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Sensitivity studies with the regional climate model REMO

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Summary

A new regional atmospheric model was set up in a joint effort by DKRZ (Deutsches Klimarechenzentrum), DWD (Deutscher Wetterdienst), GKSS (Forschungszentrum Geesthacht) at the MPI (Max-Planck-Institut fuer Meteorologie). This model, called REMO (REgional MOdel) can be used in the weather forecast mode as well as in the climate mode. It is based on the Europa-Model (EM), the main weather forecast model of the new numerical weather prediction system of the Deutscher Wetterdienst. In addition to the physical parameterizations implemented in the EM, REMO has the possibility of using the same physics as the global climate model (MPI) into which it is nested to assess the scale dependence of physical parameterizations within the same dynamical framework.

This paper gives an overview over different case studies investigating the dependence of model results on simulation domain size, horizontal resolution, initial conditions and lateral boundaries especially for long term calculations. A sample of one month long integrations for an arbitrary July month, a four year long run for the Baltic Sea and its drainage basin and two summer seasons of the Indian Monsoon will be used to demonstrate the sensitivity of regional climate model results to different environments.

The sensitivity studies show that it is very important to use realistic large scale driving fields at the lateral boundaries. The regional model results are strongly influenced by the driving fields. The domain size and the simulation length are also influencing the results.

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References

  • Alestalo, M., 1981: The energy budget of the earthatmosphere system in Europe.Tellus,33, 360–371.

    Google Scholar 

  • Bergstroem, S., Carlsson, B., 1993: Hydrology of the Baltic Basin. Inflow of fresh water from rivers and land for the period 1950–1990.SMHI Reports Hydrology,7, 32pp.

    Google Scholar 

  • Creß, A., Majewski, D., Podzun, R., Renner, v., 1995: Simulation of European climate with a limited area model. Part I: Observed boundary conditions.Beitr. Phys. Atmosph.,68, 161–178.

    Google Scholar 

  • Davies, H. C., 1976: A lateral boundary formulation for multi-level prediction models.Quart. J. Roy Meteor. Soc.,102, 405–418.

    Google Scholar 

  • DKRZ, 1994: The ECHAM3 atmospheric general circulation model. Tech. Rep.6.

  • Jacobsen, I., Heise, E., 1982: A new economic method for the computation of the surface temperature in numerical models.Beitr. Phys. Atmos.,55, 128–141.

    Google Scholar 

  • Jones, R. G., Murphy, J. M., Noguer, M., 1995: Simulation of Relimate change over Europe using a nested regional-climate model, I: Assessment of control climate, cicluding sensivity to location of lateral boundaries.Quart. J. Roy. Meteor. Soc.,121, 1413–1449.

    Google Scholar 

  • Legates, D. R., Willmott, C. J., 1990: Mean seasonal and spatial variability in gauge-corrected precipitation.Int. J. Climatol.,10, 111–127.

    Google Scholar 

  • Louis, J. F., 1979: A parametric model of vertical eddy fluxes in the atmosphere.Bound.—Layer Meteorol.,17, 187–202.

    Google Scholar 

  • Machenhauer, B., Windelband, M., Botzet, M., Jones, R. G., Déqué M., 1996: Validation of present-day regional climate simulations over Europe: Nested LAM and variable resolution Global Model simulations with observed or mixed layer ocean boundary conditions. Max-Planck Institut f. Meteorologie, Hamburg, Report No. 191.

    Google Scholar 

  • Majewski, D., 1991: The Europa-Modell of the Deutscher Wetterdienst.Seminar Proceedings ECMWF,2, 147–191

    Google Scholar 

  • Mellor, G. L. Yamada, T., 1974: A hierachy of turbulence closure models for planetary boundary layers.J. Atmos. Sci.,31, 1791–1806.

    Google Scholar 

  • Podzun, R., Creß, A., Majewski, D., Renner, V., 1995: Simulation of European climate with a limited area model. Part II: AGCM boundary conditionsBeitr. Phys. Atmosph.,68, 205–225.

    Google Scholar 

  • Ritter, B., Geleyn, J. F. 1992: A comprehensive radiation scheme for numerical weather prediction models with potential applications in climate simulations.Mon. Wea. Rev.,120, 303–325.

    Google Scholar 

  • Rockel, B., Raschke, E., Weyres, B., 1991: A parameterization of broad band radiative transfer properties of water, ice and mixed clouds.Beitr. Phys. Atmosph.,64, 1–12

    Google Scholar 

  • Simmons, A. J., Burridge, D. M., 1981: An energy and angular-momentum conserving vertical finite-difference scheme and hybrid vertical coordinates.Mon. Wea. Rev.,109, 758–766.

    Google Scholar 

  • Sjoeberg, B. (ed.), 1992:Sea and Coast. National Atlas of Sweden. Stockholm: Almqvist & Wiksell International.

    Google Scholar 

  • Tiedke, M., 1989: A comprehensive mass flux scheme for cumulus parameterization in large-scale models.Mon. Wea. Rev.,117, 1779–1800.

    Google Scholar 

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Jacob, D., Podzun, R. Sensitivity studies with the regional climate model REMO. Meteorl. Atmos. Phys. 63, 119–129 (1997). https://doi.org/10.1007/BF01025368

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  • DOI: https://doi.org/10.1007/BF01025368

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