Like any successful emergent technology, DAC will probably scale through
high-cost edge-case uses. Initially, nobody tried to make mobile phones
affordable for African cattle farmers, they tried to make them affordable
for rich Western businessmen.

You don't need high volumes initially, to start seeing major costs
reductions. The learning curve is usually dependent on volume doubling - so
rapid proportional growth from a low base is sufficient.

It's often forgotten that DAC costs are hugely dependent on energy costs.
These will fall rapidly, as both solar and batteries have their own
experience curve effects.

Andrew

PS if anyone has decent cost estimates for mid century solar, let me know.
Module costs are falling reliably, but it's hard to project the impact on
industrial or domestic electricity costs, as solar modules are only one
part of the costs structure.

On Mon, 6 Aug 2018, 02:31 Michael MacCracken, <mmacc...@comcast.net> wrote:

> In that we are already in an overshoot situation given the objective of
> the UNFCCC and we want to be in overshoot the least amount of time possible
> given the acceleration of loss of ice sheet mass and increase in extreme
> weather and precipitation, I would hope all would also agree that it is
> essential to be working toward early, gradual deployment of climate
> intervention approaches  to push warming back down toward less than 0.5 C
> as soon as possible, with DAC, in addition to aggressive mitigation, being
> a vital component of an envisioned exit strategy to be scaled up as quickly
> as practicable.
>
> "The fact is that all that is needed is the decision to do it....I [too]
> would hope all the very talented and positively motivated geoengineering
> community will throw their support behind a strong global effort .."
>
> Peter E--In my view, there is also the need to avoid very serious impacts
> that are building now, so very early forcing down of the temperature as
> well as dealing with the higher CO2 concentration over the time it will
> take to build up and do this in the manner that you focus on.
>
> Mike
>
>
>
> On 8/5/18 4:30 PM, Peter Eisenberger wrote:
>
> I can tell you that there is a major change going on with reapect to
> negative emissions and DAC in particular,. After years of neglect all the
> major players
> are showing alot of interest in negative emissions and DAC in particular.
> This spans the large petro chemical companies , the goovernments and
> international efforts - I do not have the time to document this for you so
> you can ignore the input but neverthe less it is happening and the change
> is dramatic. I think as the world takes NETs more seriously a quesion will
> emerge for the SRM supporters. Again for the record I support research on
> SRM but
> oppose using the possible failure of NETS as the basis for the effort. The
> fact is that all that is needed is the decsion to do it,  do NET with DAC
> playing a big role. I am optimisitic that the academy study that is coming
> out will
> provide an additional strong impetus for getting together and doing NET. I
> hope all the very talented and positively motivated geoengineering
> community will throw their support behind
> a strong global effort for NET and adopt the factually correct perspective
> that if we develop a global consencus and work together we can get this
> done, eg limit the time we spend in the overshoot CO2 condition.
>
> On Fri, Jul 27, 2018 at 2:08 AM, Andrew Lockley <andrew.lock...@gmail.com>
> wrote:
>
>> Stopping the Flood: Could We Use Targeted Geoengineering to
>> Mitigate Sea Level Rise?
>> Michael J. Wolovick1
>> and John C. Moore2,3
>> 1Atmosphere and Ocean Sciences Program, Department of Geosciences,
>> Princeton University, GFDL, 201 Forrestal Road,
>> Princeton, NJ 08540, USA
>> 2College of Global Change and Earth System Science, Beijing Normal
>> University, Beijing, China
>> 3Arctic Centre, University of Lapland, Finland
>> Correspondence: M.J. Wolovick (wolov...@princeton.edu)
>> Abstract. The Marine Ice Sheet Instability (MISI) is a dynamic feedback
>> that can cause an ice sheet to enter a runaway collapse.
>> Thwaites Glacier, West Antarctica, is the largest individual source of
>> future sea level rise and may have already entered the
>> MISI. Here, we use a suite of coupled iceā€“ocean flowband simulations to
>> explore whether targeted geoengineering using an
>> artificial sill or artificial ice rises could counter a collapse.
>> Successful interventions occur when the floating ice shelf regrounds
>> 5 on the pinning points, increasing buttressing and reducing ice flux
>> across the grounding line. Regrounding is more likely with a
>> continuous sill that is able to block warm water transport to the
>> grounding line. The smallest design we consider is comparable
>> in scale to existing civil engineering projects but has only a 30%
>> success rate, while larger designs are more effective. There
>> are multiple possible routes forward to improve upon the designs that we
>> considered, and with decades or more to research
>> designs it is plausible that the scientific community could come up with
>> a plan that was both effective and achievable. While
>> 10 reducing emissions remains the short-term priority for minimizing the
>> effects of climate change, in the long run humanity may
>> need to develop contingency plans to deal with an ice sheet collapse.
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