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1)  the upper Chaohe River Basin
潮河上游
1.
Impacts of soil and water conservation measures on annual runoff in the upper Chaohe River Basin in northern China based on hydrological analysis method;
基于水文分析法评估水保措施对潮河上游年径流量的影响
2)  the upper reach of Chaobaihe River Basin
潮白河上游
1.
Trend and causation analysis of runoff variation in the upper reach of Chaobaihe River Basin in northern China during 1961-2005;
潮白河上游1961—2005年径流变化趋势及原因分析
3)  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
4)  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。
5)  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
6)  upper reaches of Huaihe River
淮河上游
1.
Calculation of ecological water demand in upper reaches of Huaihe River
淮河上游生态需水量计算分析
2.
The upper reaches of Huaihe River is the area where flood - waterlogging and drought disasters take place frequently.
淮河上游修建了大量的水库,收到了显著成效,但在特大暴雨出现年份,由于全力泄洪或溃坝提高了洪峰流量。
3.
Based on the land use maps of the study region during 3 different periods(the 1980s,the 1990s and the 2000s),the influence of land use change on the runoff generation in the upper reaches of Huaihe River basin(upstream of Xixian hydrological station) was simulated and analyzed.
以淮河上游息县水文站以上为研究区域,基于研究区域3期(20世纪80年代2、0世纪90年代、2000年以后)土地利用图模拟分析土地利用变化对流域产水的影响。
补充资料:迎潮送潮辞·送潮
【诗文】:
潮西来兮又东下,日染中流兮红洒洒。汀葭苍兮屿蓼枯,
风骚牢兮愁烟孤。大几望兮微将晦翳,睨瀛溶兮敛然而退。
爱长波兮数数,一幅巾兮无缨可濯。帆生尘兮楫有衣,
怅潮之还兮吾犹未归。



【注释】:



【出处】:
全唐诗:卷621-22
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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