By Hance D. Smith
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Additional info for Advances in the Science and Technology of Ocean Management (Ocean Management and Policy)
Roy. Astr. Soc. 74: 331–76. L. (1975) ‘Model decomposition of the velocity field near the Oregon coast’, J. Phys. Oceanogr. 5: 683–704. G. (1987) ‘Tidal flow forum—introduction’, Adv. Water Resources 10: 114. NERC (1987) ‘North Sea Project’, NERC News 3: 10–12, 4: 10–11. , and Moskowitz, L. Kitaigorodskii’, J. Geophys. Res. 69: 5181–90. M. (1980) ‘Applications of the joint probability method for extreme sea level computations’, Proc. Inst. Civ. Eng. 69: 959–75. R. Jamart (eds) Three-dimensional models of marine and estuarine dynamics, Amsterdam: Elsevier, pp.
By the mid-1960s these instruments were becoming obsolescent, having been replaced by the expendable bathythermograph (XBT). At first these obtained readings of temperature to 460 m but later versions were developed which dropped to 760 m and then 1830 m. Variations of these probes are designed for launching from aircraft. Expendable bathythermograph probes send a signal from their temperature sensor up a thin piece of copper wire to a shipborne recorder. Drop rate equations are used to calculate depth.
Kitaigorodskii’, J. Geophys. Res. 69: 5181–90. M. (1980) ‘Applications of the joint probability method for extreme sea level computations’, Proc. Inst. Civ. Eng. 69: 959–75. R. Jamart (eds) Three-dimensional models of marine and estuarine dynamics, Amsterdam: Elsevier, pp. 89–111. Society for Underwater Technology (1987) Modelling the offshore environment, Advances in Underwater Technology, Ocean Science and Offshore Engineering 12, London: Graham & Trotman. Townsend, J. ) Floods due to high winds and tides, London: Academic Press.
Advances in the Science and Technology of Ocean Management (Ocean Management and Policy) by Hance D. Smith