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Precipitation amount and event size interact to reduce ecosystem functioning during dry years in a mesic grassland

机译:降水量和事件尺寸相互作用,以减少浅血管草地干旱岁月的生态系统功能

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Ongoing intensification of the hydrological cycle is altering rainfall regimes by increasing the frequency of extreme wet and dry years and the size of individual rainfall events. Despite long-standing recognition of the importance of precipitation amount and variability for most terrestrial ecosystem processes, we lack understanding of their interactive effects on ecosystem functioning. We quantified this interaction in native grassland by experimentally eliminating temporal variability in growing season rainfall over a wide range of precipitation amounts, from extreme wet to dry conditions. We contrasted the rain use efficiency (RUE) of above-ground net primary productivity (ANPP) under conditions of experimentally reduced versus naturally high rainfall variability using a 32-year precipitation-ANPP dataset from the same site as our experiment. We found that increased growing season rainfall variability can reduce RUE and thus ecosystem functioning by as much as 42% during dry years, but that such impacts weaken as years become wetter. During low precipitation years, RUE is lowest when rainfall event sizes are relatively large, and when a larger proportion of total rainfall is derived from large events. Thus, a shift towards precipitation regimes dominated by fewer but larger rainfall events, already documented over much of the globe, can be expected to reduce the functioning of mesic ecosystems primarily during drought, when ecosystem processes are already compromised by low water availability.
机译:通过增加极端潮湿和干燥年的频率和各个降雨事件的大小来改变水文循环的持续加剧正在改变降雨制度。尽管长期以来识别大多数陆地生态系统流程的降水量和变异性的重要性,但我们缺乏对生态系统功能的互动影响。通过通过实验消除生长季节降雨量的季节性变化在各种沉淀量,从极端潮湿到干燥条件,我们通过实际消除了天然草原中的这种相互作用。在通过与我们的实验不同的32年降水DataSet,我们在实验减少的条件下对地上净初级生产率(ANPP)的雨利用效率(ANPP)对比。我们发现,日益增长的季节降雨变化可以减少rue,从而在干燥年内减少rue,从而减少了42%的生态系统,但随着年来削弱,这种影响削弱了。在低降水年期间,当降雨事件尺寸相对较大时,rue是最低的,并且当较大比例的总降雨量源于大事件时。因此,在已经记录在全球范围内已经记录的降水事件较少但更大的降雨事件中的降水制度转变,可以预期在生态系统过程已经通过低水可用性损害时,在干旱期间主要在干旱期间减少介质生态系统的运作。

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