Renaud

I can believe that some, even most, tropospheric aerosols are associated with heart, lung and respiratory diseases. But the sub-micron salt we would use for marine cloud brightening is beneficial especially for lung problems. Asthmatic children in Poland get breathing exercises down salt mines. Perhaps it is unfortunate that so little of it will reach land from mid-ocean spray regions.

Stephen


Emeritus Professor of Engineering Design. School of Engineering. University of Edinburgh. Mayfield Road. Edinburgh EH9 3JL. Scotland [email protected] Tel +44 (0)131 650 5704 Cell 07795 203 195 WWW.see.ed.ac.uk/~shs YouTube Jamie Taylor Power for Change
On 02/08/2014 00:52, Michael Hayes wrote:
Renaud et.al.,

I'm 100% behind any effort to stop */any /*particulates from being released. However, the current levels of BC/S seems to be keeping the atmospheric moisture levels (i.e. global tempurature) artificially low (up to 10% per S. Solomon <http://eaps-www.mit.edu/people/solos>) through the BC/S wetting process. At this time, I can not find the study in which she described this phenomena, yet I'm sure I can eventually find it if you need.

Has the proposed particulate cleaning/trans-boundary injection method considered the overall climate temperature implications of reducing the BC/S wetting (i.e. moisture reduction/global temperature) factor?

Best regards,

Michael

On Friday, August 1, 2014 5:53:56 AM UTC-7, Renaud de_Richter wrote:

    Currently, anthropogenic tropospheric aerosols present both Dr
    Jekyll and Mr Hyde faces.

    On the one hand, tropospheric aerosols play an important role on
    climate, with a net cooling radiative forcing effect.

    On the other hand, tropospheric aerosols affect terrestrial
    ecosystems and human health and are associated with increased
    heart, lung and respiratory diseases, which lead to disablement
    and numerous premature human deaths (Shindell et al, 2012).

    Consequently, reducing anthropogenic tropospheric aerosols
    emissions, on the one hand will lead to a positive forcing
    (warming) at local and regional scale, and on the other hand will
    save numerous lives and significantly reduce health costs.

    *What is proposed is to investigate means whereby the cooling
    effect of current emissions is kept unchanged and their
    deleterious effects are reduced,*using onlymodifications of
    existing industrial aerosols emitters. Key advantages of such
    investigations are that they avoid most of the roadblocks
    associated with SRM.
    So, what is proposed is a Win-Win research program that will at
    the same time allow indirect geoengineering research, and reduce
    tropospheric pollution.

    /(Important remark: it is not proposed to perform CCS, or CDR).///

    This is so, because the current anthropogenic tropospheric
    sulphate aerosol emissions are estimated to be _almost two orders
    of magnitude larger_ than requested by Stratospheric Particle
    Injection geoengineering schemes to offset the effects of a
    2 X CO_2 (carbon dioxide concentration doubling in the atmosphere).

    Thus the strategy to reduce current sulphate _tropos_pheric
    emissions and at the same time to keep their current cooling
    effects will be like performing indirect climate engineering
    without the need to artificially inject sulphates in the
    _strato_sphere.

    Now, the radiative forcing due to sulphate aerosols is estimated
    to be ???0.4 W/m^2 with a range of ???0.2 to ???0.8 W/m^2 .
    On a global average basis, the sum of direct and indirect
    radiative forcing at the top of atmosphere by anthropogenic
    aerosols is estimated to be ???1.2 W/m^2 [???2.4 to ???0.6 W/m^2 ]
    (*cooling*) over the period of 1750 - 2000. This is significant
    when compared to the positive (*warming*) forcing of +2.63 [??0.26]
    W/m^2 by anthropogenic long-lived greenhouse gases over the same
    period [Forster et al., 2007].
    In heavily polluted regions, aerosol cooling overwhelms greenhouse
    warming [Ramanathan et al., 2001; Li et al., 2010].

    The tropospheric aerosol lifetimes are approximately 1 to 2 weeks,
    which is quite shorter. Therefore, these current human made
    aerosols have an uneven distribution, both horizontally and
    vertically, and are more concentrated near their source regions
    over continents and in the boundary layer.

    *Emission reductions of aerosols in the troposphere will lead to a
    positive forcing (warming), unless the sulphates lifetimes are
    increased and their horizontal and vertical distribution are
    improved. **Whilst the particulates are removed, some part of the
    sulphates can be lofted higher to where they can act as a
    solar-reflective shield to cool larger regions.***

    To do so, what is proposed is to model the effects of a
    theoretical fivefold aerosols emission reduction (80% removal of
    sulphates, NOx, and > 95% removal of soot, black carbon, ash???) by
    adding filters or electrostatic precipitators to the flue stack of
    a majority of fossil fuel fired power plants, for adequate
    particulate filtering and scrubbing, and *at the same time
    increasing the height release of sulphates for a reduced number of
    other power plant stacks in order to allow these (20% SOx)
    emissions to over pass the boundary layer and stay longer in the
    atmosphere*.

    This can be__performed by the use of taller chimneys allowing the
    flue gases to pass the boundary layer, so that the impact of a
    regional emission reduction is not confined to the region itself,
    by allows intercontinental transport (long-range transport) of
    these sulphates _produced by existing anthropogenic aerosols_.
    Several other possibilities exist to increase the height release
    and dilution of gas emissions from flue stacks.

    **

    This strategy was proposed in page 818-819 of an _open access
    article_
    http://www.sciencedirect.com/science/article/pii/S1364032113008460
    <http://www.sciencedirect.com/science/article/pii/S1364032113008460>
    Fighting global warming by climate engineering.

    //

    /Two figures are attached to summarize this research proposal/

    /
    /

    Public perception of SRM climate engineering is often presented as
    Ulysses choices between the perils of Scylla and Charybdis,
    despite the very good cooling potential to mitigate global
    warming, and the high effectiveness and accessibility of
    geoengineering schemes consisting of the stratospheric injection
    of sulphate aerosols.

    The Win-Win strategy proposed here may change this perception at
    the same time as helping to advance CE research...


    Renaud de_Richter, PhD

    http://www.solar-tower.org.uk/

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