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Dryland Riparian Ecosystems in the American Southwest: Sensitivity and Resilience to Climatic Extremes

机译:美国西南部的旱地河岸生态系统:对极端气候的敏感性和复原力

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Drylands make up over 40% of the earth’s land surface (Noy-Meir 1973; Reynolds and others 2007). In these arid and semiarid landscapes, surface and subsurface water flows create mesic riparian environments (Kingsford 2006; Stromberg and Tellman 2009). Dryland riparian areas sustain water-limited plants and animals that cannot withstand upland conditions year-round, thereby supporting regional diversity (Sabo and others 2005; Lite and others 2005). Dryland rivers are also characterized by occasional large, high-intensity floods that rework the bed geomorphology and increase riparian heterogeneity. This combined variation in water availability and flood disturbance creates spatiotemporally complex and unique landscapes (Soykan and Sabo 2009; Soykan and others 2012).
机译:旱地占地球陆地面积的40%以上(Noy-Meir 1973; Reynolds等,2007)。在这些干旱和半干旱的景观中,地表水和地下水流创造了中流河岸环境(Kingsford 2006; Stromberg和Tellman 2009)。旱地河岸地区一年四季都不能忍受旱地的水和动植物,从而支持了区域多样性(Sabo等人,2005; Lite等人,2005)。旱地河流的特征还在于偶尔发生的大型高强度洪水,这些洪水会重整河床的地貌并增加河岸的异质性。可用水量和洪水干扰的综合变化造成了时空上复​​杂而独特的景观(Soykan和Sabo 2009; Soykan等2012)。

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