Upward transport of boundary layer air to altitudes of the Asian summer monsoon anticyclone in Eulerian and Lagrangian model simulations
The Asian summer monsoon anticyclone is a dominant circulation system in the upper troposphere and lower stratosphere (UTLS) in boreal summer (about June–September). An appropriate simulation of the monsoon anticyclone is an important challenge for chemistry climate and chemistry transport models. H...
Furkejuvvon:
| Váldodahkkit: | , , , , , , , , , , |
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| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Borntraeger
2025-11-01
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| Ráidu: | Meteorologische Zeitschrift |
| Fáttát: | |
| Liŋkkat: | http://dx.doi.org/10.1127/metz/1266 |
| Fáddágilkorat: |
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