Adiabatic and radiative cooling are both important causes of aerosol activation in simulated fog events in Europe
<p>Aerosol–fog interactions affect the visibility in, and life cycle of, fog and are difficult to represent in weather and climate models. Here we explore processes that impact the simulation of fog droplet number concentrations (<span class="inline-formula"><i>N</i><sub>d</sub></span>) at sub-kilom...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Copernicus Publications
2025-09-01
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| Rangatū: | Atmospheric Chemistry and Physics |
| Urunga tuihono: | https://acp.copernicus.org/articles/25/11157/2025/acp-25-11157-2025.pdf |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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