the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Molecular simulations reveal that heterogeneous ice nucleation occurs at higher temperatures in water under capillary tension
Will Cantrell
Tianshu Li
Issei Nakamura
Raymond A. Shaw
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The processes that establish how mixed-phase closed-cell clouds transition to open-cells are poorly known. First-of-its kind aircraft observations document such a transition in the presence of anomalously high aerosol concentrations, reducing the drop size thereby discouraging riming, over the Nordic Seas at cloud temperatures < −15 °C. Eventually, ice precipitation produces surface cold pools that appear to drive the convective transition, despite strong counteracting surface fluxes.
The processes that establish how mixed-phase closed-cell clouds transition to open-cells are poorly known. First-of-its kind aircraft observations document such a transition in the presence of anomalously high aerosol concentrations, reducing the drop size thereby discouraging riming, over the Nordic Seas at cloud temperatures < −15 °C. Eventually, ice precipitation produces surface cold pools that appear to drive the convective transition, despite strong counteracting surface fluxes.