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Bora on the northern Adriatic coast during the ALPEX SOP, 20–25 March 1982 (CROSBI ID 184437)

Prilog u časopisu | izvorni znanstveni rad

Ivančan-Picek, Branka ; Vučetić, Višnja Bora on the northern Adriatic coast during the ALPEX SOP, 20–25 March 1982 // Hrvatski meteorološki časopis, 25 (1990), 1-12

Podaci o odgovornosti

Ivančan-Picek, Branka ; Vučetić, Višnja

engleski

Bora on the northern Adriatic coast during the ALPEX SOP, 20–25 March 1982

Results from investigation of the bora during the period of 20-25 March 1982 are characterized by a large variability od bora strength, direction and duration. The two distinct wind speed maxima indicate two different origins of bora genesis. The first bora (21 March) was caused by a cold air stream, followed by the Genova cyclogenesis process. The second bora situation (23-25 March) is connected with the central Eyrope anticyclone and the cold NE flow - upstream of the Dinaric Alps. Assuming that the bora has a certain similarity with the supercritical flows described by hydraulic theory, the parameters of the real flow could be successfully predicted on the entire northern Adriatic in the case with the strongest bora.

bora layer ; hydraulic theory ; ALPEX SOP ; temperature inversion ;

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Podaci o izdanju

25

1990.

1-12

objavljeno

1330-0083

1849-0700

Povezanost rada

Geofizika

Poveznice