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Divergent responses of vegetation cover in Southwestern US ecosystems to dry and wet years at different elevations

机译:美国西南生态系统中植被覆盖度对不同海拔地区的干旱和潮湿年份的不同响应

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In the semiarid Southwestern United States, prolonged drought conditions since the early 2000s have resulted in widespread declines of the vegetation productivity in this water-constrained ecosystem, as revealed by analyses of the Normalized Difference Vegetation Index (NDVI). However, the spatial pattern of the NDVI response to dry years is not uniform: a divergent response of NDVI to precipitation is observed between the low-lying desert and the high montane forests at elevations above 2,500 meter. We analyzed relationships between 15 years of Moderate Resolution Imaging Spectroradiometer (MODIS) NDVI and gridded climate data (PRISM) along elevation gradients at scales from regional to local. Our elevation-explicit analysis captures the transition from water-limited to temperature-limited ecosystems, with a sign-reversal in the correlation coefficient between precipitation and NDVI observed at about 2,500-3,000m altitude. We suggest warmer temperatures and less snow cover associated with drier years as explanations for high elevation gains in vegetation productivity during dry years.
机译:根据归一化植被指数(NDVI)的分析,在美国西南部半干旱地区,自2000年代初以来长期干旱导致该水受限生态系统的植被生产力普遍下降。但是,NDVI对干旱年份的空间分布并不均匀:在海拔2500米以上的低洼沙漠和高山森林之间,NDVI对降水的响应有所不同。我们分析了15年的中分辨率成像光谱仪(MODIS)NDVI和网格气候数据(PRISM)沿从区域到本地尺度的海拔梯度之间的关系。我们的海拔高度明晰分析捕获了从缺水的生态系统转变为受温度限制的生态系统,并且在大约2500-3,000m的高度观测到的降水与NDVI之间的相关系数出现了符号反转。我们建议与干旱年份相关的温度升高和积雪减少,以解释干旱年份植被生产力的高程提高。

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