Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model

TM2 is a three-dimensional atmospheric transport model which solves the continuity equation for an arbitrary number of atmospheric tracers on an Eulerian grid spanning the entire globe. It is driven by stored meteorological fields from analyses of a weather forecast model or from output of an atmosp...

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Bibliographic Details
Main Authors: Legutke, S., Maier-Reimer, E.
Format: Report
Language:English
Published: 1999
Subjects:
Sea ice
Online Access:http://hdl.handle.net/21.11116/0000-0009-1432-8
http://hdl.handle.net/21.11116/0000-0009-1434-6
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spelling ftpubman:oai:pure.mpg.de:item_3338061 2023-08-27T04:11:54+02:00 Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model Legutke, S. Maier-Reimer, E. 1999 application/pdf http://hdl.handle.net/21.11116/0000-0009-1432-8 http://hdl.handle.net/21.11116/0000-0009-1434-6 eng eng info:eu-repo/semantics/altIdentifier/pissn/0940-9327 http://hdl.handle.net/21.11116/0000-0009-1432-8 http://hdl.handle.net/21.11116/0000-0009-1434-6 info:eu-repo/semantics/openAccess Technical Report / Deutsches Klimarechenzentrum, Hamburg info:eu-repo/semantics/workingPaper 1999 ftpubman 2023-08-02T00:42:15Z TM2 is a three-dimensional atmospheric transport model which solves the continuity equation for an arbitrary number of atmospheric tracers on an Eulerian grid spanning the entire globe. It is driven by stored meteorological fields from analyses of a weather forecast model or from output of an atmospheric general circulation model. Tracer advection is calculated using the “slopes scheme” of Russell and Lerner [1981]. Vertical transport due to convective clouds is computed using a simplified version of the cloud mass flux scheme of Tiedke [1989]. Turbulent vertical transport is calculated by stability dependent vertical diffusion according to the scheme by Louis [1979]. Report Sea ice Max Planck Society: MPG.PuRe
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description TM2 is a three-dimensional atmospheric transport model which solves the continuity equation for an arbitrary number of atmospheric tracers on an Eulerian grid spanning the entire globe. It is driven by stored meteorological fields from analyses of a weather forecast model or from output of an atmospheric general circulation model. Tracer advection is calculated using the “slopes scheme” of Russell and Lerner [1981]. Vertical transport due to convective clouds is computed using a simplified version of the cloud mass flux scheme of Tiedke [1989]. Turbulent vertical transport is calculated by stability dependent vertical diffusion according to the scheme by Louis [1979].
format Report
author Legutke, S.
Maier-Reimer, E.
spellingShingle Legutke, S.
Maier-Reimer, E.
Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
author_facet Legutke, S.
Maier-Reimer, E.
author_sort Legutke, S.
title Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
title_short Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
title_full Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
title_fullStr Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
title_full_unstemmed Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model
title_sort climatology of the hope-g global ocean - sea ice general circulation model
publishDate 1999
url http://hdl.handle.net/21.11116/0000-0009-1432-8
http://hdl.handle.net/21.11116/0000-0009-1434-6
genre Sea ice
genre_facet Sea ice
op_source Technical Report / Deutsches Klimarechenzentrum, Hamburg
op_relation info:eu-repo/semantics/altIdentifier/pissn/0940-9327
http://hdl.handle.net/21.11116/0000-0009-1432-8
http://hdl.handle.net/21.11116/0000-0009-1434-6
op_rights info:eu-repo/semantics/openAccess
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