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The geographical environment elements to form weather disasters in yunnan include low latitude plateau,approaching tropical oceans,complicated topographical features,cliffy mountain,few vegetation,concentrated rainfall,complicated geological structure and strong fault actions.

由于云南复杂的低纬高原地理环境,多样的局地气候背景,特殊的地貌植被状况以及同时受东亚、南亚两支季风的共同作用,形成了鲜明的区域气象灾害特征[1,2]。1 云南气象灾害的特征1.1 种类多、频率高、重叠交错云南自然地理环境特殊,7种气候带交错分布,气候资源丰富,立体气候明显,地域差异大。

Those four classification models work well in first class of Chinese Vegetaion Division. The KAPPA value of Holdridge Life Zone System,at high value of 0.57,would probably more effective than the others. But in specific area,like tibetan plateau,all of those models need to be refined or consider more elements and factors. This research also points out that the concept and technology of Digitall Earth would promote and push forward the climate-vegetation relationship research,especially in climate-vegetation factors,climatically parameters and modeling parameters,real time dynamic monitoring,effectively managing the magnitude data of climate-vegetation relationship information and supporting the mainframe of Functional Types Modeling Library.

这四个传统的分类方法在中国植被区划一级分类上是适用的,Holdridge生命地带系统KAPPA一致性指数达到0.57模拟效果优于其它三者,但在特定地区,如青藏高原,所有模型均需改进优化或启用新的模型因子才能很好地区分植被亚地带,本研究还指出,数字地球技术的应用有助于推动气候—植被关系的研究,尤其在气候—植被指标的大范围实的动态监测、气候—植被关系数据的海量信息高效、有序基础管理和功能模型库支撑框架体系方面。

To explore the climatic implication of compound-specific hydrogen isotope ratios of sedimentary n-alkanes, the author sampled shallow sediment cores respectively from the climatically and environmentally distinct basins Qiangyong Glacier Lake,Kongmu Co Lake,Nam Co Lake, Keluke Lake and Xiao Qaidam Lake along a S-N transect on the Tibetan Plateau for the extraction and analysis of these biomarkers.

本文分别在青藏高原南部的大枪勇错、空姆错,中部的纳木错以及东北部的克鲁克湖和小柴达木湖钻取了浅岩芯,通过对沉积物中正构烷烃的提取分析和单体氢同位素比值的测定来探讨该类生物标志物单体δD值的气候指示意义。

The compressional wave velocities and electrical conductivity in some crustal rocks collected from Tibet Plateau are measured under the conditions of high temperature and high pressure.

在高温高压条件下研究了地壳岩石的纵波速度和电导率变化特征。

The mother always loves to copy that big river of to concuss;torrent at Mongolia plateau my faraway home town.

母亲总爱描摹那大河浩荡;奔流在蒙古高原我遥远的家乡。

The Tibetan Plateau isostatically uplifted after contractional shortening and crustal thickening in Paleogene and is dominated by strike-slip and extension in Late Cenozoic.

青藏高原经过古近纪挤压缩短和增厚地壳均衡隆升,晚新生代形成了以走滑和伸展为主的相对稳定构造环境。

The Tibetan Plateau isostatically uplifted after contractional shortening and crustal thickening in Paleogene and is dominated by strikeslip and extension in Late Cenozoic.

青藏高原经过古近纪挤压缩短和增厚地壳均衡隆升,晚新生代形成了以走滑和伸展为主的相对稳定构造环境。

The prediction shows that the total yield in the corrasive region of Loess Plateau in 2010 will reach 1400.71×10^4t. The demand of grain based on the three levels (400kg, 425kg or 450kg/person) will be respectively 1389.34×10^4t, 1470.37×10^4t and 1563.01×10^4t.

3粮食需求预测表明,2010年黄土高原水土流失区粮食总量将达1400.71×10^4t,在人均400kg×10^4t,在人均400kg, 425k和450kg水平下粮食需求分别为1389.34×10^4t, 470.37×10^4t和1563.01×10^4t。

In Project A, grain shortage will not appear in the corrasive region of Loess Plateau on the whole. But in order to achieve an equilibrium of demand and supply, loess hill regions must import grain from the Loess Platform region.

从A方案看,就黄土高原水土流失区整体而言将不会出现粮食短缺;但具体到分区而言,黄土丘陵区必须通过粮食调入才能满足本区需求,而黄土台塬区则有一定盈余。

Cosmogenic isotopes 〓Be was used to date the glacial geomorphic surface of Qinghai-Xizang Plateau in this paper.

本文应用宇生核素〓Be对青藏高原冰川地貌面的年代进行计算。

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