雅鲁藏布江

雅鲁藏布江河谷风沙地貌分类体系由4级21个类型组成，其中风积地貌划分为谷底与谷坡风积地貌2个亚类。

Aeolian sand landform in the Yarlung Zangbo river valley can be divided into 4 classes and 21 types , among them , aeolian deposition form can be further divided into two sub types at valley bottom and at valley slop .

雅鲁藏布江航磁异常带性质及其意义

The property of the Yarlung Zangbo River aeromagnetic anomaly zone and its significance

高原上最频繁的对流区在以30°N，90°E为中心的地区，而不在高原东部，而且喇叭口形的雅鲁藏布江出口区是一个小值区。

The most frequent convective region over the Plateau is centered at 30 ° N , 90 ° E , not in the eastern Plateau .

基于HHT变换的雅鲁藏布江径流多时间尺度分析

Multi-temporal Scales Analysis of Runoff Series in Yarlung Zangbo River Based on Hilbert-Huang Transform

雅鲁藏布江主洋盆演化可分为4个阶段：（1）裂谷起始阶段（P2）；

The evolution of Yarlung-Zangbo main Ocean can be divided into four stages : ( 1 ) Rifting stage ( P2 ) .

文中用NOAA数据、DEM数据结合实测气象数据对Penman公式进行修正，再用修正后的Penman公式计算雅鲁藏布江流域潜在蒸散量。

NOAA / AVHRR and DEM ( Digital Elevation Model ) together with the measured meteorological data are applied to modify Penman Formula . And the monthly potential evapotranspiration of Yarlung Tsangpo River Basin is calculated with the modified Penman Formula .

雅鲁藏布江流域地-气系统的水平衡

Water Balance in Land-Atmospheric System over the Yalu Tsangpo River Basin

雅鲁藏布江流域潜在蒸散量计算方法

Method for computation of potential evapotranspiration in Yarlung Tsangpo River Basin

雅鲁藏布江河谷黄土的沉积特征及成因

Deposition Features and Causes of Loess in Yarlung Zangbo River Valley Area

雅鲁藏布江断裂带附近地应力场的变化特征

Variety characteristics of the crustal stress field near the Brahmaputra fault zone

雅鲁藏布江断裂带的形成

On the formation of Yarlung Zangbo River Fault Zone

雅鲁藏布江下游地区地质构造特征

A preliminary note on the tectonic features of the lower YALU-TSANGPO River Region

雅鲁藏布江以南的所有人以前都是猎首者。

All the people living south of the Brahmaputra River were formerly headhunters .

雅鲁藏布江形成了印度的布拉马普特拉河

The Yarlung , which becomes India 's Brahmaputra ,

雅鲁藏布江中游高山鸟类对绢毛蔷薇种子传播的影响

Effects of Alpine birds on Seed Dispersal of Rosa Sericea in the Mid-Brahmaputra River

雅鲁藏布江断裂是印度板块与欧亚板块缝合线的置疑

Is the Yarlung Zangbo fault zone the suture between the Indian and Eurasian plates

雅鲁藏布江的上游是高寒地带。

The upper reaches of the Yarlung Zangbo River lie in a frigid zone .

雅鲁藏布江从山峦间穿过形成了世界最深的峡谷

As the Yarlung River cuts through the mountains , it 's created the world 's

雅鲁藏布江流域土地沙漠化现状与成因初步研究&兼论人为因素在沙漠化中的作用

Tentative study on the status and the causes of desertification in Yarlung Zangbo River Basin

贡噶雅鲁藏布江大桥简支转连续梁的设计与施工

Design and Constructing in Transforming Simple Supported into Continuous System on Brahmaputra River Bridge in Gongga

雅鲁藏布江缝合带及其邻区构造演化

On the tectonic evolution of the Yarlung Zangbo ( Tsangpo ) suture zone and its adjacent areas

雅鲁藏布江常年水温较低和营养盐缺乏，导致水生生物生物量较低。

Aquatic organism biomass were low because of low temperature and lack nutrients in Yarlung Zangbo River .

雅鲁藏布江两岸风成沙覆盖区地球化学找矿方法及效果

On a Geochemistry Method of Hunting for Ores in the Banks of Yarlung Zangbo River Covering with Eolian Sand

恒河-雅鲁藏布江流域雪线场的建立及其环境意义

The Field of Equilibrium Line Altitude in the Ganga - Yarlung Zangbo Rivers System : Establishment and Its Environmental Significance

总之，雅鲁藏布江河谷地区特殊的地形和地貌以及与其他热带地区的地理隔离是造成丝须蒟蒻薯在这一地区遗传多样性极低的可能原因。

The extremely low genetic diversity in Brahmaputra populations was probably due to the unique landforms and vicariance of the Brahmaputra valley .

泽当蛇绿混杂宕是雅鲁藏布江蛇绿岩带重要组成部分，受控于板块结合带。

The Zetang ophiolitic melange is an important component part of the Yarlung Zangboophiolite belt and controlled by the plate junction zone .

板块汇聚带的造山和重力垮塌作用及其力学成因：以雅鲁藏布江-喜马拉雅山汇聚带为例

Orogeny and gravitational collapse along the convergent plate boundary and their mechanical origin : a case study on the Yarlung Tsangpo-Himalaya belt

在雅鲁藏布江、拉萨河与年楚河流域中部地区人为因子致使生态退化作用较强。

The artificial factor in the middle area of brahmaputra , Lhasa River and Nianchu River induced relatively strong ecological degradation action .

雅鲁藏布江源头区的植被及其地理分布特征黄河源头区土壤侵蚀现状分析

Vegetation Types and Their Geographic Distribution in the Source Area of the Yarlung Zangbo Soil Erosion Analysis in Headstream Basin of Yellow River

降水变化是雅鲁藏布江天然径流最主要的影响因子，降水变化在一定程度上控制着河川径流的演变规律。

Precipitation change was the most important factor of the natural runoff , controlled the evolution of river runoff to a certain degree .