Microcirculation and Heat Uniqueness of Tbilisi

Abstract

Atmospheric processes are highly heterogeneous and anisotropic in space and time. This study examines the climate adaptation strategies. These processes are irregular everywhere, especially in such difficult physical terrain as the TransCaucasus and Georgia in particular. One of such areas is the well-known Tbilisi hollow, which is characterized by a long-standing thermal inversion layer that keeps warm air close to the relief and strengthens heat waves. Extreme heat is a hazard that is capable of causing economic problems and potentially high mortality rates. In order to investigate heat waves, NEA 1991-2020 hydrometeorological observation and ERA5 reanalysis data are used. The results are important for the early warning system and stakeholders.