A description of tides near the Chesapeake Bay entrance using in situ data with an adjoint model

Time series of surface elevation and current velocity in the vicinity of the Chesapeake Bay entrance are assimilated into a linear, barotropic model using an iterative adjoint method. Tide surface elevations, NOAA‐NOS tidal data, moored acoustic Doppler current profiler (ADCP), and ocean surface cur...

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Veröffentlicht in:	Journal of Geophysical Research. C. Oceans 2003-03, Vol.108 (C3), p.20.1-n/a
Hauptverfasser:	Hallock, Z. R., Pistek, P., Book, J. W., Miller, J. L., Shay, L. K., Perkins, H. T.
Format:	Artikel
Sprache:	eng
Schlagworte:	Chesapeake Bay data assimilation Earth, ocean, space Exact sciences and technology External geophysics Marine Physics of the oceans Surface waves, tides and sea level. Seiches tides
Online-Zugang:	Volltext
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