a and b, spatial patterns of the difference in recovery time between hot-dry and dry events (ΔRT = RT hot-dry-RT dry) based on the NDVI and LAI, respectively. c and d, ΔRT under different aridity ...
Regarding the ex-polar lands, compound hot-dry extremes prevail due to active land–atmosphere interactions. Specifically, a mid-tropospheric ridge initiates descending motions, creating clear-sky ...
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