Lagrangian transport based on the winds of the icosahedral nonhydrostatic model (ICON)
Representing atmospheric transport of constituents accurately in a chemistry climate model is a challenge. This is true in particular for a realistic representation of atmospheric transport barriers, e.g. at the edge of the polar vortices or at the tropopause. When transport is represented employing...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Borntraeger
2024-07-01
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| Rangatū: | Meteorologische Zeitschrift |
| Ngā marau: | |
| Urunga tuihono: | http://dx.doi.org/10.1127/metz/2024/1207 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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