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首页> 外文期刊>Hydrology and Earth System Sciences >Projecting water yield and ecosystem productivity across the United States by linking an ecohydrological model to WRF dynamically downscaled climate data
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Projecting water yield and ecosystem productivity across the United States by linking an ecohydrological model to WRF dynamically downscaled climate data

机译:通过将生态水文模型与WRF关联以动态缩减气候数据,预测全美国的水产量和生态系统生产力

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Quantifying the potential impacts of climate change on water yield and ecosystem productivity is essential to developing sound watershed restoration plans, and ecosystem adaptation and mitigation strategies. This study links an ecohydrological model (Water Supply and Stress Index, WaSSI) with WRF (Weather Research and Forecasting Model) using dynamically downscaled climate data of the HadCM3 model under the IPCC SRES A2 emission scenario. We evaluated the future (2031-2060) changes in evapotranspiration (ET), water yield (Q) and gross primary productivity (GPP) from the baseline period of 1979-2007 across the 82 773 watersheds (12-digit Hydrologic Unit Code level) in the coterminous US (CONUS). Across the CONUS, the future multi-year means show increases in annual precipitation (P) of 45mm yr(-1) (6 %), 1.8 degrees C increase in temperature (T), 37 mm yr(-1) (7 %) increase in ET, 9 mm yr(-1) (3 %) increase in Q, and 106 gCm(-2)yr(-1) (9 %) increase in GPP. We found a large spatial variability in response to climate change across the CONUS 12-digit HUC watersheds, but in general, the majority would see consistent increases all variables evaluated. Over half of the watersheds, mostly found in the northeast and the southern part of the southwest, would see an increase in annual Q (> 100 mm yr(-1) or 20 %). In addition, we also evaluated the future annual and monthly changes of hydrology and ecosystem productivity for the 18 Water Resource Regions (WRRs) or two-digit HUCs. The study provides an integrated method and example for comprehensive assessment of the potential impacts of climate change on watershed water balances and ecosystem productivity at high spatial and temporal resolutions. Results may be useful for policy-makers and land managers to formulate appropriate watershed-specific strategies for sustaining water and carbon sources in the face of climate change.
机译:量化气候变化对水产量和生态系统生产力的潜在影响,对于制定合理的流域恢复计划以及生态系统适应和减缓战略至关重要。这项研究使用IPCC SRES A2排放情景下HadCM3模型的动态降尺度气候数据,将生态水文模型(供水和压力指数,WaSSI)与WRF(天气研究和预报模型)联系起来。我们评估了1979-2007年基线期在82773个流域(12位水文单位代码级别)上的蒸散量(ET),水产量(Q)和总初级生产力(GPP)的未来(2031-2060)变化在相邻的美国(CONUS)中。在整个CONUS上,未来的多年平均值表明年降水量(P)增加了45mm yr(-1)(6%),温度增加了1.8摄氏度(T),37 mm yr(-1)(7% )ET的增加,Q值增加9 mm yr(-1)(3%),GPP则增加106 gCm(-2)yr(-1)(9%)。我们发现CONUS 12位HUC流域响应气候变化存在很大的空间变异性,但总的来说,大多数人会看到所有评估的变量都持续增加。超过一半的流域(主要分布在东北和西南部的南部)将出现年Q值增加(> 100 mm yr(-1)或20%)。此外,我们还评估了18个水资源区(WRR)或两位数的HUC的水文和生态系统生产力的未来年度和每月变化。该研究为在高时空分辨率下综合评估气候变化对流域水平衡和生态系统生产力的潜在影响提供了综合方法和实例。结果可能有助于决策者和土地管理者制定针对流域的适当策略,以应对气候变化而维持水和碳源。

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