The annual flow over the upper reaches of the Heihe River shows increasing in the recent 42 years, which is extremely significant in winter, but all in all, it is relatively stable, the conversion of abundant and rare year is fairly balanced. Precipitation is the primary factor to impact the flow of the upper reaches of the Heihe River, the increasing of precipitation is closely related to the increasing of flow in summer, and the increasing of flow in summer impacts the increasing of annual flow. The ascending of air temperature, especially in autumn, causes the enlargement of snow melting of high mountain, and therefore makes flow increase during the non-flood period, which accelerates the river basin evaporation, especially in summer, and also makes the depletion of ground water resource increasing, and has a elimination function for the annual flow increasing caused by the precipitation.
LI Lin, WANG Zheng-Yu, WANG Qing-Chun
. Inflence of Climatic Change on Flow over the Upper Reaches of Heihe River[J]. SCIENTIA GEOGRAPHICA SINICA, 2006
, 26(1)
: 40
-46
.
DOI: 10.13249/j.cnki.sgs.2006.01.40
[1] 青海省水利志编委会办公室.青海河流[M].西宁:青海人民出版社,1995.125～139.
[2] 蓝永超,康尔泗,金会军,等.黑河出山径流量年际变化特征和趋势研究[J].冰川冻土,1999,21(1):49～53.
[3] 李栋梁.黑河流量和祁连山气候的年代际变化[J].高原气象,2003,22(2):104～110.
[4] 张杰,李栋梁.祁连山及黑河流域降雨量的分布特征分析[J].高原气象,2004,23(1):81～88.
[5] 丁永建,叶柏生,周文娟.黑河流域过去40年来降水时空分布特征[J].冰川冻土,1999,21(1):42～48.
[6] 汤奇成,曲耀光,周聿超.中国干旱区水文及水资源利用[M].北京:科学出版社,1992.44～80.
[7] 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[J].天气(日本),1979,26(12):759～763.
[8] 高前兆,杨新源.甘肃内陆河径流特征与冰川补给[A].程国栋.中国科学院兰州冰川冻土研究所集刊(第6号)[C].北京:科学出版社,1992.54～63.
[9] 徐国昌,董安祥.我国西部降水量的准三年周期[J].高原气象,1982,1(2):11～17.
[10] 康尔泗,程国栋,蓝永超,等.西北干旱区内陆流域出山口径流变化趋势对气候变化的响应模型[J].中国科学(D),1999,29(增刊1):47～54.
[11] 李林,汪青春,张国胜,等.黄河上游气候变化对地表水的影响[J].地理学报,2004,59(5):716～722.
[12] 李林,王振宇,秦宁生,等.长江上游径流量变化及其与影响因子关系分析[J].自然资源学报,2004,19(6):694～700.
[13] 丁永建,叶柏生,刘时银.祁连山区流域径流影响因子分析[J].地理学报,1999,54(5):431～437.
[14] 王国庆,王云璋,史忠海,等.黄河流域水资源未来变化趋势分析[J].地理科学,2001,25(1):369～400.
[15] 邓慧平,李秀彬,张明,等.气候与地表覆被变化对梭磨河流域水文影响的分析[J].地理科学,2001,21(6):493～497.
[16] 李丽娟,李海滨,王娟.澜沧江水文与水环境特征及其时空分异[J].地理科学,2002,22(1):49～56.
[17] 王根绪,王建,仵颜卿.近10年来黑河流域生态环境变化特征分析[J].地理科学,2002,22(5):527～534.
[18] 张勃,程国栋.黑河绿洲坡面分异演化研究[J].地理科学,2003,23(2):193～199.
[19] 邓伟,翟金良,闫敏华.水空间管理与水资源的可持续性[J].地理科学,2003,23(4):385～390.
[20] 李森,李凡,孙武,等.黑河下游额济纳绿洲现代荒漠化过程及其驱动机制[J].地理科学,2004,24(1):61～67.
