Hi Nathan

In these two reports on DMSP and DMS, there is no mention of which
species of phytoplankton produces DMS -

http://www.whoi.edu/oceanus/viewArticle.do?id=45946

http://www.whoi.edu/cicor/page.do?pid=19476&tid=282&cid=40014

The search for the 'right' phytoplankton has to go on ...

regards

Bhaskar

On Apr 22, 10:34 pm, Nathan Currier <natcurr...@gmail.com> wrote:
> Hi, Bhaskar -
>
> You wrote -
>
> "Based on a combined reading of all papers on the subject I understand
> the following -
> Coccolithophores increase Albedo and DMS production and
> Diatoms sequester more carbon by falling to ocean bed."
>
> I used to believe something like that, too.
> But actually the primary arctic DMS producer is a diatom, Nitzschia
> frigida.http://en.wikipedia.org/wiki/Nitzschia
>
> There's a very interesting ppt from Los Alamos on the arctic DMS
> situation:
>
> Biogeochemistry in the Los Alamos National Laboratory (LANL) 
> modelwww.whoi.edu/fileserver.do?id=76944&pt=2&p=83808
>
> After I first saw it I proposed something here about possibly trying
> to use it
> for arctic geoengineering purposes, but no one responded at all at the
> time.....
> Maybe you'll be interested in it now?
>
> All best,
>
> Nathan
>
> On Apr 20, 10:36 pm, M V Bhaskar <bhaskarmv...@gmail.com> wrote:
>
>
>
>
>
>
>
> > Dear Dr Vivien
>
> > You said -
>
> > > Also, how could you ensure the "right" phytoplankton would bloom to 
> > > ensure the albedo effect.
>
> > This is the core issue.
>
> > Based on a combined reading of all papers on the subject I understand
> > the following -
> > Coccolithophores increase Albedo and DMS production and
> > Diatoms sequester more carbon by falling to ocean bed.
>
> > Coccolithophores have a calcium carbonate shell and Diatoms a silica
> > shell.
>
> > Since 2005 we are successfully growing Diatoms in open waters in large
> > lakes, using our silica based micro nutrient.
> > This works on the principle that since Diatoms require silica, they
> > consume it and grow rapidly and dominate the water as long as it is
> > fertilized with this product.
>
> > This product also contains calcium, but only a very small quantity -
> > the amount required for photosynthesis.
>
> > Perhaps if we increase the calcium to the maximum extent possible, we
> > can make Coccolithophores consume it and bloom rapidly and also
> > sustain the bloom for a long period of time, through continuous
> > fertilization.
>
> > Thus we can achieve a more targeted phytoplankton bloom, by developing
> > products / fertilizers that focus on each species / group of
> > phytoplankton.
>
> > best regards
>
> > Bhaskarwww.nualgi.com/new
>
> > On Apr 18, 10:11 pm, Ken Caldeira <kcalde...@carnegie.stanford.edu>
> > wrote:
>
> > > I think Chris Viven has it right.
>
> > > But, if you are still interested in pursuing this, Toby Tyrrell has looked
> > > into this a bit.
>
> > >http://www.noc.soton.ac.uk/soes/staff/tt/eh/optics.html
>
> > > On Wed, Apr 18, 2012 at 6:16 PM, Andrew Lockley 
> > > <andrew.lock...@gmail.com>wrote:
>
> > > > I have been advised to use GNU Octave for image processing.  My guess is
> > > > the the best way to do this would be to draw a rectangle over the bloom 
> > > > and
> > > > compare it to a control rectangle elsewhere in the image. However, a 
> > > > pixel
> > > > by pixel comparison would also be useful, as it would better display the
> > > > range of albedo. Pixel comparisons would be prone to much greater 
> > > > error, as
> > > > I might pick a lucky pixel out.
>
> > > > I have no experience of this kind of thing at all, so any tips or 
> > > > comments
> > > > are welcome.  At this stage I'm just looking to get some back of 
> > > > envelope
> > > > calculations for the list, not get anything you could publish.
>
> > > > One particular concern I have is that the infra red (particularly the 
> > > > near
> > > > infra red) will be very significant. Obviously, this won't show up on a
> > > > photo. Does anyone have any ideas as to how to treat this?
>
> > > > A
> > > > On Apr 18, 2012 1:20 PM, "Chris" <chris.viv...@cefas.co.uk> wrote:
>
> > > >> Andrew,
>
> > > >> If you search Google Images for 'ocean fertilisation' you will find a
> > > >> number of satellite images of blooms from ocean fertilisation
> > > >> experiments. Here are a couple of examples:
>
> > > >>http://disc.sci.gsfc.nasa.gov/oceancolor/additional/science-focus/oce...
> > > >>http://www.csa.com/discoveryguides/oceangard/overview.php
>
> > > >> Also, if you search Google Images for 'Phytoplankton bloom' you will
> > > >> find plenty of images and there is a particularly good one from the
> > > >> western English Channel of a very bright coccolithophore bloom on this
> > > >> page:http://www.noc.soton.ac.uk/soes/staff/tt/eh/satbloompics.html.
>
> > > >> However, don't get too carried away with the possibility of generating
> > > >> phytoplankton blooms for their albedo effect. They would have all the
> > > >> potential side-effects of ocean fertilisation and since phytoplankton
> > > >> blooms are transient events, I find it difficult to see how you could
> > > >> maintain a significant albedo effect over time. Also, how could you
> > > >> ensure the "right" phytoplankton would bloom to ensure the albedo
> > > >> effect.
>
> > > >> Chris.
>
> > > >> On Apr 17, 2:56 pm, Andrew Lockley <andrew.lock...@gmail.com> wrote:
> > > >> > This image appears to show a clear albedo effect from blooms
>
> > > >> >http://en.m.wikipedia.org/wiki/File:Phytoplankton_SoAtlantic_20060215.
> > > >> ..
>
> > > >> > Does anyone have a set of high quality ocean iron fertilization 
> > > >> > images
> > > >> > which can be formally evaluated for albedo? I think this would be a 
> > > >> > very
> > > >> > interesting study.
>
> > > >> > Maybe we have missed a trick on OIF? Maybe It's actually an albedo 
> > > >> > SRM
> > > >> > method cunningly disguised as CDR.
>
> > > >> > Interestingly this would make a powerful negative feedback which 
> > > >> > could
> > > >> > explain the decent into glacials, as aeolian dust fluxes into the
> > > >> southern
> > > >> > ocean changed albedo, causing feedbacks which caused further  cooling
> > > >> and
> > > >> > drying as well as carbon drawdown. This would then lead to more dust
> > > >> flux,
> > > >> > etc.
>
> > > >> > Hopefully someone can check whether the above is right or not.
>
> > > >> > A
> > > >> > On Apr 15, 2012 5:22 PM, "Andrew Lockley" <andrew.lock...@gmail.com>
> > > >> wrote:
>
> > > >> > > Scientific American article identifies AGW sea albedo effect.  This
> > > >> > > potentially suggests ocean fertilization and similar manipulations
> > > >> could
> > > >> > > target albedo, not CO2. Awesome possibilities.  Geoengineers, start
> > > >> your
> > > >> > > computers.
>
> > > >> > > A
>
> > > >> > > *sciam* Ocean-Borne Microbes May Help Speed Warminghttp://
> > > >> t.co/NDQd2jm4
>
> > > >> > > Ocean-Borne Microbes May Help Speed Warming
>
> > > >> > > The proliferation of cyanobacteria in oceans may accelerate warming
>
> > > >> > > By Lucas Laursen | April 15, 2012 |
>
> > > >> > > Trichodesmium
>
> > > >> > > Image: Courtesy of Elizabeth C. Sargent/University of Southampton 
> > > >> > > and
> > > >> > > National Oceanography Center, Southampton
>
> > > >> > > On their own, cyanobacteria are tiny photosynthetic organisms
> > > >> floating in
> > > >> > > the sea. But when they join forces, linking together into chains 
> > > >> > > and
> > > >> then
> > > >> > > mats by the millions, they can become a threat. Before long, the
> > > >> bacteria
> > > >> > > change the color of the sea’s surface and even soften the 
> > > >> > > wind-tossed
> > > >> chop.
> > > >> > > One study of cyanobacteria, also known as blue-green algae, 
> > > >> > > although
> > > >> they
> > > >> > > are not algae, predicted that rising sea temperatures could help 
> > > >> > > the
> > > >> > > already widespread creatures expand their territory by more than 10
> > > >> > > percent. Now researchers are asking whether mats of cyanobacteria
> > > >> might
> > > >> > > themselves affect local sea temperatures, thus creating a powerful
> > > >> feedback
> > > >> > > loop.
>
> > > >> > > Cyanobacteria are ubiquitous. They spew enough oxygen into the
> > > >> atmosphere
> > > >> > > to dictate the current mix of gases we breathe. They also 
> > > >> > > compete—with
> > > >> > > great success—for nutrients such as nitrogen and phosphorus. When
> > > >> > > cyanobacteria bloom, it is often at the cost of neighboring species
> > > >> such as
> > > >> > > fish or other phytoplankton. So if cyanobacteria are shaping the
> > > >> > > temperature of their growing patch of the ocean to favor themselves
> > > >> over
> > > >> > > cold-water critters, researchers want to know how they are doing it
> > > >> and
> > > >> > > what to expect next, says climate scientist Sebastian Sonntag of 
> > > >> > > the
> > > >> > > University of Hamburg in Germany.
>
> > > >> > > Sonntag and his colleagues have adapted a computer model that
> > > >> describes
> > > >> > > the mixing of layers of seawater to take into account two kinds of
> > > >> changes
> > > >> > > produced by the cyanobacterium Trichodesmium: more light absorption
> > > >> and
> > > >> > > less choppy waves. The updated model predicted sea-surface warming 
> > > >> > > of
> > > >> up to
> > > >> > > two degrees Celsius because of light absorption. The wave dampening
> > > >> > > appeared to affect local temperatures by about one degree C.
>
> > > >> > > This may be the first such study of algal blooms in the ocean,says
> > > >> aquatic
> > > >> > > microbiologist Jef Huisman of the University of Amsterdam, who has
> > > >> studied
> > > >> > > light absorption by cyanobacteria in lakes. Both Sonntag and 
> > > >> > > Huisman
> > > >> say
> > > >> > > they would like to ask oceanographers to measure seawater 
> > > >> > > temperature
> > > >> where
> > > >> > > cyanobacteria grow and in nearby empty areas to test the new 
> > > >> > > model’s
> > > >> > > predictions and to improve future versions.
>
> > > >> > > This article was published in print as "Blue Bacteria in Bloom."-
> > > >> Hide quoted text -
>
> > > >> > - Show quoted text -
>
> > > >> --
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>
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