%0 Journal Article %1 Megann2013GO50 %A Megann, A. %A Storkey, D. %A Aksenov, Y. %A Alderson, S. %A Calvert, D. %A Graham, T. %A Hyder, P. %A Siddorn, J. %A Sinha, B. %D 2013 %I Copernicus Publications %J Geoscientific Model Development Discussions %K ocean colleagues model %N 4 %P 5747--5799 %R 10.5194/gmdd-6-5747-2013 %T GO5.0: The joint NERC-Met Office NEMO global ocean model for use in coupled and forced applications %U http://dx.doi.org/10.5194/gmdd-6-5747-2013 %V 6 %X We describe a new Global Ocean standard configuration (GO5.0) at eddy-permitting resolution, developed jointly between the National Oceanography Centre and the Met Office as part of the Joint Ocean Modelling Programme (JOMP). This programme is a working group of the UK's National Centre for Ocean Forecasting (NCOF) and part of the Joint Weather and Climate Research Programme (JWCRP). The configuration has been developed with the seamless approach to modelling in mind for ocean modelling across timescales and for a range of applications, from short-range ocean forecasting through seasonal forecasting to climate predictions as well as research use. The GO5.0 configuration has been coupled with sea-ice (GSI5.0), atmosphere (GA5.0) and land-surface (GL5.0) configurations to form a standard coupled global model (GC1). The GO5.0 model will become the basis for the ocean model component of the Forecasting Ocean Assimilation Model, which provides forced short-range forecasting services. The global coupled model (GC1) or future releases of it will be used in coupled short-range ocean forecasting, seasonal forecasting, decadal prediction and for climate prediction as part of the UK Earth System Model. <br><br> A 30 yr integration of GO5.0, run with CORE2 surface forcing from 1976 to 2005, is described, and the performance of the model in the final ten years of the integration is evaluated against observations and against a comparable integration of an earlier configuration, GO1. An additional set of 10 yr sensitivity studies, carried out to attribute changes in the model performance to individual changes in the model physics, is also analysed. GO5.0 is found to have substantially reduced subsurface drift above the depth of the thermocline relative to GO1, and also shows a significant improvement in the representation of the annual cycle of surface temperature and mixed-layer depth.

@article{Megann2013GO50, abstract = {We describe a new Global Ocean standard configuration (GO5.0) at eddy-permitting resolution, developed jointly between the National Oceanography Centre and the Met Office as part of the Joint Ocean Modelling Programme (JOMP). This programme is a working group of the UK's National Centre for Ocean Forecasting (NCOF) and part of the Joint Weather and Climate Research Programme (JWCRP). The configuration has been developed with the seamless approach to modelling in mind for ocean modelling across timescales and for a range of applications, from short-range ocean forecasting through seasonal forecasting to climate predictions as well as research use. The GO5.0 configuration has been coupled with sea-ice (GSI5.0), atmosphere (GA5.0) and land-surface (GL5.0) configurations to form a standard coupled global model (GC1). The GO5.0 model will become the basis for the ocean model component of the Forecasting Ocean Assimilation Model, which provides forced short-range forecasting services. The global coupled model (GC1) or future releases of it will be used in coupled short-range ocean forecasting, seasonal forecasting, decadal prediction and for climate prediction as part of the UK Earth System Model. <br><br> A 30 yr integration of GO5.0, run with CORE2 surface forcing from 1976 to 2005, is described, and the performance of the model in the final ten years of the integration is evaluated against observations and against a comparable integration of an earlier configuration, GO1. An additional set of 10 yr sensitivity studies, carried out to attribute changes in the model performance to individual changes in the model physics, is also analysed. GO5.0 is found to have substantially reduced subsurface drift above the depth of the thermocline relative to GO1, and also shows a significant improvement in the representation of the annual cycle of surface temperature and mixed-layer depth.}, added-at = {2018-06-18T21:23:34.000+0200}, author = {Megann, A. and Storkey, D. and Aksenov, Y. and Alderson, S. and Calvert, D. and Graham, T. and Hyder, P. and Siddorn, J. and Sinha, B.}, biburl = {https://www.bibsonomy.org/bibtex/296b15198d14f204d77292ae35ff42798/pbett}, citeulike-article-id = {12803410}, citeulike-linkout-0 = {http://dx.doi.org/10.5194/gmdd-6-5747-2013}, citeulike-linkout-1 = {http://www.geosci-model-dev-discuss.net/6/5747/2013/}, day = 26, doi = {10.5194/gmdd-6-5747-2013}, interhash = {64aae51d35948381ec89759755f214e8}, intrahash = {96b15198d14f204d77292ae35ff42798}, journal = {Geoscientific Model Development Discussions}, keywords = {ocean colleagues model}, month = nov, number = 4, pages = {5747--5799}, posted-at = {2013-11-27 07:50:58}, priority = {2}, publisher = {Copernicus Publications}, timestamp = {2018-06-22T18:33:58.000+0200}, title = {GO5.0: {T}he joint NERC-Met {O}ffice NEMO global ocean model for use in coupled and forced applications}, url = {http://dx.doi.org/10.5194/gmdd-6-5747-2013}, volume = 6, year = 2013 }