The Nonhydrostatic ICosahedral Atmospheric Model for CMIP6 HighResMIP simulations (NICAM16-S): experimental design, model description, and impacts of model updates
The Nonhydrostatic ICosahedral Atmospheric Model (NICAM), a global model with an icosahedral grid system, has been under development for nearly two decades. This paper describes NICAM16-S, the latest stable version of NICAM (NICAM.16), modified for the Coupled Model Intercomparison Project Phase 6,...
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Published in | Geoscientific Model Development Vol. 14; no. 2; pp. 795 - 820 |
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Main Authors | , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
04.02.2021
Copernicus Publications |
Subjects | |
Online Access | Get full text |
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Summary: | The Nonhydrostatic ICosahedral Atmospheric Model
(NICAM), a global model with an icosahedral grid system, has been under
development for nearly two decades. This paper describes NICAM16-S, the
latest stable version of NICAM (NICAM.16), modified for the Coupled Model
Intercomparison Project Phase 6, High Resolution Model Intercomparison
Project (HighResMIP). Major updates of NICAM.12, a previous version used
for climate simulations, included updates of the cloud microphysics scheme
and land surface model, introduction of natural and anthropogenic aerosols
and a subgrid-scale orographic gravity wave drag scheme, and improvement of
the coupling between the cloud microphysics and the radiation schemes.
External forcings were updated to follow the protocol of the HighResMIP. A
series of short-term sensitivity experiments were performed to determine and
understand the impacts of these various model updates on the simulated mean
states. The NICAM16-S simulations demonstrated improvements in the ice water
content, high cloud amount, surface air temperature over the Arctic region,
location and strength of zonal mean subtropical jet, and shortwave radiation
over Africa and South Asia. Some long-standing biases, such as the double
intertropical convergence zone and smaller low cloud amount, still exist or
are even worse in some cases, suggesting further necessity for understanding
their mechanisms, upgrading schemes and parameter settings, and
enhancing horizontal and vertical resolutions. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
ISSN: | 1991-9603 1991-959X 1991-962X 1991-9603 1991-962X |
DOI: | 10.5194/gmd-14-795-2021 |