OBSERVATIONS ON INTERNAL WAVES IN SHALLOW WATER

摘要: Observations made off the San Diego coast in 1959 are presented and discussed. Two different systems for recording temperatures were employed thermistors used both of them. The transducer component one consists several by which temperature is measured at fixed depths. other system includes a sea element automatically continuously positioned on selected isotherm. Ocean was simultaneously recorded three locations. Series internal waves relatively high frequency usually follow or low tide persist approximately hour. Single that separated from significant thermal disturbances not related to any particular phase progress same area. Profiles types show they strongly influenced boundary conditions. Wave displacement upward when thermocline near bottom downward higher. Internal tides present throughout 7-day record isotherm depth. relation between surface variable over time but period asymmetry two similar.