Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Dmitry S. Shaposhnikov"'
Autor:
Dmitry S. Shaposhnikov, Mykhaylo Grygalashvyly, Alexander S. Medvedev, Gerd Reinhold Sonnemann, Paul Hartogh
Publikováno v:
Remote Sensing, Vol 16, Iss 2, p 291 (2024)
Monitoring excited hydroxyl (OH*) airglow is broadly used for characterizing the state and dynamics of the terrestrial atmosphere. Recently, the existence of excited hydroxyl was confirmed using satellite observations in the Martian atmosphere. The l
Externí odkaz:
https://doaj.org/article/cc9d13e15cc54c0f8ca333c56f1b35e6
Autor:
Mykhaylo Grygalashvyly, Dmitry S. Shaposhnikov, Alexander S. Medvedev, Gerd Reinhold Sonnemann, Paul Hartogh
Publikováno v:
Remote Sensing, Vol 14, Iss 16, p 3866 (2022)
Observations of excited hydroxyl (OH*) emissions are broadly used for inferring information about atmospheric dynamics and composition. We present several analytical approximations for characterizing the excited hydroxyl layer in the Martian atmosphe
Externí odkaz:
https://doaj.org/article/38aea883b94e459f9824e6cac757d482
Publikováno v:
Journal of Geophysical Research (Planets)
Simulations with the Max Planck Institute Martian general circulation model for Martian years 28 and 34 reveal details of the water "pump" mechanism and the role of gravity wave (GW) forcing. Water is advected to the upper atmosphere mainly by upward
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::698f24a9355b149adedd4c402e8f859a
http://arxiv.org/abs/2201.05081
http://arxiv.org/abs/2201.05081
Autor:
Paul Hartogh, Alexander Rodin, Dmitry S. Shaposhnikov, Takeshi Kuroda, Alexander S. Medvedev, Anna Fedorova
We present a new implementation of the hydrological cycle scheme into a general circulation model of the Martian atmosphere. The model includes a semi-Lagrangian transport scheme for water vapor and ice, and accounts for microphysics of phase transit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4a7f9fde4e6c27e99926ac25291156ae
http://arxiv.org/abs/2201.05086
http://arxiv.org/abs/2201.05086
We present results of simulations with the Max Planck Institute general circulation model (MPI-MGCM) implementing a hydrological cycle scheme. The simulations reveal a seasonal water "pump" mechanism responsible for the upward transport of water vapo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::11bf692d3a28e6d795371d74ab308287
http://arxiv.org/abs/1904.06391
http://arxiv.org/abs/1904.06391