Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
Temporal and spatial variability of mesoscale structures in the North-East Gdańsk Bay is discussed. During measurements in September 1997, variability in the upper layer was determined by convective cooling processes. Measurements made in January 1998 show that between the two periods renewal of a whole halocline water took place in the Gdańsk Bay.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
47--55
Opis fizyczny
rys.
Twórcy
autor
- P.P. Shirshov Institute of Oceanology, Atlantic Branch, Kaliningrad, Russian Federation
autor
- P.P. Shirshov Institute of Oceanology, Atlantic Branch, Kaliningrad, Russian Federation
Bibliografia
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-90c1623c-4aab-4544-9f06-4e0edae6d878