Development of lake parametrization in the INMCM climate model

International Conference and Early Career Scientists School on Environmental Observations, Modelling and Information Systems

生态环境科学;计算机科学

Bogomolov, V.^1,2 ; Stepanenko, V.^3,4 ; Volodin, E.^5

Institute of Monitoring of Climatic and Ecological Systems, Siberian Branch, Russian Academy of Sciences, 10/3, Academichesky ave., Tomsk, Russia^1

V.E. Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, 1, Academician Zuev square, Tomsk, Russia^2

Research Computing Center, Moscow State University, Leninskiye Gory str., 1, Moscow, Russia^3

Department of Geography, Moscow State University, Leninskiye Gory str., 1, Moscow, Russia^4

Institute of Numerical Mathematics, Russian Academy of Sciences, Gubkina str., 8, Moscow, Russia^5

关键词: Coupled general circulation models;    Land surface scheme;    Numerical experiments;    Numerical weather prediction;    Space resolutions;    Surface temperatures;    Terrestrial models;    Two-way interaction;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/48/1/012005/pdf
DOI  :  10.1088/1755-1315/48/1/012005

来源: IOP

【 摘 要 】

Land surface schemes (LSS or terrestrial models) are a crucial component of both Numerical Weather Prediction (NWP) systems and climate models. An important land- surface type is lakes. This paper presents the mechanism of incorporation of a model LAKE into a coupled general circulation model of the atmosphere and ocean INMCM4, with a space resolution 2° to 1.5° and 21 levels in height, with two-way interaction. A new map for 14 land types distribution was created using a digital map of inland waters for the entire globe. The digital map of water bodies includes the fraction of lake area on the land surface, and the average depth of water bodies, both on the grid of the climate model. This digital map is based on a dataset consisting of 14 000 freshwater lakes. In order to increase the time step in the LAKE model, the k- parameterization has been replaced by the parameterization of Henderson-Sellers. With the amended INMCM4 model, numerical experiments were carried out to simulate global climate during the second half of the XX century. The effects of the new lake parameterization on the surface temperature and heat fluxes are analyzed.