Cloud cooling effects of afforestation and reforestation at midlatitudes

Because of the large carbon sequestration potential, reforestation and afforestation (R&A) are among the most prominent natural climate solutions. However, while their effectiveness is well established for wet tropics, it is often argued that R&A are less advantageous or even detrimental at higher latitudes, where the reduction of forest albedo (the amount of reflected solar radiation by a surface) tends to nullify or even overcome the carbon benefits. Here, we carefully analyze the situation for R&A at midlatitudes, where the warming effects due to vegetation albedo are regarded to be almost balanced by the cooling effects from an increased carbon storage. Using both satellite data and atmospheric boundary-layer models, we show that by including cloud- albedo effects due to land-atmosphere interactions, the R&A cooling at midlatitudes becomes prevalent. This points to a much greater poten-tial of R&A for wet temperate regions than previously considered.

Automated summary

Reforestation and afforestation have significant carbon sequestration potential, with the cooling effects of R&A at midlatitudes becoming more prevalent due to cloud-albedo effects, indicating greater potential for these initiatives in wet temperate regions than previously considered.