Comparison of RegCM4.7.1 Simulation with the Station Observation Data of Georgia, 1985–2008

Author:

Elizbarashvili Mariam1ORCID,Amiranashvili Avtandil2,Elizbarashvili Elizbar3,Mikuchadze George1,Khuntselia Tamar1,Chikhradze Nino1ORCID

Affiliation:

1. Faculty of Exact and Natural Sciences, Ivane Javakhishvili Tbilisi State University, 0179 Tbilisi, Georgia

2. M. Nodia Institute of Geophysics, Ivane Javakhishvili Tbilisi State University, 0160 Tbilisi, Georgia

3. Climatology and Agroclimatology Department, Institute of Hydrometeorology, Georgian Technical University, 0112 Tbilisi, Georgia

Abstract

The global climate change, driven by natural processes and increasing human activities, is especially significant for Georgia. The region is experiencing increases in temperature, desertification, redistribution of precipitation, and a rise in the frequency and severity of extreme weather events. Georgia’s complex topography and its proximity to the Black and Caspian seas make it essential to employ high-resolution regional climate models to evaluate future climate change risks. In this study, we examine the results of a high-resolution simulation of mean and extreme precipitation and temperature using the Abdus Salam International Centre for Theoretical Physics Regional Climate Model version 4.7.1 for the period 1985–2008, providing an initial evaluation of the model’s performance for the territory of Georgia. The model domain (1524 km; 2388 km) encompasses the entirety of Georgia’s territory and surrounding regions. The simulation, conducted at a 12 km horizontal grid spacing using ERA5 data as boundary conditions, indicates that the least discrepancy between observed and modeled average annual temperatures and precipitation, falling within a −1 to 1 °C and −200 to 200 mm range, respectively, was observed at most stations of eastern Georgia. The largest disparities between the model and observed average annual precipitation totals were noted along the Black Sea coast, in the Kolkheti Lowland, and in some high mountain stations in western Georgia. The most significant differences in average annual temperatures between the model and observations were observed in Ambrolauri, Mt. Sabueti, and Dedoplistskaro. For Georgia territory, such a long run with such a high resolution using ERA5 as boundary conditions was conducted for the first time. Overall, the modeling results are quite satisfactory, providing a solid basis for the successful utilization of the regional climate model RegCM4.7.1 with the selected parameterization for modeling monthly mean and extreme temperatures and precipitation in Georgia.

Funder

Shota Rustaveli National Science Foundation of Georgia

Publisher

MDPI AG

Reference48 articles.

1. Georgian climate change under global warming conditions;Elizbarashvili;Ann. Agrar. Sci.,2017

2. Elizbarashvili, E. (2017). Climate of Georgia, Georgian Technical University, Institute of Hydrometeorology. (In Georgian Language).

3. Elizbarashvili, E. (2007). Climatic Resources of Georgia, Institute of Hydrometeorology. (In Georgian Language).

4. Trends in daily temperature and precipitation extremes over Georgia, 1971–2010;Keggenhoff;Weather Clim. Extrem.,2014

5. Recent changes in Georgia’s temperature means and extremes: Annual and seasonal trends between 1961 and 2010;Keggenhoff;Weather Clim. Extremes,2015

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