Air temperature anomaly in Croatia

U siječnju najmanju anomaliju (7 st. C) imaju vanjski otoci zbog termičkog utjecaja Jadranskog mora i tople advekcije s juga. U ljetnim mjesecima su razlike između unutrašnjosti i obale manje, ali je anomalija veća u obalnom pojasu (osim na krajnjem jugu). Najveću anomaliju imaju kvarnerski otoci (>5 st. C). U godišnjem prosjeku veličina anomalije u unutrašnjosti ovisi o hladnoj advekciji, a najveću anomaliju (>5 st. C) ima uski obalni pojas, osobito Kvarnersko primorje i dio srednje Dalmacije s otocima.In January due to the advection of cold air from the North and Northeast the smallest anomaly (7 C) characterises tie islands far from the coastline. It is the result of the thermic influence of the Adriatic Sea and the warm advection from lower latitude. In the summer months the differences between the coastal belt and the interior are not so great, but the anomaly is greater in the coastal belt (exept of the farthest South). The greatest anomaly (>5 C) is on the Kvarner islands. The annual anomalies in the range from ≤2 C to 35 C. In the interior the anomaly depends on the cold advection. The greatest anomaly (>5 C) is in the narrow coastal belt, especially the Kvarner Littoral and the Kvarner islands, as well as a part of middle Dalmatia