Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Miguel Andrés-Martínez"'
Publikováno v:
Journal of the Franklin Institute. 360:6880-6905
Autor:
Jan Streffing, Dmitry Sidorenko, Tido Semmler, Lorenzo Zampieri, Patrick Scholz, Miguel Andrés-Martínez, Nikolay Koldunov, Thomas Rackow, Joakim Kjellsson, Helge Goessling, Marylou Athanase, Qiang Wang, Jan Hegewald, Dmitry V. Sein, Longjiang Mu, Uwe Fladrich, Dirk Barbi, Paul Gierz, Sergey Danilov, Stephan Juricke, Gerrit Lohmann, Thomas Jung
Publikováno v:
eISSN
EPIC3Geoscientific Model Development, Copernicus GmbH, 15(16), pp. 6399-6427, ISSN: 1991-959X
EPIC3EGUsphere, Copernicus
EPIC3Geoscientific Model Development, Copernicus GmbH, 15(16), pp. 6399-6427, ISSN: 1991-959X
EPIC3EGUsphere, Copernicus
We developed a new version of the Alfred Wegener Institute Climate Model (AWI-CM3), which has higher skills in representing the observed climatology and better computational efficiency than its predecessors. Its ocean component FESOM2 (Finite-volumE
Autor:
Svetlana N. Losa, Longjiang Mu, Marylou Athanase, Jan Streffing, Miguel Andrés-Martínez, Lars Nerger, Tido Semmler, Dmitry Sidorenko, Helge F. Goessling
Publikováno v:
EPIC3
Assimilation of sea ice and ocean observational data into coupled sea-ice, ocean and atmosphere models is known as an efficient approach for providing a reliable sea-ice prediction (Mu et al. 2022). However, implementations of the data assimilation i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::314dbd42c681f831422adef948118a5d
https://hdl.handle.net/10013/epic.45d71580-aec9-4c20-bf72-cea7c3181983
https://hdl.handle.net/10013/epic.45d71580-aec9-4c20-bf72-cea7c3181983
Autor:
Marylou Athanase, Merle Schwager, Jan Streffing, Miguel Andrés-Martínez, Svetlana Loza, Helge Goessling
The Arctic sea ice cover and thickness have significantly declined since the 1970s, while exhibiting large interannual variability. Snow cover on sea ice, acting as an insulating barrier, was shown to be instrumental in driving the variability and tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08ec08069ad48f5ffc182e9ee2d0ee43
https://doi.org/10.5194/egusphere-egu22-5836
https://doi.org/10.5194/egusphere-egu22-5836
Publikováno v:
Tectonics
Tectonics, American Geophysical Union (AGU), 2019, 38 (2), pp.641-665. ⟨10.1029/2018TC005346⟩
Tectonics, American Geophysical Union (AGU), 2019, 38 (2), pp.641-665. ⟨10.1029/2018TC005346⟩
International audience; Erosion and deposition redistribute mass as a continental rift evolves, which modifies crustal loads and influences subsequent deformation. Surface processes therefore impact both the architecture and the evolution of passive
During the last two decades, modern societies have gradually understood the urge to tackle the climate change challenge, and consequently, a growing number of national and international initiatives have been launched with the aim of better understand
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3be9fc7c52c7e10e2bfb5cff2d774640
https://doi.org/10.5194/egusphere-egu21-5489
https://doi.org/10.5194/egusphere-egu21-5489
Publikováno v:
Tectonics
Tectonics, American Geophysical Union (AGU), 2020, 39 (12), pp.e2020TC006255. ⟨10.1029/2020TC006255⟩
Tectonics, American Geophysical Union (AGU), 2020, 39 (12), pp.e2020TC006255. ⟨10.1029/2020TC006255⟩
International audience; Synrift stratigraphy and the distribution of breakup-related erosional unconformities vary vastly between passive margins and cannot be explained by classical rifting models. Here we use numerical modeling to predict their spa
Autor:
Marco Thoaldo Romeiro, Marta Pérez-Gussinyé, Mario Araujo, Jason Phipps Morgan, Miguel Andrés-Martínez, Elena Ros
Publikováno v:
Geochemistry, Geophysics, Geosystems. 18:4538-4557
Publikováno v:
Physics of the Earth and Planetary Interiors. 246:41-51
The surface of the solid Earth is effectively stress free in its subaerial portions, and hydrostatic beneath the oceans. Unfortunately, this type of boundary condition is difficult to treat computationally, and for computational convenience, numerica