Browsing by Author "Vaithiyanathan, R."
Now showing items 1-7 of 7
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Determination of wave direction using an orbital following buoy
Fernandes, A.A.; Almeida, A.M.; Vaithiyanathan, R.; Vethamony, P. (Publ. and Inf. Dir., New Delhi, India, 1994)Software has been developed in FORTRAN language using a personal computer for the determination of wave direction from time series measurements of heave, pitch and roll of an orbital following buoy. The method of digital ... -
Digital image processing techniques in archaeology
Santanam, K.; Vaithiyanathan, R.; Tripati, S. (Harman Publishing House, 2004)Digital image processing involves the manipulation and interpretation of digital images with the aid of a computer. This form of remote sensing actually began in the 1960's with a limited number of researchers analysing ... -
Directional wave spectra off Candolim, Goa Coast measured through ENDECO directional wave track buoy
Vethamony, P.; Vaithiyanathan, R.; Almeida, A.M.; Fernandes, A.A.; Rao, L.V.G. (1993) -
Geosat altimeter derived sea surface wind speeds and significant wave heights for the north Indian Ocean and their comparison with in situ data
Vethamony, P.; Vaithiyanathan, R.; Almeida, A.M.; Santanam, K.; Rao, L.V.G.; Sarkar, A.; Kumar, R.; Gairola, R.M.; Gohil, B.S. (Publ. and Inf. Dir., New Delhi, India, 1994)Geosat altimeter data for the period November 1986-October 1987 over the north Indian Ocean have been processed to retrieve wind speeds and significant wave heights. Smoothed Brown algorithm is used to retrieve wind speeds ... -
Micro VAX - 2. Primer
Vaithiyanathan, R.; Santanam, K.; Sathe, P.V. (1993) -
Total reflectance of wind-roughened sea surfaces: Directional properties
Sathe, P.V.; Vaithiyanathan, R. (Elsevier, 1994) -
Wind fields of storms from surface isobars for wave hindcasting
Varkey, M.J.; Vaithiyanathan, R.; Santanam, K. (Allied, Chennai (India), 1996)Marine operations of various types are critically linked to mean and extreme wave statistics. In the Indian seas extreme wave conditions are caused by cyclones and steady strong monsoon winds. Wave data from cyclone areas ...