绿化
干旱
植被(病理学)
反照率(炼金术)
植被类型
环境科学
增强植被指数
天蓬
气候变化
自然地理学
地理
归一化差异植被指数
生态学
草原
植被指数
表演艺术
病理
艺术
生物
医学
艺术史
作者
Yixuan Zhu,Yangjian Zhang,Zhoutao Zheng,Yaojie Liu,Zhipeng Wang,Nan Cong,Jiaxing Zu,Ze Tang,Guang Zhao,Jie Gao,Yihan Sun
标识
DOI:10.1016/j.agrformet.2022.109119
摘要
• Correlation between albedo and LAI varies with vegetation type and growth stage. • Greening dominates albedo change in arid and semi-arid areas of China. • Land use change affects albedo change under greening by altering canopy structure. Land surface albedo (LSA) is a key parameter in the process of vegetation feedback to climate due to its decisive role in land surface radiation budget. However, our current knowledge on the relationship between LSA and vegetation changes is limited by one-sided attention to sole vegetation growth change or land use/land cover change (LULCC). How vegetation growth or LULCC respectively contributes to LSA change under their interactions remains poorly quantified. In this study, the arid and semi-arid areas of China (ASAC) with profound vegetation changes were selected to tackle this problem. The LSA showed a general downward trend (-0.00009 year −1 ) during 2000-2018 in response to ASAC's wide-range greening (0.0086 m 2 m −2 year −1 ). Pairwise comparison analysis revealed that under the same unit of vegetation coverage change, the LSA change magnitude was contracted when grassland was converted to cultivated land or forest land, while the conversions of forest land to other vegetations led to an amplified change magnitude of LSA. Vegetation type directly leads to a difference in LSA change magnitude under greening due to their distinct canopy spectral characteristics. Grassland possesses lower LAI and its pixel-level LSA is more prone to be contaminated by background coverage, while LSA of forest land contains more vegetation canopy signal. In most areas where vegetation type converted, greening dominated LSA change with a contribution rate up to 98.14 %, except for the conversion of grassland to forest land, where LULCC accounted for about 66.38 % of LSA change. This study could improve the estimation of LSA from LAI, which is useful for optimizing vegetation-climate interaction models.
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