Non‐Abrupt Vegetation Changes due to Altered Nutrient Balance Make Complex Scale‐Dependent Warming and Cooling Effects

Land-atmosphere exchanges are mediated by biophysical properties (e.g., albedo change, evaporative cooling) and biogeochemical cycle (e.g., CO₂ fluxes), with both processes exerting global feedback as radiative forcing ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"> mml:semantics mml:mrow mml:miRF</mml:mi></mml:mrow> mml:annotation $RF$ </mml:annotation></mml:semantics> </mml:math> ). While most research on <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML">