METHOD FOR MONITORING GIDROMETEOROLOGOAKUSTICHESKOGO waters of the sea GROUND

摘要

1.method for u0433u0438u0434u0440u043eu043cu0435u0442u0435u043eu0440u043eu043bu043eu0433u043eu0430u043au0443u0441u0442u0438u0447u0435u0441u043au043eu0433u043e u043du0430u0431u043bu044eu0434u0435u043du0438u00a0 zone of the site, including the simultaneous implementation of an area of seabed surveying echolocation survey of surveying and u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 amendments for the bottom of the u0438u0437u043cu0435u0440u0435u043du0438u00a0u0445, placement of instrumentation on the surface, in the aquatic environment and the aquatic torii of the polygon.the quantity of which u0443u0434u043eu0432u043bu0435u0442u0432u043eu0440u00a0u0435u0442 condition u0437u0430u043fu043eu043bu043du0435u043du0438u00a0 all at the waters for the u0440u0430u0441u043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 in researched area by defined u0438u00a0 coordinates u043cu0435u0441u0442u043eu043fu043eu043bu043eu0436u0435u043du0438u00a0 instrumentation, comparing them with predetermined coordinates measurement by measuring equipment of dynamic noise u043cu043eu0440u00a0, seawater temperature and atmosphereatmospheric and hydrodynamic pressure, density and salinity of sea water, the speed of u0442u0435u0447u0435u043du0438u00a0, analysis of spectra recorded signals, the definition of the no m u0441u043eu0441u0442u0430u0432u043bu00a0u044eu0449u0438u0445 energy noise u043cu043eu0440u00a0, average wind speed, wave height of 3%, and with the inclusion of these parameters in the information u043eu0431u0435u0441u043fu0435u0447u0435u043du0438 u00a0 transferred to recipient items through u0441u0432u00a0u0437u0438, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 orderwhat u0443u0441u043bu043eu0432u0438u00a0 u0437u0430u043fu043eu043bu043du0435u043du0438u00a0 researched area of the u0440u0430u0441u043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 in her u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442u0441u00a0 by u0432u043eu0441u0441u0442u0430u043du043eu0432u043bu0435u043du0438u00a0 u043fu0440u043eu0444u0438u043bu00a0 bottom at an elevation u0432u0430u0442u043eu0440u0438u0438 from an area survey and u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 critical points arising from the change of gravityregistration of dynamic noise u043cu043eu0440u00a0 additionally registers the low frequency waves by artificially high frequency waves (with led u0434u0435u0442u0435u043au0442u0438u0440u043eu0432u0430u043du0438u0435u043c u043au043eu043cu0431u0438u043du0430u0446u0438u043eu043du043du044bu0445 signals on u043cu043eu0434u0443u043bu00a0u0446u0438u043eu043du043du044bu043c characteristics of acoustic noise u043cu043eu0440u00a0 and navigation in u0440u0430u0441u0441u0435u00a0u043du0438u0438 flat harmonic waves on aug u0440u0430u043du0438u0447u0435u043du043du043eu043c space wave packetthe length of which is less than the wavelength and u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 speed instrumentation under the influence of u0442u0435u0447u0435u043du0438u00a0, average wind speed u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 u043fu0443u0442u0435 m processing of energy spectrum, selected by clustering and u0441u0438u043du0442u0430u043au0441u0438u0447u0435u0441u043au0438u043c analysis and definition of velocity surface the u0442u0435u0447u0435u043du0438u00a0, speed u0434u0440u0435u0439u0444u043eu0432u043eu0433u043e u0442u0435u0447u0435u043du0438u00a0, speed of the surface of the u0442u0435u0447u0435u043du0438u00a0,the speed of the orbital u0442u0435u0447u0435u043du0438u00a0, wave period, wave length and wave velocity.;2. method for surveying an area 1, including the elevation floor by u0433u0438u0434u0440u043eu043bu043eu043au0430u0446u0438u043eu043du043du043eu0439 filming with mobile u043du043eu0441u0438u0442u0435u043bu00a0 through at least two u044du0445u043eu043bu043eu043au0430u0442u043eu0440 s, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 so that relative u043fu0440u0435u0432u044bu0448u0435u043du0438u00a0 bottom u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 by u0438u0437u043cu0435u0440u0435u043du0438u00a0 longitudinal u043fu0430u0440u0430u043bu043bu0430u043au0441u043eu0432 in arbitrary locations obtained by discrete ism u0435u043du0435u043du0438u00a0 angle direction of rays.;3. method for p.1, containing u0433u0440u0430u0432u0438u043cu0435u0442u0440u0438u0447u0435u0441u043au0443u044e footage, including measurement of force u0442u00a0u0436u0435u0441u0442u0438 through u0433u0440u0430u0432u0438u043cu0435u0442u0440u043eu0432 of amendments in u043fu043eu043au0430u0437u0430u043du0438u00a0u0445 u0433u0440u0430u0432u0438u043cu0435u0442u0440u043eu0432, u043eu0431u0443u0441u043bu043eu0432u043bu0435u043du043du044b the change in force u0442u00a0u0436u0435u0441u0442u0438 fixed point on the surface of the ocean, u043au043eu043bu0435u0431u0430u043du0438u00a0u043cu0438 u0443u0440u043eu0432u043du00a0 sea surface in time, u0432u043bu0438u00a0u043du0438u0435u043c sun and the moon, a grave u0438u043cu0435u0442u0440u0438u0447u0435u0441u043au0438u0445 maps of the sitewith the measurement of u0443u0440u043eu0432u043du00a0 u043cu043eu0440u00a0 through measures with the registration time and the peak of the moon at the top u0438u0437u043cu0435u0440u0435u043du0438u00a0 fixed geographical mary diana, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0, u0438u0437u043cu0435u0440u0435u043du0438u00a0 u0443u0440u043eu0432u043du00a0 u043cu043eu0440u00a0 u0432u044bu043fu043eu043bu043du00a0u044eu0442 at interval time commensurate change the phase of the tide.;4. method for ap.1 and 3, containing a gravity maps of the area, including the chart items with value of gravity anomalies, u0438u043du0442u0435u0440u043fu043eu043bu00a0u0446u0438u044e values of the anomalies, the u0438u0437u043eu0430u043du043eu043cu0430u043b on measured u0437u043du0430u0447u0435u043du0438u00a0u043c anomalies, u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0, chart u0438u0437u043eu0430u043du043eu043cu0430u043b u0432u044bu043fu043eu043bu043du00a0u044eu0442 as fractal lines u0443u0434u043eu0432u043bu0435u0442u0432u043eu0440u00a0u044eu0449u0438u0445 condition l () = 1. ()where l (a) = q1 - d; l is the length of the coast; (1) length between the points u0438u0437u043eu0430u043du043eu043cu0430u043bu044b anomalies; qd 1 - numerical constants, u043eu043fu0440u0435u0434u0435u043bu00a0u0435u043cu044bu0435 degree u0438u0437u0440u0435u0437u0430u043du043du043eu0441u0442u0438 form the coastline and the degree of u0438u0437u0440u0435u0437u0430u043du043du043eu0441u0442u0438 u0444u0440u0430u043au0442u0430u043bu044cu043du043eu0439 line respectively; the scale of the map.