The CO5 configuration of the 7 km Atlantic Margin Model: large-scale biases and sensitivity to forcing, physics options and vertical resolution

O'Dea, Enda; Furner, Rachel; Wakelin, Sarah ORCID: https://orcid.org/0000-0002-2081-2693; Siddorn, John ORCID: https://orcid.org/0000-0003-3848-8868; While, James; Sykes, Peter; King, Robert; Holt, Jason ORCID: https://orcid.org/0000-0002-3298-8477; Hewitt, Helene. 2017 The CO5 configuration of the 7 km Atlantic Margin Model: large-scale biases and sensitivity to forcing, physics options and vertical resolution. Geoscientific Model Development, 10 (8). 2947-2969. 10.5194/gmd-10-2947-2017

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Official URL: http://dx.doi.org/10.5194/gmd-10-2947-2017

Abstract/Summary

We describe the physical model component of the standard Coastal Ocean version 5 configuration (CO5) of the European north-west shelf (NWS). CO5 was developed jointly between the Met Office and the National Oceanography Centre. CO5 is designed with the seamless approach in mind, which allows for modelling of multiple timescales for a variety of applications from short-range ocean forecasting to climate projections. The configuration constitutes the basis of the latest update to the ocean and data assimilation components of the Met Office's operational Forecast Ocean Assimilation Model (FOAM) for the NWS. A 30.5-year non-assimilating control hindcast of CO5 was integrated from January 1981 to June 2012. Sensitivity simulations were conducted with reference to the control run. The control run is compared against a previous non-assimilating Proudman Oceanographic Laboratory Coastal Ocean Modelling System (POLCOMS) hindcast of the NWS. The CO5 control hindcast is shown to have much reduced biases compared to POLCOMS. Emphasis in the system description is weighted to updates in CO5 over previous versions. Updates include an increase in vertical resolution, a new vertical coordinate stretching function, the replacement of climatological riverine sources with the pan-European hydrological model E-HYPE, a new Baltic boundary condition and switching from directly imposed atmospheric model boundary fluxes to calculating the fluxes within the model using a bulk formula. Sensitivity tests of the updates are detailed with a view toward attributing observed changes in the new system from the previous system and suggesting future directions of research to further improve the system.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.5194/gmd-10-2947-2017
ISSN:	1991-9603
Date made live:	28 Feb 2018 10:52 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/519422

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.5194/gmd-10-2947-2017

ISSN:

1991-9603

Date made live:

28 Feb 2018 10:52 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/519422