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Języki publikacji
Abstrakty
The Maximum Cross Correlation method (MCC) modified with divergence checking was used to calculate the surface velocity field in the Gulf of Gdansk. The brightness temperature in channel 4 of the AVHRR taken 10 times between 6 and 9 August 1996 served as input data. The surface velocity vector distribution obtained with the use of MCC are compared with the results of a 3D hydrodynamic model and field observation of a drifting rhodamine spill during the POLRODEX?96 experiment.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
35--44
Opis fizyczny
Bibliogr. 7 poz., tab., wykr.
Bibliografia
- [1.] Emery W. J., Thomas A. C., Collins M. J., Crawford W. R., Mackas D. L., 1986, An objective method for computing advective surface velocities from sequential infrared satellite images, J. Geoph. Res., 91 (Cl 1), 12865-12878.
- [2.] Gajewski L., Gajewski J., 1997, Modelling of drift and spreading in wiew of rhodamine B tracing, Bull. Mar. Inst. Gdańsk, 24, 1, 59-67.
- [3.] Garcia C. A. E., Robinson I. S., 1989, Sea surface velocities in shallow seas extracted from the sequential coastal zone color scanner satelite data, J. Geoph. Res., 94, 12681-12691.
- [4.] Jędrasik J., Kowalewski M., 1992, Transport model of pollutants in Gdańsk Bay, Stud. Mat. Oceanol., 64 (3), 61-75.
- [5.] Kelly, K. A., Strub P. T., 1992, Comparison of velocity estimates from advanced very high resolution radiomeler in the coastal transition zone, J. Geoph. Res., 97 (C6), 9653-9668.
- [6.] Kowalewski M., 1997, A three-dimensional hydrodynamic model of the Gulf of Gdańsk, Ocean. Stud., 26 (4), 77-98.
- [7.] Wald L., 1983, Predictability of the oceanie current field from routine satellite surveys of the sea surface temperature, CTAMN/83/R/05 - March, 1983, ESA, 76 pp.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0025-0011