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Inclusion of land use changes in long‐term regional climate simulations over East Asia

机译:将土地利用变化纳入东亚的长期区域气候模拟中

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Long‐term simulations with regional climate models (RCMs) show biases over East Asia that result partly from fix‐in‐time land use data (EX2001). Using four satellite‐based land use images (EX8901) from the past 30 years instead of default values, 34‐year integrations were performed to make comparisons (EX8901 minus EX2001) over East Asian land areas. The decreased albedo (?0.019) resulted in weakened upward short‐wave flux, contributing to positive surface radiative forcing (2.89 W m~(?2)), which then induced enhanced sensible heat fluxes. The near‐surface wind speed was weakened (?0.15 m s~(?1)) in relation to the increased roughness length (0.042 m) and weakened pressure gradient, and induced a decreased precipitation bias of 0.0095 mm day~(?1). The increased ground temperature and enhanced soil water content promoted strengthened sensible and latent heat fluxes, which induced a decreased surface air temperature bias (?0.24 °C). Results show that by including land use changes, model simulations can be improved.
机译:使用区域气候模型(RCM)进行的长期模拟显示,东亚地区的偏差部分是由固定时间的土地利用数据(EX2001)引起的。使用过去30年中的四个基于卫星的土地使用图像(EX8901)代替默认值,进行了3​​4年的积分以对东亚陆地区域进行比较(EX8901减去EX2001)。反照率的降低(?0.019)导致向上的短波通量减弱,有助于产生正表面辐射强迫(2.89 W m〜(?2)),进而引起显着的热通量。相对于粗糙度增加(0.042 m)和压力梯度减弱,近地表风速减弱(?0.15 m s〜(?1)),导致降水偏差降低0.0095 mm day〜(?1)。升高的地面温度和增加的土壤含水量促进了感热通量和潜热通量的增强,从而导致地表空气温度偏差降低(约0.24°C)。结果表明,通过包括土地利用变化,可以改善模型模拟。

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