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Formation of reversed lee flow over the north- eastern Adriatic during bora (CROSBI ID 158760)

Prilog u časopisu | kratko priopćenje | međunarodna recenzija

Telišman Prtenjak, Maja ; Belušić, Danijel Formation of reversed lee flow over the north- eastern Adriatic during bora // Geofizika, 26 (2009), 2; 145-155

Podaci o odgovornosti

Telišman Prtenjak, Maja ; Belušić, Danijel

engleski

Formation of reversed lee flow over the north- eastern Adriatic during bora

In-situ measurements indicate the existence of reversed near-surface airflow over the north- eastern Adriatic during the bora wind. Here we examine its structure and evolution by means of a numerical simulation. The studied phenomenon developed during typical summer frontal bora that is associated with a cold air advection from the north-east. It is characterized by a sudden increase in wind speed and a brief duration. Within a sheltered area near the town of Malinska on the island of Krk, onshore flow occurred as the bottom branch of the lee rotor-like circulation that was associated with the hydraulic jump. While the closed circulation somewhat resembles the hypothesized hydraulic-jump rotor, there are significant differences, particularly in the strength of the turbulence associated with the rotor formation.

wake ; hydraulic jump ; lee rotor

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Podaci o izdanju

26 (2)

2009.

145-155

objavljeno

0352-3659

Povezanost rada

Fizika, Geologija

Poveznice
Indeksiranost