The Influence of Climate Change on Surface Water in the Upper Yellow River

Expand
  • 1. Qinghai Climate Center, Xining 810001, China;
    2. Qinghai Meteorological Bureau, Xining 810001, China;
    3. Division of Qinghai Meteorological Science, Xining 810001, China

Received date: 2004-03-07

  Revised date: 2004-06-27

  Online published: 2004-09-25

Abstract

Based on the hydrological data of Tangnag hydrometric station in the upper Yellow (Huanghe) River and meteorological data of this river basin in the same period, this paper studied the influence of climate change on surface water resource in the upper Yellow River. The results show that the annual flow in the upper Yellow River has been decreasing, it is especially more significant since the 1990s; while the climate change in the upper Yellow River tends toward desiccation with the increase of air temperature, decrease of precipitation and increment of evaporation, which is extremely significant in the 1990s. The increase of air temperature, decrease of precipitation and increment of evaporation resulted in the decrease of flow in the upper Yellow River, and among them, precipitation amount is the main climate factor to impact flow. The decrease of precipitation amount, especially its decrease in summer, is the direct cause to make the flow decrease in the upper Yellow River.

Cite this article

LI Lin, WANG Qingchun, ZHANG Guosheng, FU Yang, YAN Liangdong . The Influence of Climate Change on Surface Water in the Upper Yellow River[J]. Acta Geographica Sinica, 2004 , 59(5) : 716 -722 . DOI: 10.11821/xb200405009

References


[1] Li Lin, Zhang Guosheng, Wang Qingchun et al. Dry climate impact on evapotranspiration in the upper valley of the Huanghe River. Meteorological Monthly, 1999, 25(8): 11-15.
[李林, 张国胜, 汪青春 等. 青海地表水资源的变化及影响因子. 气象, 1999, 25(8): 11-15.]

[2] Kouyichirou Takahashi. The calculation method of monthly average temperature, monthly precipitation and evapotranspiration. Synoptics (Japan), 1979, 26(12): 759-763.
[高桥浩一郎. 月平均气温月降水量以及蒸发散量的推定方式. 天气(日本), 1979, 26(12): 759-763.]

[3] Song Zhengshan, Yang Hui, Zhang Qingyun. The characteristics of temporal and spatial variation of water resource components over North China. Plateau Meteorology, 1999, 18(4): 552-565.
[宋正山, 杨辉, 张庆云. 华北地区水资源各分量的时空变化特征. 高原气象, 1999, 18(4): 552-565.]

[4] Tang Qicheng. The Utilization of Hydrologic and Water Resources over Drought-hit Area in China. Beijing: Science Press, 1992. 44-80.
[汤奇成, 曲耀光 等. 中国干旱区水文及水资源利用. 北京: 科学出版社, 1992. 44-80.]

[5] Shi Yafeng. The Impact of Climate Change on Water Resource over Northwest and North China. Jinan: Shandong Science Press, 1995. 127-141.
[施雅风. 气候变化对西北华北水资源的影响. 济南: 山东科学出版社, 1995. 127-141.]

[6] Wang Shaowu, Dong Guangrong. The Environment Characteristics and Development in Western China. Beijing: Science Press, 2002. 81-85.
[王绍武, 董光荣. 中国西部环境特征及其演变. 北京: 科学出版社, 2002. 81-85.]

[7] Ding Yihui. The Forecasting of Environment Change over North China. Beijing: Science Press, 2002. 57-62.
[丁一汇. 中国西部环境变化的预测. 科学出版社, 2002. 57-62.]

[8] Li Lin, Zhang Guosheng, Wang Qingchun et al. Study on evapotranspiration and its impact factors over Huanghe River upper stream area. Advance in Earth Sciences, 2000, 15(3): 256-259.
[李林, 张国胜, 汪青春 等. 黄河上游流域蒸散量及其影响因子研究. 地球科学进展, 2000, 15(3): 256-259.]

Outlines

/