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Climate Change Impacts on Wetlands of the Yellow River Headwaters

机译:气候变化对黄河源头湿地的影响

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The impacts of climate change and human activities have modified the structure and the distribution patternof wetlands of the Yellow River headwaters. We studied ETM and TM satellite images data using GIS from1990, 2000 and 2010 to analyse changes in the spatial distribution and patterns of the wetland area thatsupplies water to the Yellow River. We propose stable conditions for the different types of wetlands andmutual transition probabilities. Time series data on temperature, precipitation and evaporation at the Jimaiand Maduo hydrological and meteorological stations were analysed. Characteristics and trends ofmeteorological factors were studied. The relational grades of different wetlands and meteorological factorswere calculated using Grey System Theory. Major factors determining wetland evolution in the Yellow Riverheadwaters were proposed and the impacts of climate change on wetland evolution were analysed. Wetlandevolution in the Yellow River headwaters is closely related to climate change. Precipitation is the dominantmeteorological determinant for the wetland pattern evolution and transformation of the other wetland types.Presence of wetland areas is positively correlated with precipitation and temperature and negatively correlatedwith evaporation. Wetlands are important for maintaining the “cold and wet” effect on regional climates;when precipitation increases, the “cold and wet” effect of the wetland increases.
机译:气候变化和人类活动的影响改变了黄河源头湿地的结构和分布格局。我们使用GIS研究了1990年,2000年和2010年的ETM和TM卫星图像数据,以分析向黄河供水的湿地面积的空间分布和格局变化。我们为不同类型的湿地和相互过渡的可能性提出了稳定的条件。分析了吉迈和马多水文气象站的温度,降水和蒸发量的时间序列数据。研究了气象因素的特征和趋势。应用灰色系统理论计算了不同湿地与气象因子的关系等级。提出了决定黄河源头湿地演变的主要因素,并分析了气候变化对湿地演变的影响。黄河源头的湿地演变与气候变化密切相关。降水是其他湿地类型湿地格局演变和转化的主要气象决定因素。湿地面积的存在与降水和温度呈正相关,与蒸发量呈负相关。湿地对于维持对区域气候的“冷湿”作用非常重要;当降水增加时,湿地的“冷湿”作用增加。

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