中国农业气象

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黄河源区气候温暖化及其对植被生产力影响评价

李英年;赵新全;汪诗平;周华坤;   

  1. 中国科学院西北高原生物研究所,中国科学院西北高原生物研究所,中国科学院西北高原生物研究所,中国科学院西北高原生物研究所 西宁810001,西宁810001,西宁810001,西宁810001
  • 出版日期:2007-08-10 发布日期:2007-08-10
  • 基金资助:
    中科院西北高原生物研究所百人计划;; 中科院西部行动计划;; 西部之光人才培养计划项目

Impact Assessment of Climate Warming up on Primary Productivity in Yellow River Source Region

LI Ying-nian, ZHAO Xin-quan, WANG Shi-ping, ZHOU Hua-kun(Northwest Institute of Plateau Biology, CAS, Xining 810001, China)   

  • Online:2007-08-10 Published:2007-08-10

摘要: 在分析黄河源区气温、降水变化的基础上,用Turc经验模式计算黄河源区的蒸散量,同时分析了近十几年来土壤湿度、植被地上净初级生产力的变化特征。结果表明,1959-2005年,黄河源区年平均气温按0.0284℃/a的变率升高,降水变化态势平稳,但蒸散量增加趋势明显,上升倾向率达0.7315mm/a,气温上升趋势与年代增加具有明显的相关性。从1987年以来土壤湿度的监测结果分析得知,黄河源区下垫面蒸散量的加大使土壤向干暖化发展。这种气候因素的影响,导致近十几年来植被地上净初级生产力按9.506g/(m2a)的倾向率下降。

关键词: 黄河源区, 气候变化, 蒸散量, 生态环境

Abstract: On the basis of analysis of the variations of temperature and precipitation in the Yellow River Source Region, the evapotranspiration was calculated by Turc experiential model and the soil humidity and net primary productivity aboveground in the last ten years were analyzed. The results suggested that temperature and evapotranspiration were significantly correlated and increased by 0.0284℃ per year and 0.7315mm per year respectively, while the precipitation was stable in 1959-2005. This drier and warmer tendency could be proved by the soil moisture monitoring results since 1987. The net plant primary productivity aboveground decreased by 9.506 g m-2 per year as meteorological factors changed.

Key words: Yellow River source regions, Yellow River source regions, Climate change, Evapotranspiration, Ecosystem