RE: [geo] Meanwhile: 'Irreversible' Melting Threatens 'Considerable Increase' to Sea Level Rise

2014-01-15 Thread Peter Flynn
This is a marvelous concept that is new to me.



Envision a large number of such pipes installed in polar ice sheets. One
might focus on two goals.



The first would be to lower the temperature of the bottom of the ice sheet
in order to promote its growth from the bottom. This has the merit of
avoiding the issue of salt in ice: when ice forms at the bottom of an ice
sheet the ice itself is low in salt and a brine sinks away from the ice.
Would one have to keep sinking the pipe into the ice sheet as the ice
thickens.



But alternatively, one might simply have a long pipe with the goal of just
getting more heat above the ice, to be ultimately radiated away, with a
goal of countering deep ocean temperature rise.



Interesting technical concept.



Peter



Peter Flynn, P. Eng., Ph. D.

Emeritus Professor and Poole Chair in Management for Engineers

Department of Mechanical Engineering

University of Alberta

peter.fl...@ualberta.ca

cell: 928 451 4455









*From:* Ronal W. Larson [mailto:rongretlar...@comcast.net]
*Sent:* January-14-14 6:04 PM
*To:* Keith Henson; John Nissen; Peter Flynn
*Cc:* RAU greg; Geoengineering
*Subject:* Re: [geo] Meanwhile: 'Irreversible' Melting Threatens
'Considerable Increase' to Sea Level Rise



Keith etal  (adding in John Nissen and Peter Flynn )



1.  Most interesting.   I own a solar thermal system with the same heat
pipe theory at work - and would have never carried it over to your Pine
Island example.  This to answer your first question on my part.  Thanks.



2.   Adding John and Peter because of their interest in the northern
equivalent.  I think there we are talking of possibly being able also to
add ice just below the existing surface layer, so as to maybe add months to
the ice area/extent lifetime.  Maybe especially to be located where there
is known methane below.



3.  One beauty is that this is a closed system.  Any cites on the liquids
used for the Alaska pipeline?  Should be able to design something that
floats; totally passive. Has potential multi-year usage even if nothing
possible during part of the summer.  Maybe a gang could be tied together
underwater.



4.  Answering your second and final question,  I would guess that the idea
does qualify as “geoengineering” - but not under the SRM or CDR categories.
  The Oxford dictionary says:

·*the deliberate large-scale manipulation of an environmental
process that affects the earth’s climate, in an attempt to counteract the
effects of global warming.*



5.  Since you “obviously need a three-letter acronym, a few possibilities
(has to work at both poles, with both long and short pipes) are:  “PIM=
Polar Ice Making”, “PPI = Polar Passive Ice-Making”,  “PHP = Polar Heat
Pipe”,  “PHI = Polar Heatpipe Ice-making” .

These are maybe not inclusive enough terms.  Maybe “TET = Thermal
Energy Transfer”  or “PET=Passive Energy Transfer”  or “POC  - Passive
Ocean Cooling”



Best stop until we hear more about past pipeline economics, and more
knowledgable feasibility responses than mine.  Again thanks.



Ron





On Jan 14, 2014, at 3:59 PM, Keith Henson hkeithhen...@gmail.com wrote:



I wonder if anyone has thought about stopping the Pine Island Glacier
by freezing it to bedrock?

What it would take is a number of thermal diodes.  They were used on
the Alaskan pipeline to keep it from sinking over areas of permafrost.

All they are is a hole drilled to the bottom of the glacier, lined
with a closed end pipe, a heat radiator on the top and a few gallons
of propane or ammonia.

The way they work is that when the air is colder than the bottom of
the pipe, the liquid boils at the bottom, sucking out heat, vapors go
up and liquid runs back down.  The process stops when it is warmer on
top than at the bottom.

They are not very expensive, each one (over time) freezes a large area
of the glacier to the underlying rock.

A floating version can freeze a substantial block of ice out of
seawater in the winter.

I wonder if this would be considered geoengineering?

Keith


On Tue, Jan 14, 2014 at 2:31 PM, Ronal W. Larson
rongretlar...@comcast.net wrote:

Greg etal

  Because this paper is behind a paywall,  I can barely glean from their
figures that they may be looking at a fifty year time horizon.  Did they
look at all at either SRM or CDR when using the term “irreversibility?
(quotes in the original - why?)

Ron


On Jan 14, 2014, at 12:43 PM, Greg Rau gh...@sbcglobal.net wrote:

http://www.commondreams.org/headline/2014/01/13-2
Antarctic Glacier's 'Irreversible' Melting Threatens 'Considerable Increase'
to Sea Level Rise
New study on Pine Island Glacier shows 'striking vision of the near future,'
says co-author
- Andrea Germanos, staff writer
An Antarctic glacier is melting irreversibly, offering a striking vision
of the near future, a new study shows.
The study published Sunday in the journal Nature Climate Change looked at
Pine Island Glacier, the largest single contributor to sea-level rise in the

Re: [geo] Case Study by Holly Buck on Haida Gwaii OIF demonstration

2014-01-15 Thread Holly Buck
Hi Jim,

Part of the purpose of the piece is to show how such an event can have diverse 
and contested interpretations; I appreciate hearing yours and Gloria's 
perspectives.  

I do think the idea of village science is more than just a framing or PR, and 
worthy of further thought. For me village science connotes something about 
scale.  I've been to HSRC's company office in Vancouver, as well as spent some 
time in the village of Old Massett, and there's a huge jump between the 
resources HSRC had and what would be available to a lab in a research 
university.  You can hardly compare it— so I don't mean that all the work was 
literally done in a village, but that both the funds and the research protocol 
were smaller, more personal and DIY, than what you would get in what would have 
been a very expensive study if it had been done by an established research 
institution.  I think it's village science by comparison to science with 
national-scale funding, levels of formality and hierarchy, less personal 
relationships, etc.

  The reason I think this is important to think about is that it's quite 
possible that people other than university scientists may want to participate 
in various types of science / climate remediation / geoengineering, and not all 
of them will be rogue; some may be concerned citizens or makers, though of 
course at this point it's hard to imagine a group taking an action that has 
planetary-level effects.  I think there's a cultural turn— with the idolization 
of Silicon Valley wizards who didn't go to college, and bootstrapping, and 
everyone should learn to code, and the maker movement— towards people 
without advanced research degrees being involved in data-driven science, and 
not just for creating flashy apps, but for real-world problems.  Traditional 
research institutions can try to keep a monopoly on solutions and research, 
or find more creative ways to engage with other groups who might have different 
methods and levels of expertise and resources. So it's worth thinking about 
what scales geoengineering might happen on, and the interactions between these 
scales, no matter if you're seeking moratoriums or increased research funding 
or governance protocols.  

Cheers, Holly


On 15 Jan 2014, at 11:54 AM, jim thomas j...@etcgroup.org wrote:

 Hi Holly
 
 Thanks for the interesting paper and comments below
 
 Regarding whether a cook describes themself as a cook or an engineer 
 describes themself as an engineer (does a con artist describe themselves as a 
 con artist??): I think you maybe give a little too much credence to John 
 Disney's after-the-fact claim that  I never once heard the term 
 ‘geoengineering’.. Of course its important to take your interview subjects 
 at their word and give them the benefit of the doubt but John Disney had 
 worked for many years with his colleague Russ George whose previous iron 
 fertilization endeavours with Planktos have been widely and  very commonly 
 described as geoengineering going back to at least 2003. I find it very 
 surprising that John Disney would not have heard this word associated with 
 ocean fertilization. Russ George himself certainly knew his own work was 
 commonly described as geoengineering. Until last year Russ was the main mover 
 behind HSRC, he appears to have written all of their public materials, owned 
 a majority of the company, chaired the board and seemingly made all the key 
 decisions until he became too much of a liability for the Old Massett band 
 council to be associated with. All the deliberate framing of 'village 
 science' and 'stewardship of ocean pastures' is 100% Russ George PR talk. 
 
  The 'village science' framing is especially open to question as to its 
 authenticity. As I understand it from reports out of the village and what 
 names were publically shared almost the entire crew of the Ocean Pearl was 
 non-Haida, - the same is true of its past and present day to day leadership, 
 The 'research' and most of the company activities was carried out in 
 Vancouver (not in old Massett). An account of what happened in the village by 
 Gloria Tauber which you  can read on p4 of the attached newsletter  describes 
 that the crew had been assembled and contracts signed before the village even 
 learned about the scheme. let alone voted on it. I just noticed that Gloria 
 has also posted an extensive response  on your original piece that gives a 
 bit more of the 'village perspective'.
 
 a few other small points:
 
 You  quote an interview subject (Macnamee?) as describing the research 
 purpose of the ocean fertilization event to be answering the question  “Does 
 adding a trace amount of iron to an HNLC[1] ocean eddy located in a known 
 salmon migration route cause phytoplankton to grow, and if so, what are the 
 resulting environmental benefits or costs?”. Once again this is an 
 after-the-fact description. As far as i'm aware no research protocols were 
 ever made available to the 

[geo] Making ice (change of thread title)

2014-01-15 Thread Ronal W. Larson
Keith:
   I go through line by line - but deleting as much as I can.  Mine all in bold 
caps.


On Jan 15, 2014, at 10:28 AM, Keith Henson hkeithhen...@gmail.com wrote:

 On Tue, Jan 14, 2014 at 9:50 PM, Ronal W. Larson
 rongretlar...@comcast.net wrote:
 Keith:
 
 Again thanks
 
 Re- being able to make thicker ice in the Arctic - from the bottom, not the
 top.
 
 I don't see it being the bottom.  The ocean is thousands of feet deep
 and I can't see making these thing more than a 100 feet, say 30 meters
 long.
 [RWL1:  I am projecting only adding like a meter to ice that is already 
(hypothetically) a meter thick - so it can get through a September area/extent 
minimum.  Most Arctic ice forms from the bottom - only a little from falling 
snow.  Asking Peter for more input here on best thickness change projections.
I project something that can be thrown from a helicopter wherever an 
opening crack appears.  Only operates when there is already a little ice.
   This might work also to extend the area of Antarctic ice, keeping the 
area/extent up for more months.  By not deploying in some areas, you can keep 
some transport lanes open.



 Snip two

 The Antarctic case seems a bit harder - with a need for stiffer, stronger
 pipe. Any reason the floating Arctic unit couldn’t be made of a thinner
 plastic and get closer to a $1 or so per foot (with a total of (?) less than
 10 feet?)
 
 I doubt it.  The floating versions have to stand a fair amount of
 pressure just from the water pressure on them.  But no matter the
 cost, who is going to pay for them?  Polar bears?
 [RWL2:   I don’t get the “pressure” issue.  These can be relatively thick 
walled plastic, and the shape is appropriate for compression forces.  I don’t 
see much shear for floating ice a few meters thick.  Again - Peter?

 
 I hope you can find your earlier cost calculations.  I think we have a
 chicken and egg situation.  The person finding the money (John Nissen?) will
 have to have some cost calculations.
 
 It would take a few days with a spreadsheet.  I think I figured them
 out years ago on the basis of a 5 year ball of ice several hundred
 feet in diameter.  But that's just the start of the complexity.  The
 wind blows the ice around and in spite if being in the middle of some
 very hard ice, the heat pipes are going to get broken on a regular
 basis.
 
 Make a case that someone would pay for it and I can run off the calculation.
 
 Then again, you can probably ignore the hardware cost since the legal
 expenses are likely to dominate.
 [RWL3:  We have very different geometries in mind - as above, I am hoping 
for diameters like yours , but only a thickness like a meter.  I ask Peter 
Flynn for support on whether this might seem possible.   Re breakage, that 
would be the purpose of some early testing.
   I’m afraid in this game there are no design funds - all open source.

again snip a bit

 It would be great if anyone could make a synthetic
 char, starting with CO2.
 
 That's been done decades ago.  NASA had a project that would reduce
 CO2 to carbon flakes and oxygen.  It's also an energy hog, not as bad
 as synthetic wax or oil, but you can't pump char.
  [RWL4:  I don’t want carbon, I want something that has big interior 
surface area and very low density;  charcoal.   I have not looked into the NASA 
literature on recycling CO2 and will.  But hope someone can comment.  I doubt 
it will lead to a structure that looks like charcoal  (needed to get high CEC - 
cation exchange capacity and other desirable features that cost nothing with 
char.).

 
 I once read that no-one knows how to make a
 synthetic volcanic lava (maybe no longer true, anyone?   It would make a
 great material for simple char-making carbon-negative stoves.)
 
 Melted rock is easy.  But I don't get a carbon-negative stove.
 Plants *and* a char process together are carbon negative, sort of.
 The carbon returns to the air in less than geological time.
[RWL5.  Sorry, I didn’t explain enough on the lava question.  I am looking 
for a very light weight porous but very strong, heat resistive material.  I 
have seen an ideal product that is “sawn”commercially  out of a solid lava 
mountain in Nicaragua.  Melted rock is not what is needed - too dense.
 Any char-making stove (look up the word “TLUD”) can be carbon negative if 
the char is placed in soil (then changing name to “biochar”).  Yes lifetime is 
an issue, but char is used for anthropological dating going back millions of 
years.  We will be happy with a commonly used value of 1000 - and can live with 
less.

 
 Your proposed diode will operate with the “hot” side always around 0 oC, and
 the cold side dependent on the nighttime air temperature that (not looking
 anything up) might average -30 or -40 oC.
 
 No, the hot end goes down to the lowest temperature of the air, less
 relatively minor heat leakage.
[RWL6:  Not understanding.  Ask for Peter Flynn’s help again.  If you are 

[geo] Building Climate Solutions Conference

2014-01-15 Thread Rau, Greg
Good news - looks like buildings, agriculture, and natural resources are going 
to do the heavy lifting in solving AGW. Geoengineers need not apply. Greg

[Email-Banner-2]http://www.buildingclimatesolutions.org/
[2014-Vision-2]http://www.buildingclimatesolutions.org/topics/view/51cbfca3f702fc2ba8130b34/
[2014-Registration]http://www.buildingclimatesolutions.org/topics/view/523af4fc0cf264abcd6728be/
[2014-Agenda]http://www.buildingclimatesolutions.org/topics/view/51cbfca3f702fc2ba8130b33/
[2014-Venue2014]http://www.buildingclimatesolutions.org/topics/view/523a08ef0cf264abcd587ac3/
[2014-Leadership]http://www.buildingclimatesolutions.org/topics/view/51cbfca2f702fc2ba8130aa0
[2014-Sponsorship]http://www.buildingclimatesolutions.org/topics/view/523208a70cf2ea76e5235e3a/
[2014-Exhibit]http://www.buildingclimatesolutions.org/topics/view/52320c310cf264abcccfb669
[2014-Posters]http://www.buildingclimatesolutions.org/topics/view/5238d2b30cf264abcd4024cd/
[2014-Collabs]http://www.buildingclimatesolutions.org/topics/view/523711040cf2ea76e573f557
[2014-Affiliates]http://www.buildingclimatesolutions.org/topics/view/5239e8f10cf2ea76e5aa415d

Please note the
NEW VENUE:
Hyatt Regency Crystal 
Cityhttp://crystalcity.hyatt.com/en/hotel/our-hotel/map-and-directions.html
at Washington, D.C. National Airport
Hotel reservations close January 13, 2014

HYATT VIP WELCOME CONTEST

What can make the soothing décor of a Hyatt Regency Crystal City Guestroom more 
inviting? What about a plate of Chocolate Truffles or an Artisans Meats and 
Cheese platter when you arrive? Each month a lucky conference attendee will 
randomly be selected to receive a complementary Hyatt VIP Welcome Amenity.

You must be registered for the 
conferencehttps://www.cvent.com/events/2014-building-climate-solutions-conference/registration-715b726def1245288b37276db2dc3c38.aspx
 and book at least one night stay at the host 
hotelhttps://aws.passkey.com/g/20484301 to be eligible.  One more winner will 
be announce before the conference!



Registration Rates:

Individual Attendee:
$495 - three days
$275 - single day

Full-time Student:
$345 - three days
$190 - single day

Federal Employee:
$445 - three days
$250 - single day
___
Non-profit Organization:
$395 - three days
$220 - single day

University or Community College Affiliate Member:
 Complimentary



The 14th National Conference and Global Forum on Science, Policy and the 
Environment: Building Climate Solutions will engage over 1,200 key individuals 
from many fields of sciences and engineering, government and policy, business 
and civil society to advance solutions to minimize the causes and consequences 
of anthropogenic climate change.

The conference will be organized around two areas: [1]The Built Environment; 
and [2] Agriculture and Natural Resources.  Under these two themes, 24 tracks 
connect the conference to specific initiatives led by partnering organizations 
that advance solutions. In this manner, participants will engage with and have 
lasting impact on real world responses to climate change.


We invite you to join with others, work across traditional boundaries, and 
contribute your insights and skills to addressing the most significant 
environmental challenge of our time.


[Register-Now-Button3]http://www.buildingclimatesolutions.org/topics/view/523af4fc0cf264abcd6728be/

Don't Miss These Keynote Speakers
[James Hansen cvent photo]
James Hansen, former Director of the NASA Goddard Institute for Space Studies 
(GISS), is Adjunct Professor and at Columbia University’s Earth Institute, 
where he directs a program in Climate Science, Awareness and Solutions. He was 
trained in physics and astronomy in the space science program of Dr. James Van 
Allen at the University of Iowa. His early research on the clouds of Venus 
helped identify their composition as sulfuric acid. Since the late 1970s, he 
has focused his research on Earth's climate, especially human-made climate 
change. Dr. Hansen is best known for his testimony on climate change to 
congressional committees in the 1980s that helped raise broad awareness of the 
global warming issue. He was elected to the National Academy of Sciences in 
1995 and was designated by Time Magazine in 2006 as one of the 100 most 
influential people on Earth. He has received numerous awards including the 
Carl-Gustaf Rossby and Roger Revelle Research Medals, the Sophie Prize and the 
Blue Planet Prize. Dr. Hansen is recognized for speaking truth to power, for 
identifying ineffectual policies as greenwash, and for outlining actions that 
the public must take to protect the future of young people and other life on 
our planet.

Hansen will receive the John H. Chafee Memorial Lecture Wednesday, January 29th 
at 6:15 p.m.


 [Gummer - cvent]


Rt. Hon. John Gummer, Lord Deben,Chairman of the UK Government’s Committee on 
Climate Change, served for sixteen years as a British minister in the 
governments of Margaret Thatcher and John Major, as 

Re: [geo] Making ice (change of thread title)

2014-01-15 Thread Andrew Lockley
Personally, I can't see these thermal diodes being at all practical.
Far cheaper and simpler to just break up the ice, or pump water on top
of it.  The maths is pretty simple.  The thermal diode can only be at
a temperature of the water, at a maximum.  It's heat transfer is a
function of the surface area exposed to the air.  This heat exchanger
is a manufactured item, and thus expensive, with a small surface area.
 Flooding the ice with seawater gives a far higher surface area and
thus far higher heat transfer.

A

On 15 January 2014 21:58, Ronal W. Larson rongretlar...@comcast.net wrote:
 Keith:
I go through line by line - but deleting as much as I can.  Mine all in
 bold caps.


 On Jan 15, 2014, at 10:28 AM, Keith Henson hkeithhen...@gmail.com wrote:

 On Tue, Jan 14, 2014 at 9:50 PM, Ronal W. Larson
 rongretlar...@comcast.net wrote:

 Keith:

 Again thanks

 Re- being able to make thicker ice in the Arctic - from the bottom, not the
 top.


 I don't see it being the bottom.  The ocean is thousands of feet deep
 and I can't see making these thing more than a 100 feet, say 30 meters
 long.

  [RWL1:  I am projecting only adding like a meter to ice that is already
 (hypothetically) a meter thick - so it can get through a September
 area/extent minimum.  Most Arctic ice forms from the bottom - only a little
 from falling snow.  Asking Peter for more input here on best thickness
 change projections.
 I project something that can be thrown from a helicopter wherever an
 opening crack appears.  Only operates when there is already a little ice.
This might work also to extend the area of Antarctic ice, keeping the
 area/extent up for more months.  By not deploying in some areas, you can
 keep some transport lanes open.



 Snip two


 The Antarctic case seems a bit harder - with a need for stiffer, stronger
 pipe. Any reason the floating Arctic unit couldn’t be made of a thinner
 plastic and get closer to a $1 or so per foot (with a total of (?) less than
 10 feet?)


 I doubt it.  The floating versions have to stand a fair amount of
 pressure just from the water pressure on them.  But no matter the
 cost, who is going to pay for them?  Polar bears?

  [RWL2:   I don’t get the “pressure” issue.  These can be relatively
 thick walled plastic, and the shape is appropriate for compression forces.
 I don’t see much shear for floating ice a few meters thick.  Again - Peter?


 I hope you can find your earlier cost calculations.  I think we have a
 chicken and egg situation.  The person finding the money (John Nissen?) will
 have to have some cost calculations.


 It would take a few days with a spreadsheet.  I think I figured them
 out years ago on the basis of a 5 year ball of ice several hundred
 feet in diameter.  But that's just the start of the complexity.  The
 wind blows the ice around and in spite if being in the middle of some
 very hard ice, the heat pipes are going to get broken on a regular
 basis.

 Make a case that someone would pay for it and I can run off the calculation.

 Then again, you can probably ignore the hardware cost since the legal
 expenses are likely to dominate.

  [RWL3:  We have very different geometries in mind - as above, I am
 hoping for diameters like yours , but only a thickness like a meter.  I ask
 Peter Flynn for support on whether this might seem possible.   Re breakage,
 that would be the purpose of some early testing.
I’m afraid in this game there are no design funds - all open source.

again snip a bit


 It would be great if anyone could make a synthetic
 char, starting with CO2.


 That's been done decades ago.  NASA had a project that would reduce
 CO2 to carbon flakes and oxygen.  It's also an energy hog, not as bad
 as synthetic wax or oil, but you can't pump char.

   [RWL4:  I don’t want carbon, I want something that has big interior
 surface area and very low density;  charcoal.   I have not looked into the
 NASA literature on recycling CO2 and will.  But hope someone can comment.  I
 doubt it will lead to a structure that looks like charcoal  (needed to get
 high CEC - cation exchange capacity and other desirable features that cost
 nothing with char.).


 I once read that no-one knows how to make a
 synthetic volcanic lava (maybe no longer true, anyone?   It would make a
 great material for simple char-making carbon-negative stoves.)


 Melted rock is easy.  But I don't get a carbon-negative stove.
 Plants *and* a char process together are carbon negative, sort of.
 The carbon returns to the air in less than geological time.

 [RWL5.  Sorry, I didn’t explain enough on the lava question.  I am
 looking for a very light weight porous but very strong, heat resistive
 material.  I have seen an ideal product that is “sawn”commercially  out of a
 solid lava mountain in Nicaragua.  Melted rock is not what is needed - too
 dense.
  Any char-making stove (look up the word “TLUD”) can be carbon negative
 if the char is 

[geo] Re: Making ice (change of thread title)

2014-01-15 Thread Keith Henson
On Wed, Jan 15, 2014 at 1:58 PM, Ronal W. Larson
rongretlar...@comcast.net wrote:
 Keith:
I go through line by line - but deleting as much as I can.  Mine all in
 bold caps.


 On Jan 15, 2014, at 10:28 AM, Keith Henson hkeithhen...@gmail.com wrote:

 On Tue, Jan 14, 2014 at 9:50 PM, Ronal W. Larson
 rongretlar...@comcast.net wrote:

 Keith:

 Again thanks

 Re- being able to make thicker ice in the Arctic - from the bottom, not the
 top.

 I don't see it being the bottom.  The ocean is thousands of feet deep
 and I can't see making these thing more than a 100 feet, say 30 meters
 long.

  [RWL1:  I am projecting only adding like a meter to ice that is already
 (hypothetically) a meter thick - so it can get through a September
 area/extent minimum.  Most Arctic ice forms from the bottom - only a little
 from falling snow.  Asking Peter for more input here on best thickness
 change projections.

I see, bottom of the ice layer, not bottom of the ocean.

 I project something that can be thrown from a helicopter wherever an
 opening crack appears.  Only operates when there is already a little ice.

That's a long way from how I modeled this.  I figured starting with
open water and freezing cylinders of ice in the 100 meter diameter
range and that deep. They would drift into hexagonal aggregations that
would be harder to overturn and perhaps thick enough to resist
buckling from wind forces.

Dropping anything from a helicopter runs the price up by an order of
magnitude, at least.

This might work also to extend the area of Antarctic ice, keeping the
 area/extent up for more months.  By not deploying in some areas, you can
 keep some transport lanes open.

 Snip two

 The Antarctic case seems a bit harder - with a need for stiffer, stronger
 pipe. Any reason the floating Arctic unit couldn’t be made of a thinner
 plastic and get closer to a $1 or so per foot (with a total of (?) less than
 10 feet?)

 I doubt it.  The floating versions have to stand a fair amount of
 pressure just from the water pressure on them.  But no matter the
 cost, who is going to pay for them?  Polar bears?

  [RWL2:   I don’t get the “pressure” issue.  These can be relatively
 thick walled plastic, and the shape is appropriate for compression forces.
 I don’t see much shear for floating ice a few meters thick.  Again - Peter?

The walls have to be thick enough to deal with the pressure of propane
or ammonia at least.  Then they have to resist the effects of a few
atmospheres of water pressure on them at the bottom.  Think of the
wall thickness fraction as being at least that of a propane bottle you
hook up to the grill.

 I hope you can find your earlier cost calculations.  I think we have a
 chicken and egg situation.  The person finding the money (John Nissen?) will
 have to have some cost calculations.

 It would take a few days with a spreadsheet.  I think I figured them
 out years ago on the basis of a 5 year ball of ice several hundred
 feet in diameter.  But that's just the start of the complexity.  The
 wind blows the ice around and in spite if being in the middle of some
 very hard ice, the heat pipes are going to get broken on a regular
 basis.

 Make a case that someone would pay for it and I can run off the calculation.

 Then again, you can probably ignore the hardware cost since the legal
 expenses are likely to dominate.

  [RWL3:  We have very different geometries in mind - as above, I am
 hoping for diameters like yours , but only a thickness like a meter.  I ask
 Peter Flynn for support on whether this might seem possible.   Re breakage,
 that would be the purpose of some early testing.
I’m afraid in this game there are no design funds - all open source.

Not concerned with getting paid for the design work, but it's
pointless if nobody will ever pay for testing or deployment.  Any
ideas?  Do you suppose friends of the polar bears might fund a test?

snip

 Your proposed diode will operate with the “hot” side always around 0 oC, and
 the cold side dependent on the nighttime air temperature that (not looking
 anything up) might average -30 or -40 oC.

 No, the hot end goes down to the lowest temperature of the air, less
 relatively minor heat leakage.

 [RWL6:  Not understanding.  Ask for Peter Flynn’s help again.  If you
 are boiling a fluid at the bottom the thermal energy movement is upward.
 Maybe we are not disagreeing - but the bottom “hot end in a heat pipe sense
 has to be a good bit warmer than the atmospheric above ground (condensing)
 temperature to have heat transfer.

That's not the case.  Heat pipes have the capacity to move heat
thousands of time better than the best metal conductors. I would be
surprised to find more than a degree difference from the bottom of the
pipe to the top.  As the cold end gets colder, the pressure in the
heat pipe decreases, which lowers the boiling point of the working
fluid.

https://en.wikipedia.org/wiki/Heat_pipe


RE: [geo] Making ice (change of thread title)

2014-01-15 Thread Doug MacMartin
The only advantage is the disposition of the salt - making ice thicker at
the bottom ensures that the salt stays in the water, not the ice.  As has
been pointed out before, we don't know what happens with the salt if you
flood the ice from the top, nor whether higher-salinity ice creates a
problem by melting earlier.   

However, given that the oil industry seems to use this approach regularly,
it seems like it ought to be relatively straightforward for the right person
to actually collect some data rather than simply trading hypotheses.  (The
right person almost certainly isn't me, much though I'd love the excuse to
head up to the Beaufort sea.)

-Original Message-
From: geoengineering@googlegroups.com
[mailto:geoengineering@googlegroups.com] On Behalf Of Andrew Lockley
Sent: Wednesday, January 15, 2014 4:24 PM
To: Ronal Larson
Cc: Keith Henson; Geoengineering; John Nissen; Peter Flynn; RAU greg
Subject: Re: [geo] Making ice (change of thread title)

Personally, I can't see these thermal diodes being at all practical.
Far cheaper and simpler to just break up the ice, or pump water on top
of it.  The maths is pretty simple.  The thermal diode can only be at
a temperature of the water, at a maximum.  It's heat transfer is a
function of the surface area exposed to the air.  This heat exchanger
is a manufactured item, and thus expensive, with a small surface area.
 Flooding the ice with seawater gives a far higher surface area and
thus far higher heat transfer.

A

On 15 January 2014 21:58, Ronal W. Larson rongretlar...@comcast.net wrote:
 Keith:
I go through line by line - but deleting as much as I can.  Mine all in
 bold caps.


 On Jan 15, 2014, at 10:28 AM, Keith Henson hkeithhen...@gmail.com wrote:

 On Tue, Jan 14, 2014 at 9:50 PM, Ronal W. Larson
 rongretlar...@comcast.net wrote:

 Keith:

 Again thanks

 Re- being able to make thicker ice in the Arctic - from the bottom, not
the
 top.


 I don't see it being the bottom.  The ocean is thousands of feet deep
 and I can't see making these thing more than a 100 feet, say 30 meters
 long.

  [RWL1:  I am projecting only adding like a meter to ice that is
already
 (hypothetically) a meter thick - so it can get through a September
 area/extent minimum.  Most Arctic ice forms from the bottom - only a
little
 from falling snow.  Asking Peter for more input here on best thickness
 change projections.
 I project something that can be thrown from a helicopter wherever an
 opening crack appears.  Only operates when there is already a little ice.
This might work also to extend the area of Antarctic ice, keeping the
 area/extent up for more months.  By not deploying in some areas, you can
 keep some transport lanes open.



 Snip two


 The Antarctic case seems a bit harder - with a need for stiffer, stronger
 pipe. Any reason the floating Arctic unit couldn't be made of a thinner
 plastic and get closer to a $1 or so per foot (with a total of (?) less
than
 10 feet?)


 I doubt it.  The floating versions have to stand a fair amount of
 pressure just from the water pressure on them.  But no matter the
 cost, who is going to pay for them?  Polar bears?

  [RWL2:   I don't get the pressure issue.  These can be relatively
 thick walled plastic, and the shape is appropriate for compression forces.
 I don't see much shear for floating ice a few meters thick.  Again -
Peter?


 I hope you can find your earlier cost calculations.  I think we have a
 chicken and egg situation.  The person finding the money (John Nissen?)
will
 have to have some cost calculations.


 It would take a few days with a spreadsheet.  I think I figured them
 out years ago on the basis of a 5 year ball of ice several hundred
 feet in diameter.  But that's just the start of the complexity.  The
 wind blows the ice around and in spite if being in the middle of some
 very hard ice, the heat pipes are going to get broken on a regular
 basis.

 Make a case that someone would pay for it and I can run off the
calculation.

 Then again, you can probably ignore the hardware cost since the legal
 expenses are likely to dominate.

  [RWL3:  We have very different geometries in mind - as above, I am
 hoping for diameters like yours , but only a thickness like a meter.  I
ask
 Peter Flynn for support on whether this might seem possible.   Re
breakage,
 that would be the purpose of some early testing.
I'm afraid in this game there are no design funds - all open source.

again snip a bit


 It would be great if anyone could make a synthetic
 char, starting with CO2.


 That's been done decades ago.  NASA had a project that would reduce
 CO2 to carbon flakes and oxygen.  It's also an energy hog, not as bad
 as synthetic wax or oil, but you can't pump char.

   [RWL4:  I don't want carbon, I want something that has big interior
 surface area and very low density;  charcoal.   I have not looked into the
 NASA literature on recycling CO2 and will.  But hope someone can 

Re: [geo] Making ice (change of thread title)

2014-01-15 Thread Andrew Lockley
Hi

I accept that glacier grounding may have a use for thermal diodes, but
in sea ice they're pretty useless.

Breaking ice works well, because ice is an excellent thermal
insulator.  Icebreaker paths are cheap.  Broken, the cold air hits the
sea, and the water can also radiate to deep space.

The thermal diodes can't exchange heat any faster than the temperature
gradient over their surface area will allow.  Mechanical pumps expose
a huge area of water (the same temperature as the base of the thermal
diodes).  The principle is one of leverage.  Small pump - big surface
area of water.  Vs.  Small diode - small surface area of diode.

A

On 16 January 2014 01:16, Keith Henson hkeithhen...@gmail.com wrote:
 On Wed, Jan 15, 2014 at 4:24 PM, Andrew Lockley
 andrew.lock...@gmail.com wrote:
 Personally, I can't see these thermal diodes being at all practical.

 That's probably true. But don't forget that we are considering two
 problems, nailing down glaciers and restoring ice cover on the ocean.

 Far cheaper and simpler to just break up the ice, or pump water on top
 of it.

 I don't see how braking up the ice will help thicken it so it survives
 over the summer.  Could you explain?

 The maths is pretty simple.  The thermal diode can only be at
 a temperature of the water, at a maximum.

 I don't think you have a good model of a thermal diode.  The ones
 along the Alaskan pipeline freeze a large ball of permafrost rock hard
 because the deep end of the pipe goes down to the minimum air
 temperature during the winter.

  It's heat transfer is a
 function of the surface area exposed to the air.  This heat exchanger
 is a manufactured item,

 So are pumps.

 and thus expensive, with a small surface area.
  Flooding the ice with seawater gives a far higher surface area and
 thus far higher heat transfer.

 How many pumps?  How do you power them?  Does this accomplish the goal
 of keeping an ice cover on the Arctic ocean over the summer?  Not
 being snarky, I just don't know.

 Keith

 A

 On 15 January 2014 21:58, Ronal W. Larson rongretlar...@comcast.net wrote:
 Keith:
I go through line by line - but deleting as much as I can.  Mine all in
 bold caps.


 On Jan 15, 2014, at 10:28 AM, Keith Henson hkeithhen...@gmail.com wrote:

 On Tue, Jan 14, 2014 at 9:50 PM, Ronal W. Larson
 rongretlar...@comcast.net wrote:

 Keith:

 Again thanks

 Re- being able to make thicker ice in the Arctic - from the bottom, not the
 top.


 I don't see it being the bottom.  The ocean is thousands of feet deep
 and I can't see making these thing more than a 100 feet, say 30 meters
 long.

  [RWL1:  I am projecting only adding like a meter to ice that is already
 (hypothetically) a meter thick - so it can get through a September
 area/extent minimum.  Most Arctic ice forms from the bottom - only a little
 from falling snow.  Asking Peter for more input here on best thickness
 change projections.
 I project something that can be thrown from a helicopter wherever an
 opening crack appears.  Only operates when there is already a little ice.
This might work also to extend the area of Antarctic ice, keeping the
 area/extent up for more months.  By not deploying in some areas, you can
 keep some transport lanes open.



 Snip two


 The Antarctic case seems a bit harder - with a need for stiffer, stronger
 pipe. Any reason the floating Arctic unit couldn’t be made of a thinner
 plastic and get closer to a $1 or so per foot (with a total of (?) less than
 10 feet?)


 I doubt it.  The floating versions have to stand a fair amount of
 pressure just from the water pressure on them.  But no matter the
 cost, who is going to pay for them?  Polar bears?

  [RWL2:   I don’t get the “pressure” issue.  These can be relatively
 thick walled plastic, and the shape is appropriate for compression forces.
 I don’t see much shear for floating ice a few meters thick.  Again - Peter?


 I hope you can find your earlier cost calculations.  I think we have a
 chicken and egg situation.  The person finding the money (John Nissen?) will
 have to have some cost calculations.


 It would take a few days with a spreadsheet.  I think I figured them
 out years ago on the basis of a 5 year ball of ice several hundred
 feet in diameter.  But that's just the start of the complexity.  The
 wind blows the ice around and in spite if being in the middle of some
 very hard ice, the heat pipes are going to get broken on a regular
 basis.

 Make a case that someone would pay for it and I can run off the calculation.

 Then again, you can probably ignore the hardware cost since the legal
 expenses are likely to dominate.

  [RWL3:  We have very different geometries in mind - as above, I am
 hoping for diameters like yours , but only a thickness like a meter.  I ask
 Peter Flynn for support on whether this might seem possible.   Re breakage,
 that would be the purpose of some early testing.
I’m afraid in this game there are no design funds - all