全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
冰川冻土  2004 

2002年塔里木河流域“四源一干”地表径流情势

, PP. 488-495

Keywords: 塔里木河,气象条件,河川径流,运行分析,区间耗水,下游输水

Full-Text   Cite this paper   Add to My Lib

Abstract:

2002年塔河流域内平原及山区气温都明显偏高,平原降水偏多,山区降水略偏多.3~10月0℃层高度接近常年.塔里木河4条源流出山口天然径流量273.9×108m3,比多年平均值227.0×108m3多46.9×108m3,偏多20.7%,属丰水年.其中发源于天山山脉的阿克苏河和开都河孔雀河径流增幅大,水量充沛,属丰水年;而发源于喀喇昆仑山脉的叶尔羌河和源于西昆仑山的和田河径流量保持多年均值年.4条源流入塔里木河水量为54.82×108m3.在塔里木河干流上游段耗水量25.42×108m3,是干流最大的耗水区段,中游段耗水量24.55×108m3,下游段耗水量7.38×108m3.上、中游区间耗水量49.97×108m3,占阿拉尔站年径流量的90.8%.从7月20日至11月10日共计114d由博斯腾湖向塔里木河下游生态应急输水,从博斯腾湖调水12.67×108m3,恰拉水库分水闸向塔里木河输水2.339×108m3,大西海子水库下泄3.313×108m3,年内台特玛湖形成了28.74km2的水域面积,下游沿河地下水位普遍回升,影响范围达800km2,生态效益十分显著.

References

[1]  Wang Shunde, Wang Yanguo, Wang Jing, et al. Change of climate and hydrology in the Tarim River Basin during past 40 years and their impact[J]. Journal of Glaciology and Geocryology, 2003, 25(3): 315-320.[王顺德, 王彦国, 王进, 等.塔里木河流域近40 a来气候、水文变化及其影响[J].冰川冻土, 2003, 25(3): 315-320.]
[2]  Cheng Tongfu, Zhang Weiwen, Zhang Hong, et al. Hydrological effect of ecoenvironmental deteriorated in Tarim River Basin [J].Arid Land Research, 2003, 20(4):266-271. [程同福, 张雄文, 张洪,等. 塔里木河流域生态环境恶化的水文效应[J], 干旱区研究, 2003, 20(4):266-271.]
[3]  Wang Yanguo, Li Minxue, Wang Jin, et al. Hydrological regimes of four source rivers and mainstream of Tarim River, Xinjiang in 2001[J].Journal of Glaciology and Geocryology, 2003, 25(4) : 401-408.[王彦国, 李敏学, 王进, 等.塔里木河流域2001年四源一干河川径流运行分析[J].冰川冻土,2003, 25(4):401-408.]
[4]  Wang Shunde, Li Hongde, Xu Zherui, et al. Flood detention region in the middle reaches of Tarim River mainstream and its impact on ecological environments[J].Journal of Glaciology and Geocryology, 2003, 25(6) : 712-718.[王顺德, 李红德, 许泽锐, 等. 塔里木河中游滞洪区的形成及其对生态环境的影响[J].冰川冻土, 2003, 25(6): 712-718.]
[5]  Shi Yafeng, Shen Yongping, Hu Ruji. Preliminary study on signal, impact and foreground of climatic shift from warm-dry to warm-humid in Northwest China [J]. Journal of Glaciology and Geocryology, 2002, 24(3): 219-226.[施雅风, 沈永平, 胡汝骥. 西北气候由暖干向暖湿转型的信号、影响和前景初步探讨[J].冰川冻土, 2002, 24(3): 219-226.]
[6]  Zhang Guowei, Wu Sufen, Wang Zhijie. The signal of climatic shift in Northwest China deduced from river runoff change in Xinjiang Region [J]. Journal of Glaciology and Geocryology, 2003, 25(2): 183-187.[张国威, 吴素芬, 王志杰.西北气候环境转型信号在新疆河川径流变化中的反映[J].冰川冻土, 2003, 25(2): 183-187.]
[7]  Han Ping, Xue Yan, Su Hongchao. Precipitation signal of the climatic shift in Xinjiang Region [J]. Journal of Glaciology and Geocryology, 2003, 25(2): 179-182.[韩萍, 薛燕, 苏宏超.新疆降水在气候转型中的信号反应[J].冰川冻土, 2003, 25(2): 179-182.]
[8]  Su Hongchao, Wei Wenshou, Han Ping. Change in air temperature and evaporation in Xinjiang during recent 50 years [J]. Journal of Glaciology and Geocryology, 2003, 25(2): 174-178. [苏宏超, 魏文寿,韩萍.新疆近50a来的气温和蒸发变化[J].冰川冻土, 2003, 25(2): 174-178.]
[9]  Shen Yongping, Wang Shunde. New progress in glacier and water resources changes in Tarim Basin, Xinjiang. [J]. Journal of Glaciology and Geocryology, 2002, 24(6): 819. [沈永平, 王顺德. 塔里木盆地冰川及水资源变化研究新进展[J]. 冰川冻土, 2002, 24(6): 819.]
[10]  Shen Yongping, Ding Yongjian, Liu Shiyin, et al. An increasing glacial lake outburst flood in Yarkant River, Karakorum in past ten years[J].Journal of Glaciology and Geocryology, 2003, 26 (2) : 234.[沈永平, 丁永建, 刘时银,等. 近期气温变暖叶尔羌河冰湖溃决洪水增加[J].冰川冻土, 2003, 26(2): 234.]
[11]  Wu Sufen, Han Ping, Li Yan, et al. Predicted variation tendency of the water resources in the headwaters of the Tarim River[J].Journal of Glaciology and Geocryology, 2003, 25(6) : 708-711. [吴素芬, 韩萍, 李燕, 等. 塔里木河源流水资源变化趋势预测[J]. 冰川冻土, 2003, 25(6): 708-711.]

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133