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6/7/2025, 3:35:22 AM
>>16690677
Did you read it? I'd post the pdf but it's 18.8MB. For example
>Overall, the albedo enhancement in non-barren LULC non-conversion regions under LCCS 2 increased global land surface mean albedo by 0.0024, contributing to 76.6% of the GSLA increase and resulted in a global mean radiative forcing of −0.126 (−0.141, −0.107) W m−2, accounting for 76.4% of GSLA-induced forcing. The albedo changes in these non-barren, non-conversion regions could be largely explained by changes in PV, NPV and SWC. PV refers to plant types actively engaged in photosynthesis, such as green leaves and grasses. NPV includes plant components that do not photosynthesize, such as dry leaves, stems and woody material, commonly found in shrubs and dead plant matter33.
>Albedo in snow-free regions experience a substantial increase (2.2%, 0.0038 (0.0036, 0.0039)), leading to a 0.72% global land surface mean albedo increase (0.0018 (0.0006, 0.0029)). The albedo increase in snow-free regions results in considerable negative global mean radiative forcing (−0.164 (−0.186, −0.138) W m2), equivalent in magnitude to 59.9% of CO2 radiative forcing and 48.9% of total greenhouse gas emissions radiative forcing during the period 2011–2019, as reported by the IPCC AR6 (ref. 10).
Did you read it? I'd post the pdf but it's 18.8MB. For example
>Overall, the albedo enhancement in non-barren LULC non-conversion regions under LCCS 2 increased global land surface mean albedo by 0.0024, contributing to 76.6% of the GSLA increase and resulted in a global mean radiative forcing of −0.126 (−0.141, −0.107) W m−2, accounting for 76.4% of GSLA-induced forcing. The albedo changes in these non-barren, non-conversion regions could be largely explained by changes in PV, NPV and SWC. PV refers to plant types actively engaged in photosynthesis, such as green leaves and grasses. NPV includes plant components that do not photosynthesize, such as dry leaves, stems and woody material, commonly found in shrubs and dead plant matter33.
>Albedo in snow-free regions experience a substantial increase (2.2%, 0.0038 (0.0036, 0.0039)), leading to a 0.72% global land surface mean albedo increase (0.0018 (0.0006, 0.0029)). The albedo increase in snow-free regions results in considerable negative global mean radiative forcing (−0.164 (−0.186, −0.138) W m2), equivalent in magnitude to 59.9% of CO2 radiative forcing and 48.9% of total greenhouse gas emissions radiative forcing during the period 2011–2019, as reported by the IPCC AR6 (ref. 10).
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