Critical Importance of Tree and Non‐Tree Vegetation for African Precipitation

te Wierik, Sofie; Keune, J.; Miralles, D. G.; Gupta, J.; Artzy‐Randrup, Y. A.; Cammeraat, L. H.; van Loon, E. E.

doi:10.1029/2023GL103274

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Critical Importance of Tree and Non‐Tree Vegetation for African Precipitation

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te Wierik, Sofie
Potsdam Institute for Climate Impact Research;

Keune, J.
External Organizations;

Miralles, D. G.
External Organizations;

Gupta, J.
External Organizations;

Artzy‐Randrup, Y. A.
External Organizations;

Cammeraat, L. H.
External Organizations;

van Loon, E. E.
External Organizations;

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te Wierik, S., Keune, J., Miralles, D. G., Gupta, J., Artzy‐Randrup, Y. A., Cammeraat, L. H., van Loon, E. E. (2024): Critical Importance of Tree and Non‐Tree Vegetation for African Precipitation. - Geophysical Research Letters, 51, 20, e2023GL103274.
https://doi.org/10.1029/2023GL103274

Zitierlink: https://publications.pik-potsdam.de/pubman/item/item_30455

Zusammenfassung

Vegetation is a major contributor of terrestrial evaporation and influences subsequent precipitation over land. Studies suggest that forests are crucial for moisture recycling, although the specific contribution of different vegetation to precipitation remains unclear. Using a moisture recycling approach, we investigate the contribution of transpiration from trees and non-tree vegetation to precipitation over Africa. We use precipitation source regions from simulated atmospheric moisture trajectories, constrained by observation-based evaporation and precipitation products, and fractional vegetation cover data. Our findings show that trees provide a higher flux to precipitation (∼777 mm year−1) than non-tree vegetation (∼342 mm year−1). However, considering the smaller spatial extent of trees compared to non-tree vegetation, precipitation in most watersheds effectively depends more on the latter. Overall, non-tree vegetation appears equally important as trees in terms of volumetric contributions to precipitation, and deserves attention in further research, considering ongoing land use changes that affect the continental water cycle.