A coupled experiment with LICOM2 as the ocean component of CESM1

In the present study, the LASG/IAP Climate system Ocean Model version 2 (LICOM2) was implemented to replace the original ocean component in the Community Earth System Model version 1.0.4 (CESM1) to form a new coupled model referred to as CESM1+LICOM2. The simulation results from a 300-yr preindustrial experiment by using this model were evaluated against both observations and the Flexible Global Ocean-Atmosphere-Land System Model with grid-atmospheric model version 2 (FGOALS-g2). It was found that CESM1+LICOM2 simulates well the mean features of the ocean, sea ice, and atmosphere, relative to models used in the Coupled Model Intercomparison Experiment (CMIP5), when compared with observations. The spatial distribution of SST bias in CESM1+LICOM2 is similar to that in the Community Climate System Model version 4 (CCSM4). The simulated climate variabilities, such as ENSO and Pacific decadal oscillation, are also reasonably simulated when compared with observations. The successful implementation of LICOM2 in the CESM1 framework greatly enhances the capability of LICOM2 in conducting high-resolution simulations and model tuning. Compared with FGOALS-g2, the simulations of both SST and Atlantic meridional overturning circulation are significantly improved in CESM1+LICOM2. The former can be mainly attributed to the atmospheric model, and the latter to the improvement in the parameterization of diapycnal mixing. The study provides a base to further improve the present version of LICOM and its functionalities in the coupled model FGOALS at both low and high resolutions.

[1]  William E. Johns,et al.  Continuous, Array-Based Estimates of Atlantic Ocean Heat Transport at 26.5°N , 2011 .

[2]  P. Gent,et al.  Isopycnal mixing in ocean circulation models , 1990 .

[3]  J. Ohlmann,et al.  Ocean Radiant Heating in Climate Models , 2003 .

[4]  A. Gnanadesikan Numerical issues for coupling biological models with isopycnal mixing schemes , 1999 .

[5]  Markus Jochum,et al.  Impact of latitudinal variations in vertical diffusivity on climate simulations , 2009 .

[6]  J. Marotzke,et al.  Temporal variability of the Atlantic meridional overturning circulation at 26.5 degrees N. , 2007, Science.

[7]  Mariana Vertenstein,et al.  A new flexible coupler for earth system modeling developed for CCSM4 and CESM1 , 2012, Int. J. High Perform. Comput. Appl..

[8]  G. Backus Determination of the external geomagnetic field from intensity measurements , 1974 .

[9]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[10]  T. Zhou,et al.  Chinese contribution to CMIP5: An overview of five Chinese models’ performances , 2014, Journal of Meteorological Research.

[11]  G. Danabasoglu,et al.  The Community Climate System Model Version 4 , 2011 .

[12]  K. Speer,et al.  Global Ocean Meridional Overturning , 2007 .

[13]  C. Mechoso,et al.  A global perspective on CMIP5 climate model biases , 2014 .

[14]  Elizabeth C. Kent,et al.  Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century , 2003 .

[15]  Michael Steele,et al.  PHC: A Global Ocean Hydrography with a High-Quality Arctic Ocean , 2001 .

[16]  Xuehong Zhang,et al.  A flexible coupled ocean-atmosphere general circulation model , 2002 .

[17]  Christopher A. Sims,et al.  Computer Simulation of Large-Scale Econometric Models: Project Link , 1987 .

[18]  J. Wallace,et al.  A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production , 1997 .

[19]  William E. Johns,et al.  Temporal Variability of the Atlantic Meridional Overturning Circulation at 26.5°N , 2007, Science.

[20]  J. Thepaut,et al.  The ERA‐Interim reanalysis: configuration and performance of the data assimilation system , 2011 .

[21]  Thomas M. Smith,et al.  Improvements to NOAA’s Historical Merged Land–Ocean Surface Temperature Analysis (1880–2006) , 2008 .

[22]  L. St. Laurent,et al.  Estimating tidally driven mixing in the deep ocean , 2002 .

[23]  V. Canuto,et al.  Ocean Turbulence. Part II: Vertical Diffusivities of Momentum, Heat, Salt, Mass, and Passive Scalars , 2002 .

[24]  Donald J. Cavalieri,et al.  30‐Year satellite record reveals contrasting Arctic and Antarctic decadal sea ice variability , 2003 .

[25]  C. Paulson,et al.  Irradiance Measurements in the Upper Ocean , 1977 .

[26]  Frank O. Bryan,et al.  Coordinated Ocean-ice Reference Experiments (COREs) , 2009 .

[27]  M. Brandon,et al.  Transport and variability of the Antarctic Circumpolar Current in Drake Passage , 2003 .

[28]  Wei Liu,et al.  Assessing the stability of the Atlantic meridional overturning circulation of the past, present, and future , 2014, Journal of Meteorological Research.

[29]  J. Pelegrí,et al.  Meridional Overturning Transports at 7.5N and 24.5N in the Atlantic Ocean during 1992-93 and 2010-11 , 2014 .

[30]  J. Morison,et al.  Hydrography of the upper Arctic Ocean measured from the nuclear submarine U.S.S. Pargo , 1998 .

[31]  P. Lin,et al.  Long-term behaviors of two versions of FGOALS2 in preindustrial control simulations with implications for 20th century simulations , 2013, Advances in Atmospheric Sciences.

[32]  P. Lin,et al.  Oceanic climatology in the coupled model FGOALS-g2: Improvements and biases , 2013, Advances in Atmospheric Sciences.

[33]  J. C. Comiso,et al.  Bootstrap Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS, Version 3 , 2017 .

[34]  Thomas M. Smith,et al.  Interdecadal Changes of 30-Yr SST Normals during 1871–2000 , 2003 .

[35]  Pengfei Lin,et al.  The baseline evaluation of LASG/IAP climate system ocean model (LICOM) version 2 , 2012, Acta Meteorologica Sinica.

[36]  K. Speer,et al.  Closure of the meridional overturning circulation through Southern Ocean upwelling , 2012 .

[37]  M. S. Dubovikov,et al.  Ocean Turbulence I: One-Point Closure Model Momentum and Heat Vertical Diffusivities , 2001 .

[38]  P. Lin,et al.  Response of sea surface temperature to chlorophyll-a concentration in the tropical Pacific: Annual mean, seasonal cycle, and interannual variability , 2011 .

[39]  Gokhan Danabasoglu,et al.  Sensitivity of the global ocean circulation to parameterizations of mesoscale tracer transports , 1995 .

[40]  P. Xie,et al.  Global Precipitation: A 17-Year Monthly Analysis Based on Gauge Observations, Satellite Estimates, and Numerical Model Outputs , 1997 .

[41]  M. Redi Oceanic Isopycnal Mixing by Coordinate Rotation , 1982 .

[42]  Minghua Zhang,et al.  Toward understanding the double Intertropical Convergence Zone pathology in coupled ocean‐atmosphere general circulation models , 2007 .