环境科学
森林砍伐(计算机科学)
热带亚热带干阔叶林
热带
植被(病理学)
气候变化
初级生产
固碳
生物量(生态学)
生态系统
全球变化
碳纤维
碳循环
遥感
农林复合经营
土地退化
碳汇
减少毁林和森林退化造成的排放
土地利用、土地利用的变化和林业
旱季
卫星
碳储量
热带稀树草原气候
陆地生态系统
大气科学
雷达
温室气体
粗木屑
卫星图像
干燥森林
全球变暖
木本植物
气候学
林业
土地利用
生态系统服务
扰动(地质)
自然地理学
荒漠化
作者
Sam B Harrison,John L. Godlee,David Thomas Milodowski,Reza Mohammadi Asiyabi,Penelope J. Mograbi,Zhofre Huberto Aguirre Mendoza,Jarcilene Silva de Almeida‐Cortez,George K.D. Ametsitsi,Alejandro Araujo‐Murakami,Sally A. Archibald,Luzmila Arroyo,Lorena M. Benitez,Samuel J. Bowers,Thom K. Brade,Domingos Cardoso,João M. B. Carreiras,Antônio Alberto Jorge Farias Castro,Duncan Mutiso Chalo,Halidou Compaoré,Isabela Santiago Carneiro da Costa
摘要
ABSTRACT Accurate mapping of woody biomass and its temporal change is critical for understanding the global carbon balance, informing restoration and supporting evidence‐based policy on climate mitigation and livelihoods. The vegetation of the dry tropics, comprised largely of dry forests and savannas, holds substantial woody carbon stocks, but both stocks and change over time remain uncertain. Where Earth Observation (EO) data have been used to estimate change over time, different products give conflicting results on the direction, magnitude and location of change. We present pan‐dry‐tropical maps of aboveground carbon density (AGCD) and AGCD change at 100 m resolution for the years 2015–2024, developed using ALOS ScanSAR satellite radar observations calibrated with in situ measurements ( n = 237). These maps suggest an aboveground woody carbon pool (AGC) in the dry tropics of 25.3 2.0 PgC, ~13.0% of global AGC. Net AGC has increased by 0.43 0.07 PgC yr −1 , ~20.0% of the global net land sink. The overall net increase (0.43 PgC yr −1 ) is comprised of gross losses from deforestation and degradation (0.27 0.05 PgC yr −1 ) and gains due to densification and extensification of 0.59 0.1 PgC yr −1 , with the balance accounted for by small changes (change < 20% of AGCD; 0.11 PgC yr −1 ). Losses are equally split between degradation and deforestation, while gains are divided roughly 2:1 between the densification of woody ecosystems and expansion into previously grass‐dominated areas. These new maps, created with a dry‐tropics‐specific EO method, highlight the importance of tropical dry forests and savannas in the global carbon cycle. The prominent role of degradation‐related losses suggests that climate change mitigation will need to focus much more on reducing losses from overharvesting than at present. The widespread increases in carbon density and the increase in tree biomass into open systems present major challenges for biodiversity conservation, restoration and livelihoods.
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