Supersaturation Threshold is a critical atmospheric parameter that defines the minimum degree of water vapor supersaturation required for the activation of cloud condensation nuclei into cloud droplets, distinguishing it from general saturation conditions by specifying the excess vapor pressure necessary for spontaneous nucleation in warm cloud formation processes.
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Centre National de la Recherche Scientifique
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Universidad Complutense de Madrid
Madrid, Spain
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ETH Zurich
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Cooperative Institute for Research in Environmental Sciences
Boulder, United States
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University of Cambridge
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Laboratoire d'Aérologie
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