Regulation effect of planted forests on land surface temperature in China

被引:0
作者
Zhang, Zhijiang [1 ,2 ]
Yang, Kai [1 ,2 ]
Wang, Lunche [3 ]
Cheng, Kai [4 ,5 ]
Chen, Chao [1 ,2 ]
Ding, Chao [6 ]
机构
[1] Suzhou Univ Sci & Technol, Sch Geog Sci & Geomat Engn, Suzhou 215009, Peoples R China
[2] Suzhou Univ Sci & Technol, SuZhou Key Lab Spatial Informat Intelligent Techno, Suzhou 215009, Peoples R China
[3] China Univ Geosci, Sch Geog & Informat Engn, Wuhan 430074, Peoples R China
[4] Peking Univ, Inst Remote Sensing & Geog Informat Syst, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[5] Peking Univ, Inst Ecol, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[6] Beijing Normal Univ, Fac Arts & Sci, Dept Geog Sci, Zhuhai 519087, Peoples R China
关键词
Planted forests; Surface temperature; Biophysical effect; Intrinsic biophysical mechanism; Climate mitigation; BACKGROUND CLIMATE; COVER CHANGE; AFFORESTATION; MANAGEMENT; IMPACT; DEFORESTATION; ATTRIBUTION; FEEDBACKS;
D O I
10.1016/j.agrformet.2025.110660
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Afforestation has been regarded as a potentially effective strategy for the mitigation of climate warming. China has the largest planted forest area worldwide benefited by a series of large-scale afforestation and reforestation project since the 1970s. The planted forests (PF) have been widely reported as an enduring carbon sink. However, the climatic regulation effect of PF on climate through biophysical process remains unclear. To this end, we utilized satellite observations to quantify the impact of the conversion of grasslands (GRA), croplands (CRO) and natural forests (NF) to PF on land surface temperature (LST) between 2003 and 2012 and illustrated the underlying biophysical mechanisms based on a revised Intrinsic Biophysical Mechanism (IBM) method. The results indicated that afforestation of PF caused negligible daily cooling effect (-0.005 f 0.002 K) compared with NF while induced obvious daily cooling effect compared with GRA (-0.253 f 0.004 K) and CRO (-0.162 f 0.002 K). We also demonstrated that the revised IBM attribution method is applicable in interpreting the biophysical mechanism of PF on LST. Attribution analysis revealed that the surface roughness and Bowen ratio dominated the cooling effect as the surface became rougher and more evaporative cooling after converting NF, GRA, or CRO to PF. The contributions of albedo were less stark compared with other components and presented a weak warming effect. Furthermore, the atmospheric feedback was proved that have a pronounced impact on LST and should be included in the attribution of LST change. This study focuses on the potential of PF afforestation to provide local climate adaptation benefits, filling the gaps of previous studies involved to biophysical effect failure in distinguishing NF and PF, and provides new guidance for local climate impact evaluation when implementing forestry projects.
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页数:11
相关论文
共 72 条
[1]   Climatic impacts of bushland to cropland conversion in Eastern Africa [J].
Abera, Temesgen Alemayehu ;
Heiskanen, Janne ;
Pellikka, Petri K. E. ;
Adhikari, Hari ;
Maeda, Eduardo Eiji .
SCIENCE OF THE TOTAL ENVIRONMENT, 2020, 717
[2]   Clarifying the role of radiative mechanisms in the spatio-temporal changes of land surface temperature across the Horn of Africa [J].
Abera, Temesgen Alemayehu ;
Heiskanen, Janne ;
Pellikka, Petri ;
Rautiainen, Miina ;
Maeda, Eduardo Eiji .
REMOTE SENSING OF ENVIRONMENT, 2019, 221 :210-224
[3]   Quantitative analysis of the links between forest structure and land surface albedo on a global scale [J].
Alibakhshi, Sara ;
Naimi, Babak ;
Hovi, Aarne ;
Crowther, Thomas W. ;
Rautiainen, Miina .
REMOTE SENSING OF ENVIRONMENT, 2020, 246
[4]   Biophysical climate impacts of recent changes in global forest cover [J].
Alkama, Ramdane ;
Cescatti, Alessandro .
SCIENCE, 2016, 351 (6273) :600-604
[5]   Combined climate and carbon-cycle effects of large-scale deforestation [J].
Bala, G. ;
Caldeira, K. ;
Wickett, M. ;
Phillips, T. J. ;
Lobell, D. B. ;
Delire, C. ;
Mirin, A. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2007, 104 (16) :6550-6555
[6]   Offset of the potential carbon sink from boreal forestation by decreases in surface albedo [J].
Betts, RA .
NATURE, 2000, 408 (6809) :187-190
[7]   CLIMATE SCIENCE Afforestation cools more or less [J].
Betts, Richard A. .
NATURE GEOSCIENCE, 2011, 4 (08) :504-505
[8]   Forests and climate change: Forcings, feedbacks, and the climate benefits of forests [J].
Bonan, Gordon B. .
SCIENCE, 2008, 320 (5882) :1444-1449
[9]  
Bright RM, 2017, NAT CLIM CHANGE, V7, P296, DOI [10.1038/NCLIMATE3250, 10.1038/nclimate3250]
[10]   China's response to a national land-system sustainability emergency [J].
Bryan, Brett A. ;
Gao, Lei ;
Ye, Yanqiong ;
Sun, Xiufeng ;
Connor, Jeffery D. ;
Crossman, Neville D. ;
Stafford-Smith, Mark ;
Wu, Jianguo ;
He, Chunyang ;
Yu, Deyong ;
Liu, Zhifeng ;
Li, Ang ;
Huang, Qingxu ;
Ren, Hai ;
Deng, Xiangzheng ;
Zheng, Hua ;
Niu, Jianming ;
Han, Guodong ;
Hou, Xiangyang .
NATURE, 2018, 559 (7713) :193-204