the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
DCMIP2016: a review of non-hydrostatic dynamical core design and intercomparison of participating models
Christiane Jablonowski
James Kent
Peter H. Lauritzen
Ramachandran Nair
Kevin A. Reed
Colin M. Zarzycki
David M. Hall
Don Dazlich
Ross Heikes
Celal Konor
David Randall
Thomas Dubos
Yann Meurdesoif
Lucas Harris
Christian Kühnlein
Vivian Lee
Abdessamad Qaddouri
Claude Girard
Marco Giorgetta
Daniel Reinert
Joseph Klemp
Sang-Hun Park
William Skamarock
Hiroaki Miura
Tomoki Ohno
Ryuji Yoshida
Robert Walko
Alex Reinecke
Kevin Viner
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Large volcanic eruptions deposit material into the upper-atmosphere, which is capable of altering temperature and wind patterns of the Earth's atmosphere for years following. This research describes a new method of simulating these effects in an idealized, efficient atmospheric model. A volcanic eruption of sulfur dioxide is described with a simplified set of physical rules, which eventually cools the planetary surface. This model has been designed as a testbed for climate attribution studies.
modelscripts, which reproduce or build on what the Fortran model can do. You could do this same wrapping for any compiled model, not just FV3GFS.
Related subject area
mass-fluxterm. These adjustments enhance the model's performance, offering more reliable temperature and surface flux estimates.
Large volcanic eruptions deposit material into the upper-atmosphere, which is capable of altering temperature and wind patterns of the Earth's atmosphere for years following. This research describes a new method of simulating these effects in an idealized, efficient atmospheric model. A volcanic eruption of sulfur dioxide is described with a simplified set of physical rules, which eventually cools the planetary surface. This model has been designed as a testbed for climate attribution studies.
Cited articles
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