Temperature data at different layers of the past 45 years were studied and we found adiploe mode in the thermocline layer (DMT): anomalously cold sea temperatur
Direct measurements of current velocity and water temperature were undertaken at the mooring Sta. M (125°29.38′ N,31°49.70′ E) on the continental sh
Some problems concerning the ice forces and ice response spectra are studied from both theoretical and practical points of view. On the basis of structural anal