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Objective analysis of geostrophic currents in the Adriatic Sea

Nedžad Limić ; Rudjer Bošković Institute, Zagreb
Mirko Orlić ; Department of Geophysics, Faculty of Science, University of Zagreb, Zagreb, Croatia

Puni tekst: engleski, pdf (838 KB) str. 76-84 preuzimanja: 200* citiraj
APA 6th Edition
Limić, N. i Orlić, M. (1986). Objective analysis of geostrophic currents in the Adriatic Sea. Geofizika, 3 (1), 76-84. Preuzeto s https://hrcak.srce.hr/20904
MLA 8th Edition
Limić, Nedžad i Mirko Orlić. "Objective analysis of geostrophic currents in the Adriatic Sea." Geofizika, vol. 3, br. 1, 1986, str. 76-84. https://hrcak.srce.hr/20904. Citirano 22.10.2020.
Chicago 17th Edition
Limić, Nedžad i Mirko Orlić. "Objective analysis of geostrophic currents in the Adriatic Sea." Geofizika 3, br. 1 (1986): 76-84. https://hrcak.srce.hr/20904
Harvard
Limić, N., i Orlić, M. (1986). 'Objective analysis of geostrophic currents in the Adriatic Sea', Geofizika, 3(1), str. 76-84. Preuzeto s: https://hrcak.srce.hr/20904 (Datum pristupa: 22.10.2020.)
Vancouver
Limić N, Orlić M. Objective analysis of geostrophic currents in the Adriatic Sea. Geofizika [Internet]. 1986 [pristupljeno 22.10.2020.];3(1):76-84. Dostupno na: https://hrcak.srce.hr/20904
IEEE
N. Limić i M. Orlić, "Objective analysis of geostrophic currents in the Adriatic Sea", Geofizika, vol.3, br. 1, str. 76-84, 1986. [Online]. Dostupno na: https://hrcak.srce.hr/20904. [Citirano: 22.10.2020.]

Sažetak
The first results of the objective analysis of geostrophic currents in the Adriatic Sea are presented. Data collected during the “Andrija Mohorovičić” cruise in September and October 1974 are used for computing relative dynamic depths. These are then interpolated on a rectangular grid points, using a first-order polynomial for approximating the mean depths, and applying both the isotropic and anisotropic autocorrelation functions. The objectively analyzed surface currents, computed relative to those at the 50dbar surface, show a similarity with the results of subjective analysis only for the anisotropic autocorrelation function. It is concluded that detailed measurements are needed to assess the statistics of relative dynamic depths. Moreover, the problem of aliasing should be considered, and a method for transforming relative into absolute should be applied to the Adriatic Sea data.

Ključne riječi
Objective analysis; geostrophic current; Adriatic Sea

Hrčak ID: 20904

URI
https://hrcak.srce.hr/20904

[hrvatski]

Posjeta: 544 *