Zobrazeno 1 - 10
of 2 297
pro vyhledávání: '"R Herrington"'
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 16, Iss 7, Pp n/a-n/a (2024)
Abstract Canonical understanding based on general circulation models (GCMs) is that the atmospheric circulation response to midlatitude sea‐surface temperature (SST) anomalies is weak compared to the larger influence of tropical SST anomalies. Howe
Externí odkaz:
https://doaj.org/article/c2c662f12d53404caeb27f1eef303942
Publikováno v:
The Cryosphere, Vol 17, Pp 3803-3828 (2023)
Earth system models (ESMs) can help to improve the understanding of climate-induced cryospheric–hydrological impacts in complex mountain regions, such as High Mountain Asia (HMA). Coarse ESM grids, however, have difficulties in representing cryosph
Externí odkaz:
https://doaj.org/article/0af1f2d50d864ce6913656e352f7383d
Autor:
Adam R. Herrington, Peter H. Lauritzen, Marcus Lofverstrom, William H. Lipscomb, Andrew Gettelman, Mark A. Taylor
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 14, Iss 11, Pp n/a-n/a (2022)
Abstract Six different configurations, a mixture of grids and atmospheric dynamical cores available in the Community Earth System Model, version 2.2 (CESM2.2), are evaluated for their skill in representing the climate of the Arctic and the surface ma
Externí odkaz:
https://doaj.org/article/344ed1292bc447bd8ef334e0bf75a821
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 7, Pp 1894-1916 (2019)
Abstract This paper describes the implementation of a coarser‐resolution physics grid into the Community Atmosphere Model (CAM), containing 59 fewer grid columns than the dynamics grid. The dry dynamics is represented by the spectral element dynami
Externí odkaz:
https://doaj.org/article/02f2f79aae104de0bd79c6dd8f809f9f
Autor:
L. van Kampenhout, A. M. Rhoades, A. R. Herrington, C. M. Zarzycki, J. T. M. Lenaerts, W. J. Sacks, M. R. van den Broeke
Publikováno v:
The Cryosphere, Vol 13, Pp 1547-1564 (2019)
In this study, the resolution dependence of the simulated Greenland ice sheet surface mass balance (GrIS SMB) in the variable-resolution Community Earth System Model (VR-CESM) is investigated. Coupled atmosphere–land simulations are performed on tw
Externí odkaz:
https://doaj.org/article/ff9245d868b64644aa4c4758a8f6e8f2
Autor:
R.A. Howie
Publikováno v:
Mineralogical Magazine. 64:579-580
This latest slim book in this popular series (previous titles include ‘Crystals’, ‘Gemstones’, ‘Meteorites’, and ‘Volcanoes’) presents an attractive combination of colour photographs, maps and diagrams, with a clear, concise yet autho
Autor:
P. H. Lauritzen, R. D. Nair, A. R. Herrington, P. Callaghan, S. Goldhaber, J. M. Dennis, J. T. Bacmeister, B. E. Eaton, C. M. Zarzycki, Mark A. Taylor, P. A. Ullrich, T. Dubos, A. Gettelman, R. B. Neale, B. Dobbins, K. A. Reed, C. Hannay, B. Medeiros, J. J. Benedict, J. J. Tribbia
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 10, Iss 7, Pp 1537-1570 (2018)
Abstract It is the purpose of this paper to provide a comprehensive documentation of the new NCAR (National Center for Atmospheric Research) version of the spectral element (SE) dynamical core as part of the Community Earth System Model (CESM2.0) rel
Externí odkaz:
https://doaj.org/article/5ef923ff2c004d1eb752c501085d603b
Autor:
A. R. Herrington, K. A. Reed
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 10, Iss 2, Pp 560-575 (2018)
Abstract A set of idealized experiments are developed using the Community Atmosphere Model (CAM) to understand the vertical velocity response to reductions in forcing scale that is known to occur when the horizontal resolution of the model is increas
Externí odkaz:
https://doaj.org/article/494622454b5d4b0eace594d2b27ee64b
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.