Modelling mid-Pliocene climate with COSMOS

In this manuscript we describe the experimental procedure employed at the Alfred Wegener Institute in Germany in the preparation of the simulations for the Pliocene Model Intercomparison Project (PlioMIP). We present a description of the utilized Community Earth System Models (COSMOS, version: COSMO...

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Main Authors: C. Stepanek, G. Lohmann
Format: Article
Language:English
Published: Copernicus Publications 2012-10-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/5/1221/2012/gmd-5-1221-2012.pdf
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author C. Stepanek
G. Lohmann
author_facet C. Stepanek
G. Lohmann
author_sort C. Stepanek
collection DOAJ
description In this manuscript we describe the experimental procedure employed at the Alfred Wegener Institute in Germany in the preparation of the simulations for the Pliocene Model Intercomparison Project (PlioMIP). We present a description of the utilized Community Earth System Models (COSMOS, version: COSMOS-landveg r2413, 2009) and document the procedures that we applied to transfer the Pliocene Research, Interpretation and Synoptic Mapping (PRISM) Project mid-Pliocene reconstruction into model forcing fields. The model setup and spin-up procedure are described for both the paleo- and preindustrial (PI) time slices of PlioMIP experiments 1 and 2, and general results that depict the performance of our model setup for mid-Pliocene conditions are presented. The mid-Pliocene, as simulated with our COSMOS setup and PRISM boundary conditions, is both warmer and wetter in the global mean than the PI. The globally averaged annual mean surface air temperature in the mid-Pliocene standalone atmosphere (fully coupled atmosphere-ocean) simulation is 17.35 °C (17.82 °C), which implies a warming of 2.23 °C (3.40 °C) relative to the respective PI control simulation.
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spelling doaj.art-103bb8cfb352443bac6dfef26b3cb43b2022-12-22T03:18:43ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032012-10-01551221124310.5194/gmd-5-1221-2012Modelling mid-Pliocene climate with COSMOSC. StepanekG. LohmannIn this manuscript we describe the experimental procedure employed at the Alfred Wegener Institute in Germany in the preparation of the simulations for the Pliocene Model Intercomparison Project (PlioMIP). We present a description of the utilized Community Earth System Models (COSMOS, version: COSMOS-landveg r2413, 2009) and document the procedures that we applied to transfer the Pliocene Research, Interpretation and Synoptic Mapping (PRISM) Project mid-Pliocene reconstruction into model forcing fields. The model setup and spin-up procedure are described for both the paleo- and preindustrial (PI) time slices of PlioMIP experiments 1 and 2, and general results that depict the performance of our model setup for mid-Pliocene conditions are presented. The mid-Pliocene, as simulated with our COSMOS setup and PRISM boundary conditions, is both warmer and wetter in the global mean than the PI. The globally averaged annual mean surface air temperature in the mid-Pliocene standalone atmosphere (fully coupled atmosphere-ocean) simulation is 17.35 °C (17.82 °C), which implies a warming of 2.23 °C (3.40 °C) relative to the respective PI control simulation.http://www.geosci-model-dev.net/5/1221/2012/gmd-5-1221-2012.pdf
spellingShingle C. Stepanek
G. Lohmann
Modelling mid-Pliocene climate with COSMOS
Geoscientific Model Development
title Modelling mid-Pliocene climate with COSMOS
title_full Modelling mid-Pliocene climate with COSMOS
title_fullStr Modelling mid-Pliocene climate with COSMOS
title_full_unstemmed Modelling mid-Pliocene climate with COSMOS
title_short Modelling mid-Pliocene climate with COSMOS
title_sort modelling mid pliocene climate with cosmos
url http://www.geosci-model-dev.net/5/1221/2012/gmd-5-1221-2012.pdf
work_keys_str_mv AT cstepanek modellingmidplioceneclimatewithcosmos
AT glohmann modellingmidplioceneclimatewithcosmos