1) the source regions of the Yellow River
黄河河源区
1.
The annual average and rain season precipitation and yearly runoff of the source regions of the Yellow River were analyzed.
对黄河河源区多年平均和雨季降水量、年际径流量进行分析。
2) source area of the Yellow River
黄河源区
1.
Effects of neotectonic movement in the source area of the Yellow River, China on eco-environmental deterioration.;
黄河源区新构造运动对生态环境恶化的影响
2.
Discovery of early Pleistocene strata containing plants fossils in the source area of the Yellow River and significance;
黄河源区早更新世含植物化石地层的发现及意义
3.
The Hajiang saline pool in the source area of the Yellow River is located in Madoi County,Qinghai Province,at 36.
黄河源区哈江盐池被认为是古羌人从青藏高原东北部草原地带向成都平原迁徙和扩张的起点,而且得益于盐的开发和行运。
3) source region of the Yellow River
黄河源区
1.
Character analysis of ions in the source region of the Yellow River;
黄河源区水域离子特征分析
2.
Variations of soil temperature and water moisture of seasonal frozen soil with different vegetation coverages in the source region of the Yellow River,China;
黄河源区不同植被类型覆盖下季节冻土冻融过程中的土壤温湿空间变化
3.
Eco-environmental degradation in the source region of the Yellow River is a very serious ecological and socially economic problem.
生态环境退化是黄河源区所面临的重要的生态问题和社会经济问题。
4) headwater area of the Yellow river
黄河源区
1.
The reason for degeneration of the eco-environment advance trend in the headwater area of the Yellow river;
黄河源区生态环境恶化的地质原因及发展演化趋势
2.
Changes in water environment and their ecologicgeologic environmental effects in the headwater area of the Yellow River;
黄河源区水环境变化及其生态环境地质效应
3.
Since the 1990 s the aridity of the headwater area of the Yellow River has shown as increasing trend owing to the global change in the climate.
由于全球性气候变化,进入20世纪90年代后,黄河源区干旱化趋势加剧,出现大量中、小型湖、塘干涸,草场大面积退化和荒漠化,沼泽湿地失水严重,饱冰冻土向少冰冻土退化趋势明显,一些外流湖变为内陆湖等生态环境退化现象。
5) source regions of the Yellow River
黄河源区
1.
A study on the changes of soil physical properties in the desertification process of source regions of the Yellow River using Maqu as an example;
黄河源区高寒草地沙化进程中土壤物理性质的变化(简报)——以玛曲为例
2.
Study on the desertification mechanism of natural grassland in the source regions of the Yellow River;
黄河源区天然草地沙化机理分析研究
6) the source region of the Yellow River
黄河源区
1.
Research on the status of the desertification and its driving force in the source region of the Yellow river;
黄河源区荒漠化现状及其驱动力研究
2.
At present, the regime of hydrology and water resources in the source region of the Yellow River is in trend of little variations in the total volume of precipitation, continuously increased temperature and continuously decreased coming water.
目前,黄河源区水文水资源情势呈现降水总量变化不大、气温不断升高、实际来水不断减少的趋势,与之相关的水生态环境情势表现在土地荒漠化、湖泊和湿地萎缩、冰川消融、冻土层埋深加大、草场退化、鼠虫害肆虐、水土流失加剧、生物多样性和数量锐减等方面。
补充资料：固原泾河源风景名胜区
泾河源风景名胜区在宁夏南部山区泾源县境内。这里山清水秀，群峰争绿，林茂草丰，飞瀑流泉，鸟语花香，既有北国之雄，又具南国之秀，人称黄土高原上的"绿岛"，1995年被评为省级风景名胜区。
这里的风景名胜主要有荷花苑、老龙潭、小南山、二龙河、鬼门关、凉殿峡、沙南峡等景区和秋千架、延龄寺石窟、堡子山公园、城关清真寺等。
荷花苑景区，位于县城西5公里处，从峡口蜿蜒进入8公里，两侧青山对峙，溪水中流，山上万木葱绿，小溪清澈见底，蜂蝶飞舞，流水淙淙。最迷人的是溪水两旁绿草如茵，每年5月至8月，野荷遍地，伞叶交错，黄花泛香。
老龙潭，为泾水之源。潭底深绿，深不可测，传说是魏徵梦斩老龙王的地方，柳毅传书的故事也发生在这里。
二龙河，位于县城南30公里。传说老龙王盘踞龙潭时，派他的两个儿子在这里的河边安营扎寨、镇扼咽喉，故名二龙河。两侧奇峰幽谷，间有松林华盖，绿草如茵，鸟语花香，流水潺潺。
凉殿峡，位于县城西南25公里，为六盘山腹地，气候湿润，环境幽雅，景色优美，自古就是避暑胜地。史载元太祖成吉思汗西征时曾在此避暑蓄锐，并建有亭台楼阁。至今尚有勒马石、柱墩、马槽、插旗座等遗址。
泾河源风景名胜区除上述景区外，还有位于县城东北10公里处，两峰如柱的“秋千架”，传说是穆桂英曾荡过秋千的地方。南距县城30公里，俗称“石窟儿”的延龄寺，是宋代名僧济公和尚修仙行道之处，现仍有石窟4处。
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