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首页> 外文期刊>Journal of Advances in Modeling Earth Systems >Impacts of forest harvest on cold season land surface conditions and land?¢????atmosphere interactions in northern Great Lakes states
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Impacts of forest harvest on cold season land surface conditions and land?¢????atmosphere interactions in northern Great Lakes states

机译:大湖北部各州森林采伐对寒冷季节土地表面状况和土地大气相互作用的影响

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摘要

Land cover change, including temporary disturbances such as forest harvests, can significantly affect established regimes of surface energy balance and moisture exchange, altering flux processes that drive weather and climate. We examined the impacts of forest harvest on winter land?¢????atmosphere interactions in a temperate region using high?¢????resolution numerical modeling methods in paired simulations. Using the WRF?¢????ARW atmospheric model and the Noah land surface model, we simulated the balance of surface sensible and latent heat fluxes and the development and dissipation of a stable nocturnal boundary layer during generally calm synoptic conditions. Our results show reduced daily?¢????average snow?¢????covered land surface sensible heat flux (by 80%) and latent heat flux (by 60%) to the atmosphere in forest clearings due to albedo effects and rebalancing of the surface energy budget. We found a land surface cooling effect (?¢????8 W m ?¢????2 ) in snow?¢????covered cleared areas, consistent with prior modeling studies and conceptual understanding of the mechanisms for midlatitude deforestation to offset anthropogenic global warming at local scales. Results also demonstrate impacts of forest clearing on the passage of a weak cold front due to altered near?¢????surface winds and boundary layer stability. We show significant differences in both surface conditions and fluxes between harvested and undisturbed forest areas. Our results demonstrate the potential utility of high?¢????resolution remote sensing analyses to represent transient land cover changes in model simulations of weather and climate, which are usually undertaken at coarser resolutions and often overlook these changes at the land surface.
机译:土地覆盖的变化,包括诸如森林砍伐之类的暂时性干扰,会严重影响已建立的表面能平衡和水分交换制度,从而改变驱动天气和气候的通量过程。我们使用配对模拟中高分辨率的数值模拟方法,研究了森林采伐对温带地区冬季土地-大气相互作用的影响。利用WRF-ARW大气模型和诺亚陆面模型,我们模拟了在一般平静的天气条件下,表面感热和潜热通量的平衡,以及稳定的夜间边界层的发育和消散。我们的结果表明,由于反照率效应和森林覆盖率的提高,覆盖森林表面的土地表面显热通量(减少80%)和潜热通量(减少60%)每天减少。重新平衡表面能预算。我们在积雪覆盖的空旷地区发现了雪中的陆地表面降温效果(8 W m 2 2),这与先前的模型研究和对中纬度机制的概念理解相一致。砍伐森林以抵消局部规模的人为全球变暖。结果还表明由于近地表风和边界层稳定性的改变,森林砍伐对弱冷锋通过的影响。我们显示出采伐和未受干扰的森林地区之间的地表条件和通量都存在显着差异。我们的结果表明,高分辨率的遥感分析在天气和气候模型模拟中代表瞬时土地覆盖变化的潜在效用,该模拟通常在较粗的分辨率下进行,并且常常忽略了地面的这些变化。

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