T jpo, 2011, in press he origin of along-shelf pressure gradient in the Middle Atlantic Bight
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Table 2. Correlation coefficients (R) and time lags (shown as R/Lag in months; dashes mean insignificant correlation at the 95% significance level) for 3-month running averages minus 1-year averages for GS path-shifts, wind stress curl, eddy kinetic energy north of the Gulf Stream (N-EKE), CLSW transport computed off the southern coast of Nova Scotia (see text), and total river discharge. See also Figure 7. The last row indicates the correlation coefficients R for 1-year low pass of N-EKE with ASPG, wind stress curl, and GS path shifts. A positive (negative) lag indicates that the variable listed in the first column leads (lags) that listed in the first row. The 95% significance levels are shown in parentheses below each entry, and are computed as 1-(1-0.95)2/(F-1), where F is the degree of freedom calculated as N/N, N is length of time series and N is the dot product of the autocovariances of the two time series.
Figure 1. Map of the western Mid-Atlantic Ocean and locations of the 14 tide-gauge stations.  Directory: ftp -> lyo -> chiming ftp -> Tr-41. 4-03-05-024 Telecommunications ftp -> Message Race Detection for Web Services by an smt-based Analysis ftp -> A proposal submitted to the ftp -> National reports on data buoy activities ftp -> Louisiana barrier island comprehensive monitoring program (bicm) Volume 1: Barrier Shoreline Post-Storm Assessment ftp -> Jcomm expert team on chiming -> Boemre 2008 Extended Hindcast Calculation of Gulf of Mexico Circulation: Model Development, Comparisons with Observations Download 1.87 Mb. Share with your friends:
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