That's only true if you're forcing the oscillator itself, not its effects.
One cannot eject stones from ponds by forcing ripples!

A
On 29 Jan 2014 10:23, "Stephen Salter" <[email protected]> wrote:

>  Michael
>
> If meteorological oscillations behave like most other oscillations you can
> increase or reduce their amplitudes by choosing the phase of your
> intervention.  Quite small impulses can have large effects over long
> periods.
>
> Stephen
>
> Emeritus Professor of Engineering Design School of Engineering University
> of Edinburgh Mayfield Road Edinburgh EH9 3JL Scotland [email protected] +44
> (0)131 650 5704 Cell 07795 203 195 WWW.see.ed.ac.uk/~shs
>
> On 28/01/2014 23:01, Michael Hayes wrote:
>
>
> It is interesting to view the findings of Aquila et. al. with what is
> known about the relationship of the QBO and the ENSO. I did a short search
> and found this: The quasi-biennial oscillation and the El Niño Southern
> Oscillation:<http://www-das.uwyo.edu/%7Egeerts/cwx/notes/chap11/qbo_enso.html>
>
>
> *"The QBO is a regular variation of zonal (i.e. east-west) stratospheric
> winds above the equator (Section 12.3). The ENSO, on the other hand, is
> highly irregular and involves near-surface winds as well as the ocean. Both
> oscillations have a clear effect on the frequency of hurricanes in the
> Atlantic, amongst others. *
>
> *Notwithstanding their obvious differences, there appears to be a weak
> correlation between the QBO and the ENSO. An examination of the QBO signal
> over the Atlantic and Africa shows a correlation with the Southern
> Oscillation Index in the early part of the year (1). Strong La Niña events
> tend to occur when the QBO is in its westerly phase over the equatorial
> Pacific.*
>
> *A record of SOI values for 1876 - 1995 reveals that the ENSO can be
> decomposed in two cycles: a quasi-biennial rhythm and a low frequency (5-10
> year) variation (2). Both signals were notably weak during 1921-41 (when
> ENSO activity was suppressed), and both were strong prior to 1920 and after
> the mid 1960�s. The quasi-biennial ENSO rhythm appears to be a harmonic
> oscillation in equatorial Pacific atmosphere-ocean system, and it was in
> sync with the QBO in 1879-99 and 1963-83. For the quasi-biennial ENSO
> rhythm, sea-level pressures (the SOI) and SST values (El Niño) are notably
> well correlated, in particular in 1879-99 and 1963-83.".* My yellow
> highlight*.*
>  The direct surface cooling of the Subtropical Convergance Zones
> (STCZ) may be needed if SSI is to be deployed. Directly cooling the STCZs
> with MCB and or Large Scale Mariculture (LSM) would obviously effect both
> wind and ocean surface possibly countering SSIs' effect on the QBO/ENSO
> relationship. Having the Aquila study would seem to make modeling MCB and
> or LSM effects on the QBO streightforward.
>
> Best,
>
>
> Michael
>
>
>
> On Monday, January 27, 2014 9:13:03 AM UTC-8, Motoko wrote:
>
>>  *Aquila, V.; Garfinkel, C. I.; Newman, P. A.; Oman, L. D.; Waugh, D. W.
>> (2014): Modifications of the quasi-biennial oscillation by a geoengineering
>> perturbation of the stratospheric aerosol layer. (accepted article). In
>> Geophys. Res. Lett. DOI 10.1002/2013GL058818  .*
>>
>> "This paper examines the impact of geoengineering via stratospheric
>> sulfate aerosol on the quasi-biennial oscillation (QBO) using the NASA
>> Goddard Earth Observing System (GEOS-5) Chemistry Climate Model."
>>
>> Link <http://onlinelibrary.wiley.com/doi/10.1002/2013GL058818/abstract>
>> (http://onlinelibrary.wiley.com/doi/10.1002/2013GL058818/abstract, pay
>> wall)
>>
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