Информация о цитировании статьи получена из
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 3 июля 2019 г.
Аннотация:The hydrothermodynamics of the flow over a mountain range under the Novorossiysk bora is investigated. A nonlinear, stationary, two-dimensional, analytical model is used. Vertical unlimitedness of the atmosphere is taken into account by representing it in the form of three layers with different hydrostatic stability. The properties of the unperturbed incindent flotation are taken into account throughout the real range of its changes. The characteristics of the air flow at the leeward slope of the streamlined relief are studied. A hypothesis is made that the intensity of bora can be estimated from the speed at the leeward slope of the mountains.