By generating a high-resolution temperature dataset and adopting a more holistic space-and-time approach, Prof. Li's team was able to encompass all forms of realistic LCCs. Their extensive analysis of satellite observations uncovered changes in 529,128 1-km pixels from 2006 to 2015. Notably, the study expanded beyond the commonly examined afforestation and deforestation (accounting for 46.28% of the changes), to include transitions within non-forest vegetation types (18.62%) and changes involving non-vegetation types (35.10%).
The findings reveal a nuanced picture of temperature changes: a global average increase of 0.08 K in areas with LCCs, yet with significant variations across latitudes, ranging from -0.05 K to 0.18 K. These temperature effects contributed to as much as 44.6% of the overall concurrent warming, underscoring the substantial impact of LCC biophysical processes.
The study further identified distinct regional patterns. In the northern mid-latitudes, expansions of cropland predominantly drove cooling effects, while forest-related LCCs induced warming in other regions. Contrary to previous assumptions of symmetry in potential effects, the actual effects exhibited notable asymmetries: LCCs with warming impacts were more frequent and intense than those leading to cooling. This asymmetry was attributed to a combination of uneven changes in transition types and driving variables.
These insights challenge the notion that reversing a specific LCC would counterbalance its temperature impact. As such, the study offers a new perspective on land management and climate adaptation strategies, emphasizing the need for nuanced approaches in response to diverse LCC scenarios.
Research Report:Local temperature responses to actual land cover changes present significant latitudinal variability and asymmetry
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