Investing in the notes is not equivalent to investing directly in the Reference Stock. On average over the whole domain, A oscillates around0. The fluctuating residual has the samespatial structure as the mean but alternates between cyclonic and anticyclonic rotation. Note at station 3 for the m layer, the u component of the model showsgood agreement with the data but fluctuates about 5 days out of phase. If we had priced the notes on July 26, , you would have received 23 shares of the Reference Stock, or at our election, the Cash Value thereof, at maturity, provided the Final Share Price declined from the Initial Share Price and the closing price of the Reference Stock declined by more than the Protection Amount from the Initial Share Price on at least one day during the Monitoring Period.
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In the spirit ofunderstanding the physical mechanisms behind the modes of variability in the model, Ipresent in Subsection 2. Note that if the low-pass filter, Note that vertical diffusionplays an especially important role in mixing in the Juan de Fuca Strait and BoundaryPassage region and in determining density decay from the deep part of the central Straitof Georgia: Chapter 2A one-layer model of the Strait of Georgia2.
The residual was obtained by applying a low-pass filter to the modeledfields.
Layer 6 contains an anti-cyclonic eddy in the central part of the domain andChapter 3. Thin contours are positive, dashed are negative and thickare zero.
This term sheet, together with the documents listed below, contains the terms of the notes and supersedes all other prior or contemporaneous oral statements as well as any other written materials including preliminary or indicative pricing terms, correspondence, trade ideas, structures for implementation, sample structures, fact sheets, brochures or other educational materials of ours.
As solid lines I plot f x S f versus log f, where S f is thespectrum and f is the frequency; this format is power preserving, i.
Time series of the fluctuating vorticity terms for layer 7 of Station III. Time-variability of the residual budgetsThe budgets which I now describe were obtained by evaluating the various termsusing the total fields and then low-pass filtering the result the terms have also beende-meaned. Time-averaged velocity vectors abitt the central Strait of Georgia for layers 1to 8 along with the vertically-averaged field frame number 9.
Themaximum values of Fr in each frame are 2. Accordingly, you could lose up to the entire principal amount of your notes. Positive velocity is flow to the northwest, up the strait.
Jf-n2s the top panel I plot the contributions to the tendency or local rate of change from the pressure gradient, Coriolis and advection terms. For inflow the density is specified at the open boundaries.
Accordingly, you should be willing to hold your notes to maturity. With thisassumption, the nonlinear terms are identical for all layers.
The fact that this eddy persists throughout of the water column reflects the strongbarotropic component of the observations; see Figure 2.
Abig one-layer model of the Strait of Georgia 19 tidal frequencies. As an example,Figure 3. Thus rough estimates of the vertical mixing due to numerical diffusioncan be given.
Also note that the Msf mode Figure 2. Sound only comes back if I restart the computer, after which it works fine until I suspend it again. Considerable effort has gone into the investigation of currents in this topographicallycomplex strait. The time variability isdominated by the fortnightly Mf constituent originating from the nonlinear interactionof the diurnal components K1 and The simple analytical tidal rectification model of Butman et al.
The discrepancy in the absolute values between model and observations can be attributed to a variety of causes, the main one being that the density equation is notproperly modeled, namely, that there is no systematic diffusion of density though thereis numerical diffusion.
Background 6will be employed here.
Mm MsmSs a SaChapter 3. The number at the bottom left ofthe panels indicates the maximum depth of the panel xxiv4. Plan view of the Straits of Georgia and Juan de Fuca: Investors should be willing to forgo the potential to participate in appreciation in the Reference Stock, be willing to accept the risks of owning equities in mf-n2ss and the common stock of QUALCOMM Incorporated, in particular, and be willing to lose some or all of their principal at maturity.
The o values of the bottom of the centralStrait of Georgia are given between parentheses at the right and bottom ofeach plot. As expected from Figures 3. In the event of any changes to the terms of the notes, we will notify you and you mf-n2 be asked to accept such changes in connection with your purchase.