1) Zayu River
察隅河上游
1.
Status and Conservation of Large and Medium-sized Mammals in the Upper Zayu River Basin;
藏东南察隅河上游流域大中型兽类动物资源现状和保护
2) Zayü Qu
察隅河
3) Chayu
察隅
1.
Application of Jiaduo Frequency Trembler Grid Lamps in the monitor and control of forest pest insects in Chayu County,Tibet Autonomous Region;
佳多频振式杀虫灯在察隅地区森林害虫监测防治试验中的应用
4) Upper Yellow River
黄河上游
1.
Effects of Upper Yellow River Pollution on Antioxidant Enzymes Activities and Malondialdehyde Content of Bufo raddei;
黄河上游环境污染对花背蟾蜍抗氧化酶活性及丙二醛含量的影响
2.
Reconstruction of recent 522-year runoff series on Upper Yellow River and analysis on its variation trend;
黄河上游近522年径流量序列重建及其变化趋势分析
3.
Climate variation in upper Yellow River in 1990s and its influences on inflow of Longyangxia Reservoir;
近期黄河上游气候变化对龙羊峡入库水量的影响
5) upper reaches of the Yellow River
黄河上游
1.
For the severe situation of eco-unbalance in the upper reaches of the Yellow River, the study of function for soil and water conservation in rehabilitated lands not only has the theoretical values, but has the urgent need for practice.
面对黄河上游地区生态失衡的严重现实,作为植被恢复重建重要手段的退耕还林还草工程,其水保功能研究不仅具有理论价值,而且有十分迫切的实践需要。
2.
Based on field geological investigations of avalanches,landslides and mudflows in the upper reaches of the Yellow River,the authors determined the main influence factors and index system of the hazard risk evaluation and made risk evaluation with the county(city or qi)as a unit.
本文在对黄河上游地区崩塌、滑坡、泥石流进行野外地质调查和资料收集的基础上,确定了灾害风险评价的主要影响要素和指标体系,进行了以县(市、旗)为单元的风险评价。
3.
They are located among high mountains and gorges in upper reaches of the Yellow River.
黄河上游水流湍急,水量丰沛。
6) the upper reaches of the Fenhe River
汾河上游
1.
The relationship between population pressure growth and environmental change in recent 600 years in the upper reaches of the Fenhe River;
六百年来汾河上游人口压力增长与环境状态演变之关系
补充资料：察隅河
西藏东部大河之一，属双干河流。发源于德母拉山，源头海拔5475米,全长295公里，流域面积1.7827万平方公里。岗日嘎布山将察隅河上段分为两支：东支察隅河主流桑曲,长178公里,流域面积6780平方公里,落差4785米，自源头德母拉开始自西北向南东流，至竹瓦根转向南流，经察隅折向西南到下察隅与西支贡日嘎布曲汇合；贡日嘎布曲发源于岗日嘎布拉附近的现代冰川，自西北向东南流，长170公里，落差3000米,流域面积5376平方公里。桑曲和贡日嘎布曲汇合后称察隅河，向南流至前门里的巴兰岗附近流入印度，转向西南汇入布拉马普特拉河。察隅河流域属高山峡谷地貌，从源头到白学为峡谷段；白学到此坝桥为宽窄相间的河谷段，滑坡、崩塌、泥石流发育；此坝桥至零零通山嘴为交错的峡谷段。察隅河流域气候温暖湿润，降水丰沛，森林、动植物、水利等自然资源丰富，农业发达，是西藏自治区主要产稻区。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条