Original scientific paper
Air temperature anomaly in Croatia
Anita Filipčić
orcid.org/0000-0003-1346-9898
Abstract
In January due to the advection of cold air from the North and Northeast the smallest anomaly (<1 C) is evident in the Pannonian Basin and in the largest part of the Peripannonian belt. The greatest 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.
Keywords
air temperature anomaly; Croatia
Hrčak ID:
84468
URI
Publication date:
1.12.1994.
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