Lichens and mosses are rather inconspicuous plants. They grow on rocks, walls or tree trunks. Researchers of the University of Potsdam, the Max Planck Institute for Biogeochemistry Jena and the American Georgia Southern University have now discovered that these organisms absorb a significant part of the precipitation, which then evaporates directly back into the atmosphere. In doing so, lichens and mosses not only contribute decisively to the global water cycle, but also have a cooling effect on the regional temperature of the land surface. The results of the study have just been published in the journal Nature Geoscience.
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