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Journal ArticleDOI

Aerial Observations of the Yugoslavian Bora

Ronald B. Smith
- 15 Jan 1987 - 
- Vol. 44, Iss: 2, pp 269-297
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TLDR
The first aircraft observations of the bora in Yugoslavia were accomplished during the ALPEX project in 1982 as discussed by the authors, and data from all five ALPEX bora flights have been analyzed in a comparative study of bora structure.
Abstract
The first aircraft observations of the bora in Yugoslavia were accomplished during the ALPEX project in 1982. Data from all five ALPEX bora flights have been analyzed in a comparative study of bora structure. Although the bora varies considerably in depth, in the strength of the incoming low level flow, and in the direction of the winds aloft, several common features are evident. These include: upstream descent and acceleration beginning where the mountains rise; an approximate coincidence between the depth of the uppermost descending streamline and the wind reversal level upstream (when a reversal exists); a decoupling of the flow aloft associated with a splitting of the inversion and the formation of a thick mixed layer downstream; a narrow region of intense turbulence and an ascending jet just downstream of the plunging bora. The bora structure is similar in many respects to the Boulder windstorm. Internal hydraulic theory, taking into account the decoupling effect of the intermediate layer, a...

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Citations
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Book ChapterDOI

Hydrostatic airflow over mountains

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The Dynamics of Mountain-Wave-Induced Rotors

TL;DR: In this article, the development of rotor flow associated with mountain lee waves is investigated through a series of high-resolution simulations with the nonhydrostatic Coupled Ocean-Atmospheric Mesoscale Prediction System (COAMPS) model using free-slip and no-slink lower boundary conditions.
Journal ArticleDOI

Response of the Adriatic Sea to the bora and sirocco forcing

TL;DR: In this paper, the response of the Adriatic shelf waters to dominant winter winds is analyzed: the bora, which is a cold, katabatic wind blowing from the northeast; and the sirocco, which blows from the southeast and brings warm Mediterranean air.
Journal ArticleDOI

A review of recent advances in understanding the meso‐ and microscale properties of the severe Bora wind

TL;DR: In this paper, the role of the boundary layer and waves on the upwind side of the bora evolution and the consequent lee side flow structures are inadequately understood; this is especially so for bora at the southern Adriatic coast.
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