The path to CAM6: coupled simulations with CAM5.4 and CAM5.5
This paper documents coupled simulations of two developmental versions of the Community Atmosphere Model (CAM) towards CAM6. The configuration called CAM5.4 introduces new microphysics, aerosol, and ice nucleation changes, among others to CAM. The CAM5.5 configuration represents a more radical...
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doaj-d6a7755306a94c02999ccf99677dba8e2020-11-24T22:43:33ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032018-01-011123525510.5194/gmd-11-235-2018The path to CAM6: coupled simulations with CAM5.4 and CAM5.5P. A. Bogenschutz0P. A. Bogenschutz1A. Gettelman2C. Hannay3V. E. Larson4R. B. Neale5C. Craig6C.-C. Chen7Lawrence Livermore National Laboratory, Livermore, CA, USANational Center for Atmospheric Research, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USAUniversity of Wisconsin-Milwaukee, Milwaukee, WI, USANational Center for Atmospheric Research, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USAThis paper documents coupled simulations of two developmental versions of the Community Atmosphere Model (CAM) towards CAM6. The configuration called CAM5.4 introduces new microphysics, aerosol, and ice nucleation changes, among others to CAM. The CAM5.5 configuration represents a more radical departure, as it uses an assumed probability density function (PDF)-based unified cloud parameterization to replace the turbulence, shallow convection, and warm cloud macrophysics in CAM. This assumed PDF method has been widely used in the last decade in atmosphere-only climate simulations but has never been documented in coupled mode. Here, we compare the simulated coupled climates of CAM5.4 and CAM5.5 and compare them to the control coupled simulation produced by CAM5.3. We find that CAM5.5 has lower cloud forcing biases when compared to the control simulations. Improvements are also seen in the simulated amplitude of the Niño-3.4 index, an improved representation of the diurnal cycle of precipitation, subtropical surface wind stresses, and double Intertropical Convergence Zone biases. Degradations are seen in Amazon precipitation as well as slightly colder sea surface temperatures and thinner Arctic sea ice. Simulation of the 20th century results in a credible simulation that ends slightly colder than the control coupled simulation. The authors find this is due to aerosol indirect effects that are slightly stronger in the new version of the model and propose a solution to ameliorate this. Overall, in these early coupled simulations, CAM5.5 produces a credible climate that is appropriate for science applications and is ready for integration into the National Center for Atmospheric Research's (NCAR's) next-generation climate model.https://www.geosci-model-dev.net/11/235/2018/gmd-11-235-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
P. A. Bogenschutz P. A. Bogenschutz A. Gettelman C. Hannay V. E. Larson R. B. Neale C. Craig C.-C. Chen |
spellingShingle |
P. A. Bogenschutz P. A. Bogenschutz A. Gettelman C. Hannay V. E. Larson R. B. Neale C. Craig C.-C. Chen The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 Geoscientific Model Development |
author_facet |
P. A. Bogenschutz P. A. Bogenschutz A. Gettelman C. Hannay V. E. Larson R. B. Neale C. Craig C.-C. Chen |
author_sort |
P. A. Bogenschutz |
title |
The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 |
title_short |
The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 |
title_full |
The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 |
title_fullStr |
The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 |
title_full_unstemmed |
The path to CAM6: coupled simulations with CAM5.4 and CAM5.5 |
title_sort |
path to cam6: coupled simulations with cam5.4 and cam5.5 |
publisher |
Copernicus Publications |
series |
Geoscientific Model Development |
issn |
1991-959X 1991-9603 |
publishDate |
2018-01-01 |
description |
This paper documents coupled simulations of two developmental
versions of the Community Atmosphere Model (CAM) towards CAM6. The
configuration called CAM5.4 introduces new microphysics, aerosol,
and ice nucleation changes, among others to CAM. The CAM5.5
configuration represents a more radical departure, as it uses an
assumed probability density function (PDF)-based unified cloud parameterization to replace the
turbulence, shallow convection, and warm cloud macrophysics in CAM.
This assumed PDF method has been widely used in the last decade in
atmosphere-only climate simulations but has never been documented
in coupled mode. Here, we compare the simulated coupled climates of
CAM5.4 and CAM5.5 and compare them to the control coupled simulation
produced by CAM5.3. We find that CAM5.5 has lower cloud forcing
biases when compared to the control simulations. Improvements are
also seen in the simulated amplitude of the Niño-3.4 index,
an improved representation of the diurnal cycle of precipitation,
subtropical surface wind stresses, and double Intertropical
Convergence Zone biases. Degradations are seen in Amazon
precipitation as well as slightly colder sea surface temperatures
and thinner Arctic sea ice. Simulation of the 20th century results
in a credible simulation that ends slightly colder than the control
coupled simulation. The authors find this is due to aerosol
indirect effects that are slightly stronger in the new version of
the model and propose a solution to ameliorate this. Overall, in
these early coupled simulations, CAM5.5 produces a credible climate
that is appropriate for science applications and is ready for
integration into the National Center for Atmospheric Research's
(NCAR's) next-generation climate model. |
url |
https://www.geosci-model-dev.net/11/235/2018/gmd-11-235-2018.pdf |
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