Abstract

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.

Highlights

  • IntroductionLand use changes affect the regional climate by changing both surface biogeochemical and biophysical processes [4]

  • Heat flux to the atmosphere due to cropland expansion was quite different in different climatic zones of northern China

  • Except for humid North China, heat flux to the atmosphere due to cropland expansion decreased in humid Northeast China, semiarid

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Summary

Introduction

Land use changes affect the regional climate by changing both surface biogeochemical and biophysical processes [4]. Policies aimed at climate protection through land management have mainly focused on biogeochemical mechanisms, and only a few studies have focused on surface biophysical processes [5,6,7]. Land use and land cover change changes carbon storage patterns and alters energy balance at local scales, which has the potential to generate feedback on local and regional climates [8,9,10]. By ignoring biophysical processes, which sometimes offset biogeochemical effects, land use policies risk promoting suboptimal solutions [11,12]. It is necessary to carefully consider biophysical processes to promote LULCC proposals that will have the greatest potential climatic benefits. According to the fifth report of the Intergovernmental Panel on Climate

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