Detecting land cover and land use transitions and the associated temperature changes in the East Asian monsoon region

Ahyeong Im, Eungul Lee, Yaqian He
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Abstract

Unprecedented land cover and land use (LCLU) changes can significantly alter the interactions between the land and atmosphere through biogeophysical processes, potentially changing the monsoon systems. Therefore, it is necessary to quantify the LCLU changes and the impacts on the climate in the East Asian monsoon (EAM) region, where significant human‐induced LCLU changes have occurred. This study quantified the LCLU transitions with fractional maps produced using the recently developed categorical LCLU maps from 1982 to 2015. In the five sub‐regions, identified as having undergone significant LCLU transitions, the relationships of the transitions with 2 m temperature were investigated using the ERA5‐Land reanalysis data. The quantified LCLU transitions revealed that, in northeastern China, the dominant trend was forests and grasslands changing into croplands. Moreover, in the marginal areas of Inner Mongolia, the transitions of grasslands to croplands and forests were evident. Croplands were mainly converted to forests in the Sichuan region. In particular, in the Sichuan region, the temperature increased by more than 0.04°C as the forests increased by 1%. In the marginal areas of Inner Mongolia, a 1% decrease in grasslands and a 1% increase in forests, respectively, were associated with a temperature rise of more than 0.03 and 0.04°C. The detected LCLU transitions affect the regional warming as demonstrated by correlation, regression and Granger‐causality analyses and the related biogeophysical processes. Thus, the identified LCLU transitions can change the regional climate and potentially affect the monsoon systems by changing the contrast in heat between land and ocean. This empirical research will not only provide insight into possible changes to climate by LCLU transitions in the EAM region, but it will also yield practical information for implementing land cover policies while considering the geographical characteristics of the region.
探测东亚季风区土地覆被和土地利用的转变以及相关的温度变化
前所未有的土地覆被和土地利用(LCLU)变化会通过生物地球物理过程显著改变土地和大气之间的相互作用,从而可能改变季风系统。因此,有必要量化东亚季风区的土地覆被和土地利用变化及其对气候的影响。本研究利用最近开发的 1982 年至 2015 年分类 LCLU 地图制作的分数图量化了 LCLU 的变化。在被确定为经历了显著 LCLU 转变的五个次区域中,利用 ERA5-Land 再分析数据研究了 LCLU 转变与 2 米气温之间的关系。量化的 LCLU 演变显示,在中国东北地区,森林和草地转变为耕地是主要趋势。此外,在内蒙古的边缘地区,草原向耕地和森林的过渡也很明显。在四川地区,耕地主要转变为森林。特别是在四川地区,当森林面积增加 1%时,气温上升超过 0.04°C。在内蒙古边缘地区,草原减少 1%,森林增加 1%,气温分别上升 0.03 和 0.04 摄氏度以上。相关性分析、回归分析、格兰杰因果关系分析以及相关的生物地球物理过程都表明,所发现的LCLU转变影响了区域变暖。因此,已发现的 LCLU 转换可改变区域气候,并可能通过改变陆地和海洋之间的热量对比影响季风系统。这项实证研究不仅有助于深入了解 LCLU 的转变可能对 EAM 地区气候造成的变化,还将为实施土地覆被政策提供实用信息,同时考虑到该地区的地理特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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