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Original scientific paper

Air temperature anomaly in Croatia

Anita Filipčić orcid id orcid.org/0000-0003-1346-9898


Full text: croatian pdf 8.837 Kb

page 45-55

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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

https://hrcak.srce.hr/84468

Publication date:

1.12.1994.

Article data in other languages: croatian

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