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Climate change and northern prairie wetlands: Simulations of long-term dynamics

机译:气候变化与北部草原湿地:长期动态模拟

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A mathematical model (WETSIM 2.0) was used to simulate wetland hydrology and vegetation dynamics over a 32-yr period (1961-1992) in a North Dakota prairie wetland. A hydrology component of the model calculated changes in water storage based on precipitation, evapotranspiration, snowpack, surface runoff, and subsurface inflow. A spatially explicit vegetation component in the model calculated changes in distribution of vegetative cover and open water, depending on water depth, seasonality, and existing type of vegetation. The model reproduced four known dry periods and one extremely wet period during the three decades. One simulated dry period in the early 1980s did not actually occur. Simulated water levels compared favorably with continuous observed water levels outside the calibration period (1990-1992). Changes in vegetative cover were realistic except for years when simulated water levels were significantly different than actual levels. These generally positive results support the use of the model for exploring the effects of possible climate changes on wetland resources.
机译:在北达科他州大草原湿地中,使用数学模型(WETSIM 2.0)模拟了32年(1961-1992年)内的湿地水文和植被动态。该模型的水文组成部分根据降水,蒸散量,积雪,地表径流和地下入流来计算蓄水量的变化。该模型中空间上明确的植被成分根据水深,季节和植被的现有类型来计算营养覆盖和开放水域分布的变化。该模型再现了三十年来的四个已知的干旱期和一个极湿的时期。实际上在1980年代初期没有出现一个模拟的干旱时期。模拟水位与校准期(1990-1992年)以外连续观测到的水位相比具有优势。除了模拟水位与实际水位明显不同的年份外,植物覆盖率的变化是现实的。这些总体上积极的结果支持该模型用于探索可能的气候变化对湿地资源的影响。

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