黄河上游气候变化及其生态系统效应

Jianying Feng, Z. Yao, N. Guo, Mingling Gu, Hui Guo
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引用次数: 1

摘要

利用1961 ~ 2004年的气象水文资料和1982 ~ 2003年8 × 8 km空间分辨率的NOAA/AVHRR NDVI资料,分析了黄河上游地区的气候变化及其生态系统效应。结果表明:黄河上游地区气温变化趋势与全球变暖趋势一致,年平均土壤温度的增长速度高于气温的增长速度;年降水量呈波动变化。近40年来,最大冻土深度和年径流量呈减小趋势,特别是在90年代。该地区气候和土壤均呈现干暖趋势,尤其是土壤。黄河上游流域是生态系统脆弱区,对气候变化十分敏感。分析表明,黄河上游流域草地主要生长期为5 ~ 10月,NDVI峰值出现在7月。NDVI年峰值和均值较好地反映了气候变化,且在振荡中呈现出一定的上升趋势,说明研究区植被生长条件较好或生长日数较长。此外,该地区的温度表现出比降水更显著的相关性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The climate change and its ecosystem effect in the upper yellow river
Based on meteorological and hydrological data collected from 1961 to 2004,NOAA/AVHRR NDVI data with 8times8 km spatial resolution from 1982 to 2003, climate change and its ecosystem effect are analyzed in the upper yellow river in this paper. The results showed that the change trend of temperature in the upper yellow river was consistent with global warming, and the increasing rate of annual mean soil temperature was higher than that of air temperature. Annual precipitation presented fluctuant change. Annual maximum frozen soil depth and annual runoff tends to decrease over the past 40 years, especially in 1990s.Dry and warming trend takes place both in climate and soil in the region, especially in soil. The drainage area of upper yellow river is an ecosystem fragility area, and it is sensitive to climate change. Our analyses indicated that grassland main growth periods are from May to October,NDVI peak value appeared in July in drainage area of the upper yellow river. Annual NDVI peak value and NDVI mean value could reflect preferably climate changes, and the trends of them appeared increased in some degree among oscillations in the past 20 years, which meant a better condition for vegetation growth or longer growing days in the study area. Furthermore, the temperature exhibits a more remarkable relativity than precipitation in the area.
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