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生态学杂志 ›› 2012, Vol. 31 ›› Issue (06): 1517-1524.

• 研究报告 • 上一篇    下一篇

呼伦湖流域径流对气候变化的响应

顾润源1,李思慧2,赵慧颖1,2**,李翀3,宋卫士4,孟军4,王彦平4   

  1. 1内蒙古自治区气象科学研究所, 呼和浩特 010051; 2内蒙古自治区通辽市气象局, 内蒙古通辽 028000; 3中国水利水电科学研究院, 北京 100038; 4内蒙古自治区呼伦贝尔市气象局, 内蒙古呼伦贝尔 021008)
  • 出版日期:2012-06-09 发布日期:2012-06-09

Responses of runoff in Hulun Lake basin of Inner Mongolia to climate change.

GU Run-yuan1, LI Si-hui2, ZHAO Hui-ying1,2**, LI Chong3, SONG Wei-shi4, MENG Jun4, WANG Yan-Ping4   

  1. (1Meteorological Science Institute of Inner Mongolia, Hohhot 010051, China; 2Tongliao Meteorological Administration of Inner Mongolia, Tongliao 028000, Inner Mongolia, China; 3China Institute of Water Resources and Hydropower Research, Beijing 100038; 4 Hulunbeier Meteorological Administration of Inner Mongolia, Hailaer 021008, Inner Mongolia, China)
  • Online:2012-06-09 Published:2012-06-09

摘要: 根据呼伦湖流域1961—2010年的气温、降水、蒸发量资料以及1961—2008年径流量资料,利用非参数检验Mann-Kendall法,分析了近50年呼伦湖流域气候变化特征及其对流域径流量的影响。结果表明:呼伦湖流域近50年来气温整体呈显著上升趋势;年降水量受夏季降水量影响最为明显,经历了1961—1964年的上升,1964—1983年的下降,1983—2003年的上升和2003—2010年下降4个阶段;年蒸发量在1973年以前相对平稳,1973—1998年呈下降趋势,1999—2005年呈显著上升趋势,2005年为突变点,出现从高到低突变。夏、秋季节蒸发量趋势在时间段上与夏季降水量有很好的对应关系;径流量基本表现为1961—1965年偏丰,1965—1987年偏枯,其中1975—1980年间表现为显著下降趋势(P<0.05),1987—2002年偏丰,2002—2008年偏枯;在气温普遍升高的前提下,降水量整体呈减少趋势,其变化趋势在很大程度上决定蒸发量的变化,呼伦湖流域暖干化趋势显著。以径流自身的变化特征为时段划分基础,对比径流、气温、降水量和蒸发量的变化过程,经相关统计分析检验,发现夏、秋季气温、降水量和蒸发量是引起呼伦湖流域径流量变化的根本原因。

关键词: NO3-胁迫, 光合系统, 氮代谢, 草莓

Abstract: By using Mann-Kendall nonparametric test, this paper analyzed the climate changes and their effects on the runoff in Hulun Lake basin in recent 50 years, based on the air temperature, precipitation, and evaporation data from 1961 to 2010 and the runoff data from 1961 to 2008. In the study area, the air temperature in 1961-2010 had an obvious increasing trend, the annual precipitation was greatly affected by summer precipitation and experienced four stages,i.e., increased in 1961-1964 and 1983-2003 and decreased in 1964-1983 and 2003-2010, and the annual evaporation retained a relatively stable state before 1973, had a decreasing trend in 1973-1998 and an increasing trend in 1999-2005, and then decreased, with an abrupt change point in 2005. The evaporation in summer and autumn corresponded well with the precipitation in summer. The runoff was plentiful in 1961-1965 and 1987-2002, but scarce in 1965-1987 and 2002-2008, with a significant decrease in 1975 to 1980. With the increase of air temperature, precipitation presented an overall decreasing trend, which determined the evaporation change to a great degree, and thus, the Hunlun Lake basin appeared a warming and drying tendency. On the basis of the runoff variation characteristics, a comparison was made on the change processes of the runoff, air temperature, precipitation, and evaporation. Correlation analysis indicated that the air temperature, precipitation, and evaporation in summer and autumn were the primary causes of the runoff variation in the Hunlun Lake basin.  

Key words: NO3- stress, photosynthetic system, nitrogen metabolism, strawberry.