Not exact matches
NASA's Goddard Earth Observing System
Version 5 (GEOS - 5)
model simulates the atmosphere in 3 - D, which allows the research team to follow
atmospheric gases from their sources on the ground through their journey to the upper atmosphere.
In his career - long support of CESM, Rasch was formerly co-chair of the
Atmospheric Model Working Group and team lead for the
version five development of CESM's
atmospheric component, called the Community Atmosphere
Model (CAM5).
ERA - 20C was produced with the same surface and
atmospheric forcings as the final
version of the
atmospheric model integration ERA - 20CM.
The resolution of the
atmospheric model is set to TL159L91 (IFS
version 41r2), which corresponds to a 1.125 ° horizontal grid (125 km) with 91 vertical levels going up to 0.1 hPa.
We are investigating the effects of long - term emissions trends using a
version of the GISS climate
model that includes
atmospheric chemistry.
What's new here is the application of a detailed
version of one of the world's premier climate system
models, the CCSM, to understand how rising levels of
atmospheric carbon dioxide affected conditions in the world's oceans and land surfaces enough to trigger a massive extinction hundreds of millions of years ago.»
The experiments were performed with ModelE2, a new
version of the NASA Goddard Institute for Space Sciences (GISS) coupled general circulation
model that includes three different
versions for the
atmospheric composition components: a noninteractive
version (NINT) with prescribed composition and a tuned aerosol indirect effect (AIE), the TCAD
version with fully interactive aerosols, whole - atmosphere chemistry, and the tuned AIE, and the TCADI
version which further includes a parameterized first indirect aerosol effect on clouds.
We use an
atmospheric general circulation
model (AGCM) with a well - resolved stratosphere called the Whole Atmosphere Community Climate Model version 4 (WACCM4; with specified chemis
model (AGCM) with a well - resolved stratosphere called the Whole Atmosphere Community Climate
Model version 4 (WACCM4; with specified chemis
Model version 4 (WACCM4; with specified chemistry).
Each
atmospheric version is coupled to two different ocean general circulation
models: the Russell ocean
model (GISS - E2 - R) and HYCOM (GISS - E2 - H).
So, as a direct result, whatever
atmospheric model is used will reproduce conditions that are in accord with that
version of the climate.
The
model physics is largely based on the Community Climate System Model version 4 (Gent et al. 2011), which includes atmospheric physics of the Community Atmosphere Model version 4 (CAM4)(Neale et al. 2
model physics is largely based on the Community Climate System
Model version 4 (Gent et al. 2011), which includes atmospheric physics of the Community Atmosphere Model version 4 (CAM4)(Neale et al. 2
Model version 4 (Gent et al. 2011), which includes
atmospheric physics of the Community Atmosphere
Model version 4 (CAM4)(Neale et al. 2
Model version 4 (CAM4)(Neale et al. 2013).
Principal changes in the physics in the current
version of the
model are use of a step - mountain C - grid
atmospheric vertical coordinate [109], addition of a drag in the grid - scale momentum equation in both atmosphere and ocean based on subgrid topography variations, and inclusion of realistic ocean tides based on exact positioning of the Moon and Sun.
Trenberth used the
Version 5 RSS - SSM / I data set for
atmospheric water content, q, to claim that it represented a better choice for observing trends in q when validating climate
models.
Researchers investigated the response of Atlantic Meridional Overturning Circulation (AMOC) to the rise of
atmospheric CO2 in the NCAR Climate System
Model version 3, with the focus on the different responses under modern and glacial periods.
Recent calculations of
atmospheric sensitivity to increased concentrations of CO2 in the atmosphere are based on observations and provide values for sensitivity that are much lower than previous
versions that were based on
models.