Paleoenvironment studies can be done with pollen, diatom, tree ring, stalactite and sediment analyzes as well as with climate models. On a global scale, climate model data created by physical laws enable possible environments in the past to be expressed with climatic variables. There are many research centers in the world that produce this type of climate data, and these data generally offer low resolution. But the resolution of these data can be increased by various methods. In this study, the compatibility of 7 climate models produced for the Last Glacial Maximum (LGM) according to the glacial regions determined in Turkey was investigated by using datasets with increased resolution. For this purpose, the biomes of Holdridge ecological zones (HEZ) depend on the 7 different models, which has approximately 1 km resolution, monthly total precipitation, and monthly average temperature data, were created and glacial areas (cold desert + glacier) for the LGM were determined. The LGM paleo glacial areas of Turkey were vectorized, and the compatibility between these areas and the glacial areas in the HEZ biomes was evaluated. As a result, while MICRO-ESM and CNRM-CM5 models are not suitable for Turkey and MRICGCM3 model only represents Eastern Black Sea Mountains well, CCSM4 model gives accurate results for Eastern Black Sea, Southwestern Anatolia, Central Anatolia, and some parts of Eastern Anatolia. It has been determined that the FGOALS-G2 model represent good result for the Central Anatolia, Taurus Mountains and Eastern Black Sea Mountains, while the IPSL-CM5A-LR model is compatible for Turkey only in the Bitlis-Hakkari mountainous area and the Munzur Mountains. MPI- ESM-P, on the other hand, has been found to give accurate results in parts of Central Anatolia, Central Black Sea and Eastern Anatolia.