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Effects of Cropland Expansion on the Regional Land Surface Radiative Energy Balance and Heat Fluxes in Northern China

机译:农田扩张对中国北方区域土地辐射能量平衡和热量流量的影响

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摘要

Land use change can impact the land surface radiation budget and energy balance by changing surface biophysical processes. Based on satellite remote sensing data and land use data from 2000 to 2015, we quantitatively estimated radiative forcing induced by cropland expansion during the early 21st century in northern China. The results showed that heat flux from the land surface to the atmosphere due to cropland expansion was quite variable in different climate zones. The heat flux increased in humid North China, whereas it decreased in arid Northwest China, semiarid Inner Mongolia, and humid Northeast China. Cropland expansion from woodland areas led to a general decline in the land surface heat flux to the atmosphere, which led to a cooling effect on the climate. The surface heat flux to the atmosphere due to cropland expansion in grassland areas displayed significant variations in different climate zones. The surface heat flux decreased only in humid Northeast China and arid Northwest China. The net surface radiation and latent heat flux both increased when grasslands were changed into cropland, but to different extents, which produced the differences in the surface heat flux to the atmosphere between different zones.
机译:土地利用变化可以通过改变表面的生物物理过程的影响地表辐射平衡和能量平衡。基于卫星遥感数据和土地利用数据2000年至二零一五年,我们定量评价辐射21世纪初在中国北方期间强迫诱导的耕地扩张。结果表明:从地表到大气中的热通量由于耕地扩张是在不同的气候区域相当变量。在潮湿的中国北方的热通量增加,而它在干旱的中国西北下降,半干旱内蒙古,潮湿中国东北。从导致在土地表面热通量到大气中普遍下降,这导致了对气候的冷却效果林地区域农田扩张。表面热通量到大气由于在草地区域农田扩张显示在不同的气候区显著变化。表面热流只有在潮湿的中国东北和西北干旱区中国降低。净表面辐射热和潜热通量时草原被改变为农田既增加了,但在不同程度上,这产生在表面热通量的不同区域之间的气氛的差异。

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  • 作者

    Jia Ning;

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  • 年度 2021
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  • 原文格式 PDF
  • 正文语种 eng
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