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Salt flux and stability in Susiun Cut 1995: (a) Ri x (solid line) computed from observed tidal currents and dS/ dx-the critical value of Ri x = 0.6 is also shown (dashed line) (b) strength of gravitational circulation PC 2 (cm s −1) (c) near-bottom salt flux (+ upstream), decomposed as total salt flux (solid line), salt flux due to tidal averages 〈 U〉〈 S〉 (dot–dash line), and salt flux due to tidally fluctuating salinities and velocity 〈 U′ S′〉 (dashed line), where U′ and S′ are the instantaneous deviations from the low-pass filtered values 〈 U〉 and 〈 S〉 Other data are taken from Fischer (1972) and represent the Vellar (□), the Gironde (▵), and the Mersey (∇) estuaries Data taken from USGS CTD transects are the average along transect of top − bottom salinity difference for USGS from (+) 1988–93, (○) 1996–97, and (⋄) 1998–99. The (+) represent computed salinities for flows between 100 and 10 000 m 3 s −1, the (○) represent USGS observations, and the solid line is the spline fit to the USGS dataĮffect of Ri E on estuarine stratification. Steady-state X 2– Q relations computed numerically using different values of K B and keeping γ constant compared with observed valuesĬomputed salinity distributions as functions of distance from the Golden Gate normalized by X 2( Q) for K B = 30 m 2 s −1 and with γ varying between 0.081 and 0.054 depending on flow. Geometry of northern San Francisco Bay (taken from Peterson et al. Plot of K x(m 2 s −1) as a function of position in the estuary for five different flow rates (m 3 s −1) USBR salinity data from four stations 1967–91 compared with unscaled salinity as a function of ( x/ X 2) found in 1988–93 USGS CTD transects The solid line is the dimensionless function derived from the spline fit to the 1988–93 data with the salinity at x = 0 scaled by the corresponding salinity at the Golden Gate Dates corresponding to symbols are shown on plot.
Salinity distributions from water year 1995. (10)ĭepth-averaged salinity as a function of x/ X 2 X 2 was determined directly from bottom salinity measurements data taken from USGS CTD transects 1988–92Īn example of non-self-similar salinity distributions from Feb–Apr 1986 (data from USGS/USBR). The line shown is the steady-state best-fit Q– X 2 relation given by Eq.
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The data series starts on įunctional relationship between river flow, Q, and X 2. The four salinity stations shown are located at x = 19.4, 40.5, 50.5, and 72.5 kmĭaily time series of river flow and salinity intrusion length scale X 2.
The numbers mark different distances (km) from x = 0 at the Golden Gateįlow and salinity variability in 1993 in northern San Francisco Bay.
Download powerpoint for mac usfca how to#
See all of the benefits and find out how to get support with Office 365 when you need it.Northern San Francisco Bay (plotted with software provided by R. Check the UCSF Calendar for upcoming training webinars on Office 365. These resources are available on the Office 365 Training page and FAQ page. In addition to regular Service Desk support, a variety of resources have been developed and customized to make this a smooth transition.
IT has designed a fully documented and robust support model for Office 365.
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