过渡特征。根据植被特点及分布规律分析，本区植被有其自身的特殊性，并与青藏高原隆升之后气候寒冷干旱相一致。
Wang Zhiyuan. 2012. The formation mechanism analyses of a regional heavy rain on the northeast of Qinghai-Xizang Plateau [J]. J Qinghai Meteor, (4) : 2-6.
王志远。2012。青藏高原东北部一次区域性暴雨天气形成机理分析[J]。青海气象，(4)：2 - 6。
Wang Zhiyuan. 2012. The formation mechanism analyses of a regional heavy rain on the northeast of Qinghai-Xizang Plateau [J]. J Qinghai Meteor, (4) : 2-6.
王志远。2012。青藏高原东北部一次区域性暴雨天气形成机理分析[J]。青海气象，(4)：2 - 6。
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