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Abstract
The ability of pollen to enable the glaciation of supercooled liquid water has been demonstrated in laboratory studies; however, the potential large-scale effect of plants and pollen on clouds, precipitation and climate is pressing knowledge to better understand and project clouds in the current and future climate. Combining ground-based measurements of pollen concentrations and satellite observations of cloud properties within the United States, we show that enhanced pollen concentrations during springtime lead to an increase in cloud ice fraction of up to 0.1 in the temperature regime where pollen are considered to act as INP (−15
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1 Leipzig University, Institute for Meteorology , Stephanstr. 3, 04103 Leipzig, Germany
2 Leipzig University, Institute for Meteorology , Stephanstr. 3, 04103 Leipzig, Germany; Leibniz-Institute for Tropospheric Research , Permoser Str. 15, 04318 Leipzig, Germany
3 Leibniz-Institute for Tropospheric Research , Permoser Str. 15, 04318 Leipzig, Germany
4 German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig , Puschstr. 4, 04103 Leipzig, Germany; Max-Planck-Institute for Biogeochemistry , Hans-Knöll-Str. 10, 07745 Jena, Germany
5 Leipzig University, Institute for Meteorology , Stephanstr. 3, 04103 Leipzig, Germany; German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig , Puschstr. 4, 04103 Leipzig, Germany