4.7 Article

Relative effects of precipitation variability and warming on tallgrass prairie ecosystem function

期刊

BIOGEOSCIENCES
卷 8, 期 10, 页码 3053-3068

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/bg-8-3053-2011

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资金

  1. USDA-NRI
  2. DOE-NIGEC/NICCR
  3. NSF
  4. Direct For Biological Sciences [0823341] Funding Source: National Science Foundation

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Precipitation and temperature drive many aspects of terrestrial ecosystem function. Climate change scenarios predict increasing precipitation variability and temperature, and long term experiments are required to evaluate the ecosystem consequences of interannual climate variation, increased growing season (intra-annual) rainfall variability, and warming. We present results from an experiment applying increased growing season rainfall variability and year round warming in native tallgrass prairie. During ten years of study, total growing season rainfall varied 2-fold, and we found similar to 50-200% interannual variability in plant growth and aboveground net primary productivity (ANPP), leaf carbon assimilation (A(CO2)), and soil CO2 efflux (J(CO2)) despite only similar to 40% variation in mean volumetric soil water content (0-15 cm, Theta(15)). Interannual variation in soil moisture was thus amplified in most measures of ecosystem response. Differences between years in Theta(15) explained the greatest portion (14-52%) of the variation in these processes. Experimentally increased intra-annual season rainfall variability doubled the amplitude of intra-annual soil moisture variation and reduced Theta(15) by 15%, causing most ecosystem processes to decrease 8-40% in some or all years with increased rainfall variability compared to ambient rainfall timing, suggesting reduced ecosystem rainfall use efficiency. Warming treatments increased soil temperature at 5 cm depth, particularly during spring, fall, and winter. Warming advanced canopy green up in spring, increased winter J(CO2), and reduced summer J(CO2) and forb ANPP, suggesting that the effects of warming differed in cooler versus warmer parts of the year. We conclude that (1) major ecosystem processes in this grassland may be substantially altered by predicted changes in interannual climate variability, intra-annual rainfall variability, and temperature, (2) interannual climate variation was a larger source of variation in ecosystem function than intra-annual rainfall variability and warming, and (3) effects of increased growing season rainfall variability and warming were small, but ecologically important. The relative effects of these climate drivers are likely to vary for different ecosystem processes and in wetter or drier ecosystems.

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