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3 REFERENCE MANUAL FOR THE METEOROLOGICAL RESEARCH INSTITUTE COMMUNITY OCEAN MODEL (MRI.COM) VERSION 3 (MRI.COM) HIROYUKI TSUJINO, TATSUO MOTOI, ICHIRO ISHIKAWA, MIKITOSHI HIRABARA, HIDEYUKI NAKANO, GORO YAMANAKA, TAMAKI YASUDA, AND HIROSHI ISHIZAKI (OCEANOGRAPHIC RESEARCH DEPARTMENT)
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5 Preface It has long been recognized that the role of the ocean in the earth s climate system is conclusively important in such issues as the climate warming, the long-term variability in the air-sea coupled system, meteorological extreme phenomena, and so forth. In these situations, modeling of the ocean has become an indispensable method of studying the climate variability and predicting its future state as well as studying the mechanisms of the oceanic variability itself. The Oceanographic Research Department of the Meteorological Research Institute (MRI) developed its original, general-purpose numerical ocean model, the Meteorological Research Institute Community Ocean Model (MRI.COM), in the early 2000s for both the research work in MRI and operational work in the Japan Meteorological Agency (JMA) by combining two ocean models developed for their research work. The ocean modeling activities are maintained under MRI research programs Development of a high-resolution (eddy-resolving) ocean general circulation model and study on formation, maintenance, and variation mechanisms of water masses based on the model (fiscal years 2003 through 2007), Development of an ocean environmental model and assimilation system and study on variation mechanisms of the ocean environment -feasibility study- (fiscal year 2008), and Development of ocean environmental forecasting methods (started from fiscal year 2009). The present publication is the first English version of the MRI.COM manual and has been improved from the Japanese version published in 2005 by including newly developed parts. The ocean modeling study in MRI began in the late 1970s for investigating the variability of the Kuroshio south of Japan. First, an ocean model with the primitive-equation system developed by former Prof. K. Takano in UCLA, USA, was introduced. Another ocean model was then introduced slightly later in It was similar to the former but developed by an ocean research group in the University of Tokyo. Since that time, the two ocean models with different codes have been improved in parallel in MRI for various purposes. The former model from UCLA has been vigorously optimized to exhibit a high computational efficiency in vector machines, and has been used in experiments with long-term integrations. The latter model from the University of Tokyo incorporated many options from the early stage, such as a surface mixed layer model, an isopycnal diffusion scheme, and a simple sea ice process, for various research and operational purposes. In the early 1990s, the first coupled ocean-atmosphere model experiment was conducted through cooperation between the Oceanographic Research Department and the Climate Research Department, MRI, to simulate El Nino phenomenon. Since then, construction of a climate model synthesizing atmosphere, ocean, sea ice, and land surface has been strongly desired both for research and operational work associated with climate warming projection and seasonal forecasts, including the ENSO cycle prediction. To this end, development of a new, general-purpose ocean model, MRI.COM, which could provide the oceanic part of the synthetic climate model, has been initiated based on the two ocean models used so far to achieve efficiency in model improvement and management and to integrate their merits. In designing the new model, the main frame of the former model and the various physical options of the latter model were transferred to the new model, and many newly developed physical processes and schemes were added. The first Japanese version of the MRI.COM manual was published in 2005 and the model has been continuously updated through further improvements in physical processes and addition of new processes. One of the most i
6 pronounced improvements is the introduction of the chemical and biogeochemical processes associated with the oceanic carbon cycle. This is continuing even now and will be finished in a few years. MRI.COM has been developed along with its own usage as a part of the climate model and the ocean data assimilation system in MRI as well as stand-alone experiments and has already achieved many satisfactory results. Based on our experiences, we believe MRI.COM is one of the best ocean models in the world. We thank the present and past participants in the model development for their great deal of efforts and help. We hope MRI.COM and the present manual will contribute to research work in the fields of climatology, oceanography, and environmental sciences in domestic and foreign institutions as well as to the research and operational work in MRI and JMA. Hiroshi Ishizaki Director Oceanographic Research Department ii
7 2000 (MRI.COM) UCLA UCLA ENSO 1990 ENSO 2 2 UCLA 2005 iii
8 MRI.COM iv
9 Abstract About this manual and MRI.COM This technical report is a manual of the Meteorological Research Institute Community Ocean Model (MRI.COM). MRI.COM is an ocean general circulation model developed and maintained at the Meteorological Research Institute (MRI) of the Japan Meteorological Agency (JMA). As the name suggests, it has been used for studying large scale oceanic phenomena and as the oceanic part of the coupled climate models developed at MRI. The current version of MRI.COM is version 3. Version 1 (developed around 2000) was intended to present a prototype. Efforts were devoted to combining the two ocean models used until then in MRI. For this reason, users at that time tended to be restricted to MRI research scientists who were committed to the development. Thus, users were deeply knowledgeable about the model. Version 2 (early 2000s) was intended for use in the operational forecasting system in JMA. Since the number of users without direct experience in developing models was expected to increase, the developers decided to write a detailed manual for that version. The Japanese version was published in 2005 (Ishikawa et al., 2005) and eventually became the prototype of this manual. Version 3 was intended for use as an oceanic component of the Earth System Model of MRI (MRI-ESM1; Yukimoto et al., 2010). One of the reasons for creating a new version was that the definition of vertical grid arrangement was modified during the development. MRI plans to participate in the phase five of the Coupled Model Intercomparison Project (CMIP5) using MRI-ESM1, and its results on the future projection are expected to be used by a wide range of communities, so we decided to prepare a detailed description of its oceanic component in English. Note that the purpose of this manual is to present a detailed description of a particular model system. The mathematical expressions of processes, the parameterization methods, and the numerical algorithms presented here follow those adopted in the latest code. They are largely state-of-the-art, but this does not necessarily mean that they are the complete reflections of physical, mathematical, and numerical integrity. Every method is subject to possible sophistication. We welcome critical comments and suggestions from any reader or user, which we believe are necessary for further improvement. For a more general or detailed description of OGCMs, please refer to textbooks by Griffies (2004) and Kantha and Clayson (2000). The former thoroughly describes the fundamentals of OGCMs, and the latter concisely summarizes the modeling of various oceanic processes such as tide and sea ice. Organization Chapter 1 introduces OGCMs and MRI.COM. It also presents the classification of OGCMs and the status of MRI.COM with respect to the state-of-the-art OGCMs. v
10 Part I describes the model configuration. Governing equations are derived in Chapter 2, and the spatial grid arrangement and definition of continuity equations for unit grid cells are presented in Chapter 3. Part II describes the dynamical core. The method of solving the barotropic and the baroclinic part of the momentum equation are presented in Chapters 4 and 5, respectively. The method of solving the advection-diffusion equation for tracers (temperature and salinity) is presented in Chapter 6. Part III describes additional processes. Surface mixed-layer models are presented in Chapter 7, surface fluxes in Chapter 8, sea ice in Chapter 9, bottom boundary layer parameterization in Chapter 10, and biogeochemical models are presented in Chapter 11. Part IV contains miscellaneous topics. Basics of the finite difference method are presented in Chapter 12, some high-accuracy advection schemes are presented in Chapter 13, general orthogonal curvilinear coordinates and related calculus are introduced in Chapter 14, how to construct a pair of nested-grid models is presented in Chapter 15, and user s guide to construct and run a model is presented in Chapter 16. Each chapter is almost independent from other chapters. Thus the readers might be able to understand the contents of each chapter without referring to other chapters. However, reading Part I will give the readers the background to help understand the remainder of this manual. The following are some comments about the notations used throughout this manual. The characters and expressions in Courier fonts are adopted from program codes. The subscripts and indices used in discrete equations are intended to express staggered grid arrangements. They do not necessarily correspond to the array indices in program codes. References Griffies, S. M., 2004: Fundamentals of ocean climate models, Princeton University Press, 518pp. Ishikawa, I., H. Tsujino, M. Hirabara, H. Nakano, T. Yasuda, and H. Ishizaki, 2005: Meteorological Research Institute Community Ocean Model (MRI.COM) Manual, Technical Reports of the Meteorological Research Institute, No.47, 189pp. Kantha, L., and C. Clayson, 2000: Numerical models of ocean and oceanic processes, International Geophysics Series, Vol. 66, 940pp. Yukimoto, S., and coauthors, 2010: Meteorological Research Institute-Earth System Model v1 (MRI-ESM1) - Model Description -, Technical Reports of the Meteorological Research Institute, No.64, in press. vi
11 MRI.COM (MRI.COM) MRI.COM MRI.COM MRI-ESM1; Yukimoto et al., 2010 MRI-ESM1 CMIP5 Griffies (2004) Kantha and Clayson (2000) 1 MRI.COM MRI.COM vii
12 I 2 3 II III IV I (Courier) ( ) References Griffies, S. M., 2004: Fundamentals of ocean climate models, Princeton University Press, 518pp. 2005: (MRI.COM) pp. Kantha, L., and C. Clayson, 2000: Numerical models of ocean and oceanic processes, International Geophysics Series, Vol. 66, 940pp. Yukimoto, S., and coauthors, 2010: Meteorological Research Institute-Earth System Model v1 (MRI-ESM1) - Model Description -, Technical Reports of the Meteorological Research Institute, No.64, in press. viii
13 Contents Chapter 1 OGCMs and MRI.COM What do OGCMs cover? Classification of OGCMs Z-coordinate models (z-models) Sigma-coordinate models (σ-models) Isopycnal-coordinate models (ρ-models) About MRI.COM Future of OGCMs and MRI.COM... 5 Part I Configuration 7 Chapter 2 Governing Equations Formulation Coordinate System Momentum Equation Continuity equation Temperature and salinity equation Equation of state of sea water Boundary conditions Acceleration method Numerical Methods Discretization Momentum equation Continuity equation Temperature and salinity equation Equation of state Appendix Physical constants Chapter 3 Spatial grid arrangement and definition of continuity equation Horizontal grid arrangement Vertical grid arrangement Indices and symbols Continuity equation Calculation of area General orthogonal coordinates Geographic coordinate ix
14 Part II Main Processes 37 Chapter 4 Equations of motion (barotropic component) Governing equations Time integration Prognostics of physical properties in the uppermost layer Standard scheme Locally conserved scheme (option FSMOM) Introduction of σ-coordinates near the sea surface Formulation of σ-layer model Governing equations in the σ-coordinates Redistribution of tracers among the σ-layers Chapter 5 Equations of motion (baroclinic component) Advection terms Vertical mass fluxes and its momentum advection Horizontal mass flux and its momentum advection Viscosity Horizontal viscosity Horizontal anisotropic viscosity Smagorinsky parameterization for horizontal viscosity Discretization Vertical viscosity Bottom friction Chapter 6 Temperature and salinity equations Flux form Advection Diffusion Vertical diffusion Harmonic horizontal diffusion Biharmonic horizontal diffusion Isopycnal diffusion Gent and McWilliams parameterization Anisotropic Gent-McWilliams scheme Convective adjustment Algorithm Numerical procedure Part III Additional Processes 81 Chapter 7 Mixed layer model Mellor and Yamada s Turbulence Closure Model Turbulence Closure Model x
15 7.1.2 Level 2.5 Model Implementation Turbulent mixed layer model by Noh and Kim (1999) Fundamental equation Implementation K Profile Parameterization (KPP) Outline Monin-Obukhov similarity law Coefficients of vertical viscosity and diffusivity Coefficients of vertical viscosity and diffusion at the base of the mixed layer Thickness of the mixed layer Mixing due to shear instability Nonlocal Transport Chapter 8 Sea surface fluxes Momentum flux (surface stress) Input of wind stress data Calculating wind stress using a bulk formula Sea surface forcing for temperature and salinity Temperature Salinity Heat flux Shortwave radiation flux Shortwave radiation flux based on chlorophyll concentration Longwave radiation flux Latent and sensible heat fluxes Freshwater flux Introduction Calculating freshwater flux Equivalent surface temperature and salinity fluxes for constant first layer volume Bulk transfer coefficient Formulation of bulk formula Kondo (1975) BULKKONDO Large and Yeager (2004) BULKNCAR Kara et al. (2002) BULKKARA Bulk coefficient over sea ice Work flow in MRI.COM Momentum flux Temperature (heat) flux Salinity and fresh water flux Remarks Appendix Unit of constants Unit of variables xi
16 Chapter 9 Sea ice Outline Thermodynamic processes Formation of new sea ice Air-ice interface Heat balance in the ice interior Ice-ocean interface Archimedes Principle Remapping in thickness space Dynamics Momentum equation for ice pack Stresses at top and bottom Internal stress Boundary conditions Solution procedure Advection Ridging Discretization Advection (MPDATA) Momentum equation Technical issues Source codes Coupling with an atmospheric model Job parameters (namelist) Appendix Saturation water vapor pressure and latent heat Physical constant, parameters Chapter 10 Bottom Boundary Layer (BBL) General description Grid arrangement Pressure gradient terms Eddy effects Usage Usage notes Limit of the area where BBL model should be applied Limits of the BBL Notes for the program code Chapter 11 Biogeochemical model Inorganic carbon cycle and biological model Governing equations Carbon cycle component Air-sea gas exchange fluxes at the sea surface (J g ) xii
17 Dilution and concentration effects of evaporation and precipitation on DIC and Alk Obata and Kitamura model NPZD model Description of each term Primary Production Variation of DIC and Alk due to biological activity Usage Program structure Part IV Miscellaneous 169 Chapter 12 Basics of the finite difference method Diffusion equation Finite difference expressions for time derivatives Finite difference expression for space derivatives Finite differencing of advection-diffusion equation Implicit method for vertical diffusion equation A solution of tri-diagonal matrix Chapter 13 Tracer advection schemes QUICKEST for vertical advection UTOPIA for horizontal advection Second Order Moment (SOM) scheme Outline Calculating SOM advection in MRI.COM Chapter 14 Generalized orthogonal curvilinear coordinate grids Outline Generation of orthogonal coordinate system using conformal mapping Rotation of vector Mapping a quantity from geographic coordinates to transformed coordinates Vector operation and differentiation in a general orthogonal coordinate system Chapter 15 Nesting Feature Low-resolution model High-resolution model Required data Creating data Usage Compilation Running the models Program structure xiii
18 Chapter 16 User s Guide Model setup Files needed for compilation Compilation of the model Preparation of input data files for execution Topographic and grid spacing data Climatological data Nudging (body forcing) data Atmospheric forcing data Execution Structure of output files Snapshot (restart) Averaged value (history) Appendix Model options xiv
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Meteorological Research Institute Community Ocean Model (MRI.COM) Manual (MRI.COM) Ichiro Ishikawa, Hiroyuki Tsujino, Mikitoshi Hirabara, Hideyuki Nakano, Tamaki Yasuda, and Hiroshi Ishizaki MRI Community
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Studies of Foot Form for Footwear Design (Part 9) : Characteristics of the Foot Form of Young and Elder Women Based on their Sizes of Ball Joint Girth
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Yamagata Journal of Health Sciences, Vol. 16, 2013 Tamio KEITOKU 1 2 Katsuko TANNO 3 Kiyoko ARIMA 4 Noboru CHIBA 1 Abstract The present study aimed to
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The Effect of the Circumferential Temperature Change on the Change in the Strain Energy of Carbon Steel during the Rotatory Bending Fatigue Test by Ch
The Effect of the Circumferential Temperature Change on the Change in the Strain Energy of Carbon Steel during the Rotatory Bending Fatigue Test by Chikara MINAMISAWA, Nozomu AOKI (Department of Mechanical
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An Application of Multiple Induction Motor Control with a Single Inverter to an Unmanned Vehicle Propulsion Akira KUMAMOTO* and Yoshihisa HIRANE* This paper is concerned with a new scheme of independent
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Abstract The main theme of this paper is the effect on trade caused by the process of establishing the Chubu Region Scheme as the third broad economic area in Japan followed by the Tokyo Metropolitan Area
A comparison of abdominal versus vaginal hysterectomy for leiomyoma and adenomyosis Kenji ARAHORI, Hisasi KATAYAMA, Suminori NIOKA Department of Obstetrics and Gnecology, National Maizuru Hospital,Kyoto,
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The Effect of Sprint Drills for Improving Short Sprinting Ability of University Baseball Players AKAIKE, Kohei The ability to generate speed during short sprints is one of the most important abilities
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suda Open University 2019.9.28-12.16 Global Education and Sustainable Development Program An inter-disciplinary program for adult learners interested in learning about current global issues and civil society
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