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Calculating the semidiurnal ... D228YD302
consequence of the sea's constriction and the interference of
waves reflected from tile coast. It was found tc be impossible to
calculate the tidal currents of the M wave by Polukarovl-- method
in this area. Z-'Abstractor's note: Co~plete translation....,/
Card 2/2
VLADDIIROV, O.A.
Calculatinj the area increase of the sea caused by waves. Okeano-
logiia 1 no.4:630-637 161. (MIRA 14:11)
(Hydrography) (waves)
Links
[1] https://www.cia.gov/readingroom/document-type/crest
[2] https://www.cia.gov/readingroom/collection/scientific-abstracts
[3] https://www.cia.gov/readingroom/docs/CIA-RDP86-00513R001860210018-4.pdf