Köppen–Geiger Climate Clasification in the Pannonian basin According to SSP5-8.5 Scenario

Abstract The Köppen–Geiger climate classification is used to determine climate types in region of Pannonian Basin with data from the sixth phase of the Coupled Model Intercomparison Project. The study covers a period from years 2021 until 2100, and it shows how certain climate types are changing in percentage in thirty-year averages for six periods. In the period 1960-1990 years of the last century, the dominant climate type was warm summer humid continental climate (Dfb) with 98% presences in the region. The results show that the change of this climate type to the humid subtropical climate type (Cfa) began in the first half of the 21st century. The complete dominance of humid subtropical climate type in the most areas of the Pannonian Basin characterized the second half of the 21st century. Also, results show creation of a warm summer Mediterranean climate type (Csa), which according to certain simulations, is present from 10% to 30% on average in the region. In the central part of the region, a cold desert climate type (Bsk) was formed with approximately 6% presences in the region. This creation of climate types in some parts of the region shows that in the second half of 21st century drier and a warmer climate is expected compared to the last century.