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Biophysical Impacts of Land Use Change over North America as Simulated by the Canadian Regional Climate Model

机译:加拿大区域气候模型模拟的北美土地利用变化的生物物理影响

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摘要

This study investigates the biophysical impacts of human-induced land use change (LUC) on the regional climate of North America, using the fifth generation Canadian Regional Climate Model (CRCM5). To this end, two simulations are performed with CRCM5 using different land cover datasets, one corresponding to the potential vegetation and the other corresponding to current land use, spanning the 1988–2012 period, driven by European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA)-Interim at the lateral boundaries. Comparison of the two suggests higher albedo values, and therefore cooler temperatures, over the LUC regions, in the simulation with LUC, in winter. This is due to the absence of crops in winter, and also possibly due to a snow-mediated positive feedback. Some cooling is observed in summer for the simulation with LUC, mostly due to the higher latent heat fluxes and lower sensible heat fluxes over eastern US. Precipitation changes for these regions are not statistically significant. Analysis of the annual cycles for two LUC regions suggests that the impact of LUC on two meter temperature, evapotranspiration, soil moisture and precipitation are present year round. However, the impact on runoff is mostly restricted to the snowmelt season. This study thus highlights regions and variables most affected by LUC over North America.
机译:这项研究使用第五代加拿大区域气候模型(CRCM5),研究了人为土地利用变化(LUC)对北美区域气候的生物物理影响。为此,由CRCM5使用不同的土地覆盖数据集进行了两次模拟,其中一次对应于潜在的植被,另一次对应于当前的土地使用,跨度为1988-2012年,由欧洲中档天气预报中心重新启动。在横向边界处进行分析(ERA)-临时。两者的比较表明,在冬季使用LUC进行模拟时,LUC区域的反照率值较高,因此温度较低。这是由于冬天没有农作物,也可能是由于雪介导的积极反馈。在夏季,使用LUC进行模拟时观察到一些降温,这主要是由于美国东部地区较高的潜热通量和较低的显热通量。这些地区的降水变化在统计上并不显着。对两个LUC区域年周期的分析表明,LUC对全年两米温度,蒸散量,土壤湿度和降水的影响。但是,对径流的影响主要限于融雪季节。因此,本研究重点介绍了北美地区LUC影响最大的地区和变量。

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