A major task for physical oceanographers is to determine the movement of oceanic water from observations. This book introduces the P-vector inverse method, with a two-step determination of the velocity from hydrographic data. The book provide insights into the basics of the P-vector inverse method and the features of the inverted global and regional ocean circulations. Upper undergraduate and graduate students as well as oceanographers, marine biologists and other environmental scientists will find this book a valuable tool for their studies.The mean salinity profile (Fig.11.71b) shows the existence of salinity maxima ( 34.63ppt) located at the 125a175m depths and of salinity ... The spatial and temporal decorrelation scales associated to the mean field were estimated from the covariance matrix obtained from the ... (a) TaS diagram constructed from the AXCTD data, and (b) ET a ES diagram constructed from the interpolated data (from Chu andanbsp;...
|Title||:||P-Vector Inverse Method|
|Author||:||Peter C. Chu|
|Publisher||:||Springer Science & Business Media - 2007-02-15|