首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Climate-induced changes in biome distribution, NPP, and hydrology in the Upper Midwest U.S.: A case study for potential vegetation
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Climate-induced changes in biome distribution, NPP, and hydrology in the Upper Midwest U.S.: A case study for potential vegetation

机译:气候变化导致的美国中西部上层生物群落分布,NPP和水文学变化:以潜在植被为例

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We investigated the impacts of recent climate change on potential vegetation distributions and carbon and water cycling across the Upper Midwest from 1948 to 2007. We used the Agro-IBIS dynamic vegetation model driven by a newly developed gridded daily climate data set at 5 min × 5 min spatial resolution. Trends in climate variables were spatially heterogeneous over the study period and were associated with an overall increase in net primary productivity (NPP). We observed an average regional change in total NPP of 41 ± 30 g C m~(-2) (8%). Increased summer relative humidity and increased annual precipitation were key variables contributing to the positive trends. Mechanisms for increased productivity included a reduction in soil moisture stress as well as increased stomatal conductance resulting from an increase in summertime humidity. Model simulations also showed an average total increase in annual groundwater recharge throughout the region of 39 ± 35 mm (45%) driven by increases in annual precipitation. Evapotranspiration had a highly variable spatial trend over the 60 year period, with an average total change of 5 ± 21 mm (1%) across all grid cells. The location of the Tension Zone, a broad ecotone dividing northern mixed forests and southern hardwood forests and prairies, was not observed to migrate using analysis of meteorological variables. Key PointsA dynamic vegetation model was driven with historical climate dataClimate change caused an increase in total NPPIncreased annual precipitation caused an increase in groundwater recharge
机译:我们调查了近期气候变化对1948年至2007年整个中西部地区潜在的植被分布以及碳和水循环的影响。我们使用了Agro-IBIS动态植被模型,该模型由新开发​​的每日5分钟的网格化气候数据集驱动。最小空间分辨率。在研究期间,气候变量的趋势在空间上是异质的,并且与净初级生产力(NPP)的整体增加有关。我们观察到总NPP的平均区域变化为41±30 g C m〜(-2)(8%)。夏季相对湿度的增加和年降水量的增加是促成积极趋势的关键变量。提高生产力的机制包括减少土壤水分压力以及夏季湿度增加导致的气孔导度增加。模型模拟还显示,由于年降水量增加,整个区域的年地下水补给量平均平均增加了39±35毫米(45%)。蒸发蒸腾在60年期间具有高度变化的空间趋势,所有网格单元的平均总变化为5±21 mm(1%)。使用气象变量分析未发现张力带的位置,该带是划分北部混交林与南部硬木林和草原的广泛过渡带。要点利用历史气候数据驱动动态植被模型气候变化导致总NPP上升年度降水增加导致地下水补给增加

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