1) upper and middle Yellow River Basin
黄河上中游
1.
Using the energy balancing method to set up the energy and water balance monitoring System(EWBMS) for the real time monitoring in the upper and middle Yellow River Basin,and comparing the calculated values such as actual evapotranspiration,temperature,net radiation,sensible heat flux with the observed data,and hereby to improve the accuracy and reliability of the EWBMS output.
利用能量平衡方法建立能量与水平衡系统(EWBMS)对黄河上中游地区进行实时监测,并将其监测要素实际蒸散发、温度、净辐射、显热通量等与观测值比较,从而进一步说明EWBMS的准确性和可靠性。
4) Drou6rpht-flood in upper-middle reaches of Yellow River
黄河中上游旱涝
5) 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
6) 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。
补充资料：黄河中游水电规划
黄河中游水电规划
hydropower resources of Huanghe (Yellow) river system
Huong He shu一x一shu一neng zlyuon黄河水系水能资源[hydropower resourees ofHuanghe(Yellow)river system〕据1950年《中华人民共和国水力资源普查成果》统计，黄河水系水能资源理论蕴藏量为3552亿kw·h/a，其中技术可开发资源117。亿kw·h/a。黄河水系水能资涯t占中国比重仅为6%.水系内部干支流水能资源t的分布见表。黄河水系可能开发水能资派统计衰┌─────┬───┬────┬──┬──┬───┬──────┬─────────────┐│河流名称 │流城 │多年平均│河道│落差│利用 │ 理论魏藏t │可能开发资娜 ││ │面积 │流t │长度│(m) │水头 │(亿kw·h/a) ├──┬────┬─────┤│ │(kmZ) │ (m3/s)│(km)│ │(m) │ │电站│装机容t │ 年发电t ││ │ │ │ │ │ │ │厘数│ (MW) │(亿kw·h) │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│黄河全水系│ │ │ │ │ │3552 │4 15│28003 │1 170 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│其中:干流 │752443│1744.5 │5464│4830│3012 │2607.5 │43 │25136 │1037 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│流河流城 │25527 │163 │673 │2631│ │126.8 │l4 │594 │34。4 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│大通河流域│15130 │92。3 │558 │2793│884 │101.7 │1l │541 │28.1 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│渭河流域 │134766│324 │818 │2905│80。7 │75.1 │10 │93 │3。9 │├─────┼───┼────┼──┼──┼───┼──────┼──┼────┼─────┤│其他支流 │ │ │ │ │ │640.9 │337 │1 639 │66.6 │└─────┴───┴────┴──┴──┴───┴──────┴──┴────┴─────┘注:资料来源为1980年《中华人民共和国水力资琢普查成果》。 黄河干流全长5464 km，流经青海、四川、甘肃、宁夏、内蒙古、陕西、山西、河南、山东等省(自治区)，注人渤海。
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