RE: [geo] SRM offset standards?

2020-05-04 Thread Douglas MacMartin
Tim – the difference between the 0.22% and 2% is (i) factor of 4 from ratio of 
projected area to surface area of a sphere, (ii) factor of 1/0.7 to account for 
the existing albedo of the Earth, (iii) factor of 3/3.7 since 2% is a rough 
estimate for 2xCO2, and (iv) efficacy of response to solar vs CO2 is not one 
(that is, the same radiative forcing doesn’t give the same warming for 
different mechanisms, see Hansen et al 2015).

From: geoengineering@googlegroups.com  On 
Behalf Of Tim Sippel
Sent: Monday, May 4, 2020 4:08 AM
To: geoengineering 
Subject: Re: [geo] SRM offset standards?

Thanks for the feedback.  It was great to learn about a planned December 2020 
publication of ISO 14082, which is being drafted as a standard for radiative 
forcing accounting.  Now I am also aware of Andrew's 2016 'License to chill' 
paper (1).

Methane reductions qualify for carbon offsets, despite the fact that the 
methane breaks down in the atmosphere over about a decade.  So if the lifetime 
of a solar sail can be 20 years (not uncommon for many satellites), maybe it 
will be reasonable to qualify for some form of SRM offset standard.  It should 
be easier to make funding decisions once the benefits are quantified in a 
standard.

GeoShade is focused on a 1km radius design that deploys to sub-L1. A key metric 
is g/m^2, which determines the craft's solar acceleration.  L1 is 1.5M km from 
earth.  A new location farther sunward from L1 (maybe 2.4M km) will be an 
equilibrium position that accounts for the sail's solar acceleration.  Using 
its sail, active stationkeeping is possible without any fuel-based thrust.  The 
GeoShade design doesn't rely on any exotic technologies.  It uses existing 
materials that are manufactured terrestrially.  It doesn't rely on capturing an 
asteroid for building materials. The goal is to be able to manufacture and 
deploy in a relatively short amount of time.  So it is very different from a 
2006 proposal by Roger Angel (2).

A 1km radius disk at sub-L1 can cancel the radiative forcing of about 10M tons 
of CO2 emissions (based on calculations I mentioned previously).  I can't 
imagine trying to cancel out ALL anthropogenic RF with mirrors.  To cancel 
today's 3W of RF requires 3/1367 W/m^2 = 0.2% of earth's sunlight (although 
elsewhere I see a value of 2.0% being used).  The intent would be to supplement 
the primary ongoing efforts to replace fossil fuel energy with renewable energy 
sources.  These sun shades are to help buy time since we are not progressing as 
quickly as needed to achieve the IPCC 1.5C target.

The cost for the GeoShade design is estimated to be about $10/ton equivalent.  
(Based on IPCC 2018 2.8.4, it seems sufficient to assume a linear relationship 
rather than logrithmic.)  My impression is that $10/ton is 10X to 100X the cost 
of other SRM options.  (Pointers to better estimates would be appreciated.)  
Hopefully the cost remains low enough to be affordable as a temporary offset.

Could a space-based solution be used to lead the way in achieving approval for 
SRM offsets?  Once in position, sun shades look like a small sunspot.  
Hopefully something people can easily wrap their heads around.  The RF benefits 
may be easier to quantify, track, and control compared to other SRM methods.  
The solar reduction is guaranteed to be small and uniform amount across the 
globe.  It can be quickly stoped by turning the sails sideways.  As long as RF 
reductions are a small fraction of RF increases due to greenhouse gas 
emissions, concerns about unintendended consequences should be minimal.

For those interested in more details, the GeoShade design is based on a 
reflective film with a 3.9 g/m^2 density plus a 1X mass overhead for the 
structure and controls.  A 1km radius disk produces a thrust of about 20N, 
resulting in a solar acceleration of about 1mm/s^2.  Attitude control at sub-L1 
involves very slow adjustments of the center of mass vs. the center of 
pressure.  This is accomplished by adjusting the position of a mass, or by 
tilting a subset of sail panels.  The more difficult problem to solve was more 
dramatic attitude changes that are required to support orbit raising from its 
start at a high LEO (enabling a significant reduction in cost).  It will take 
about 1 year to sail to sub-L1.

(1) Licence to chill: Building a legitimate authorisation process for 
commercial SRM operations, 2016, Andrew Lockley.  
https://journals.sagepub.com/doi/10.1177/1461452916630082
(2) Feasibility of cooling the Earth with a cloud of small spacecraft near the 
inner Lagrange point (L1), 2006, Roger Angel, Univ of Arizona.  
http://www.pnas.org/content/pnas/103/46/17184.full.pdf

Reference Textbooks:
  Space Sailing, 1992, Wright
  Solar Sailing, 2004, McInnes
  Solar Sails, 2008, Vulpetti, Johnson, Matloff
  Advances in Solar Sailing, 2014, Editor: Macdonald

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Re: [geo] SRM offset standards?

2020-05-04 Thread Tim Sippel
Thanks for the feedback.  It was great to learn about a planned December 
2020 publication of ISO 14082, which is being drafted as a standard for 
radiative forcing accounting.  Now I am also aware of Andrew's 2016 
'License to chill' paper (1).

Methane reductions qualify for carbon offsets, despite the fact that the 
methane breaks down in the atmosphere over about a decade.  So if the 
lifetime of a solar sail can be 20 years (not uncommon for many 
satellites), maybe it will be reasonable to qualify for some form of SRM 
offset standard.  It should be easier to make funding decisions once the 
benefits are quantified in a standard.

GeoShade is focused on a 1km radius design that deploys to sub-L1. A key 
metric is g/m^2, which determines the craft's solar acceleration.  L1 is 
1.5M km from earth.  A new location farther sunward from L1 (maybe 2.4M km) 
will be an equilibrium position that accounts for the sail's solar 
acceleration.  Using its sail, active stationkeeping is possible without 
any fuel-based thrust.  The GeoShade design doesn't rely on any exotic 
technologies.  It uses existing materials that are manufactured 
terrestrially.  It doesn't rely on capturing an asteroid for building 
materials. The goal is to be able to manufacture and deploy in a relatively 
short amount of time.  So it is very different from a 2006 proposal by 
Roger Angel (2).

A 1km radius disk at sub-L1 can cancel the radiative forcing of about 10M 
tons of CO2 emissions (based on calculations I mentioned previously).  I 
can't imagine trying to cancel out ALL anthropogenic RF with mirrors.  To 
cancel today's 3W of RF requires 3/1367 W/m^2 = 0.2% of earth's sunlight 
(although elsewhere I see a value of 2.0% being used).  The intent would be 
to supplement the primary ongoing efforts to replace fossil fuel energy 
with renewable energy sources.  These sun shades are to help buy time since 
we are not progressing as quickly as needed to achieve the IPCC 1.5C target.

The cost for the GeoShade design is estimated to be about $10/ton 
equivalent.  (Based on IPCC 2018 2.8.4, it seems sufficient to assume a 
linear relationship rather than logrithmic.)  My impression is that $10/ton 
is 10X to 100X the cost of other SRM options.  (Pointers to better 
estimates would be appreciated.)  Hopefully the cost remains low enough to 
be affordable as a temporary offset.

Could a space-based solution be used to lead the way in achieving approval 
for SRM offsets?  Once in position, sun shades look like a small sunspot.  
Hopefully something people can easily wrap their heads around.  The RF 
benefits may be easier to quantify, track, and control compared to other 
SRM methods.  The solar reduction is guaranteed to be small and uniform 
amount across the globe.  It can be quickly stoped by turning the sails 
sideways.  As long as RF reductions are a small fraction of RF increases 
due to greenhouse gas emissions, concerns about unintendended consequences 
should be minimal.

For those interested in more details, the GeoShade design is based on a 
reflective film with a 3.9 g/m^2 density plus a 1X mass overhead for the 
structure and controls.  A 1km radius disk produces a thrust of about 20N, 
resulting in a solar acceleration of about 1mm/s^2.  Attitude control at 
sub-L1 involves very slow adjustments of the center of mass vs. the center 
of pressure.  This is accomplished by adjusting the position of a mass, or 
by tilting a subset of sail panels.  The more difficult problem to solve 
was more dramatic attitude changes that are required to support orbit 
raising from its start at a high LEO (enabling a significant reduction in 
cost).  It will take about 1 year to sail to sub-L1.

(1) Licence to chill: Building a legitimate authorisation process for 
commercial SRM operations, 2016, Andrew Lockley.  
https://journals.sagepub.com/doi/10.1177/1461452916630082
(2) Feasibility of cooling the Earth with a cloud of small spacecraft near 
the inner Lagrange point (L1), 2006, Roger Angel, Univ of Arizona.  
http://www.pnas.org/content/pnas/103/46/17184.full.pdf

Reference Textbooks:
  Space Sailing, 1992, Wright
  Solar Sailing, 2004, McInnes
  Solar Sails, 2008, Vulpetti, Johnson, Matloff
  Advances in Solar Sailing, 2014, Editor: Macdonald

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[geo] Newsletter of Week 19 of 2020

2020-05-04 Thread i...@climate-engineering.eu
Title: Climate Engineering Newsletter




  


 







 



Climate Engineering Newsletter
for Week 19 of 2020



 





04.-08.05.2020, Online conference: EGU2020: Sharing Geoscience Online (#shareEGU20), online
06.05.2020, CCIS 2020 Webinar Series: IAMs, Mitigation, and Scenario development for combined intervention strategies, online
06.05.2020, Webinar: Engineering the Carbon Economy Seminar Series: Holly Buck, UCLA - Can scaling up negative emissions be compatible with social and environmental justice? (LLNL), online
07.05.2020, Webinar: Carbon 180: Leading with Soil: How climate mitigation can unlock economic opportunity for farmers, online
13.05.2020, Conference: AirMiners 2020: Foundations for a Carbon Negative Future, online
20.05.2020, Pre-ACT webinar #5: CO2 storage case studies, online
27.05.2020, CCIS 2020 Webinar Series: Solar Radiation Management, online
10.06.2020, CCIS 2020 Webinar Series: Carbon Dioxide Removal, online
08.07.2020, CCIS 2020 Webinar Series: Observations, Lab and Field Studies, online
06. 08.2020, CCIS 2020 Webinar Series: Impacts for Climate Intervention Strategies, online
06.-09.10.2020, Conference: Climate Engineering in Context 2020, Berlin / Germany
21.-23. 10.2020, Workshop: Ecological Impacts of Solar Radiation Management, Port Jefferson, New York / USA
28.-30.10. 2020, Workshop: Community Climate Intervention Strategies, Boulder, CO / USA
02.-05.11.2020, Conference: 3rd Conference of the Arabian Journal of Geosciences (CAJG), Sousse / Tunisia
06.-13.12.2020, IEA Greenhouse Gas R Programme 2020 Summer School, Bandung / Indonesia
15.-18.03.2021, Conference: GHGT-15, Abu Dhabi / United Arab Emirates
18.-21.05.2021, Conference: 2nd International Conference on Negative CO2 Emissions, Gothenburg / Sweden



04.08.2020, Call for Applications: PICS Opportunity Projects Program - 2020 Zero-Emission Vehicles Project
04.08.2020, Call for Applications: PICS Opportunity Projects Program - 2020 Competition



10.05.2020, Job: NORCE Chief scientists
(no deadline), Job: Ph.D. Research Assistantship in climate and agricultural modeling in the Atmospheric Science Graduate Program at Rutgers University
(no deadline), Job: ClearPath: Policy Analyst (Carbon Capture & Removal)
(no deadline), Job: Postdoctoral Fellow Position – Global Warming in polar regions in ultra-high-resolution earth system model simulations



Gertler, Charles G.; et al. 2020: “Weakening of the Extratropical Storm Tracks in Solar Geoengineering Scenarios.”
Markusson, Nils; et al. 2020: “Social Science Sequestered.”
Duan, Lei; et al. 2020: “A Model‐Based Investigation of Terrestrial Plant Carbon Uptake Response to Four Radiation Modification Approaches.”
Talati, Shuchi; et al. 2020: “Once a Fringe Idea, Geoengineering Moves to Center Stage in Policy Arena.”



Carbon 180: Leading With Soil Report
National Energy Technology Laboratory. 2020: "Safe Geologic Storage of Captured Carbon Dioxide – DOE’s Carbon Storage R Program: Two Decades in Review."
Friedmann, S.J.; et al. 2020: “Capturing Investment: Policy Design to Finance CCUS Projects in the U.S. Power Sector.”
ICRLP. 2020: “Explainer: Carbon Removal.”



Project: Strategy CCUS
Project: C4U (Advanced Carbon Capture for steel industries integrated in CCUS Clusters)



Phys.org: New self-forming membrane to protect our environment
Legal Planet: Negative Emissions: The Next Bright Shiny Object in Greenhouse-Gas Emissions Reductions
Clean Air Task Force: Do it right – the IRS shows why it pays to comply with storage standards
Clean Air Task Force: The Status of Carbon Capture Projects in the U.S. (And What They Need to Break Ground)
Institution of Mechanical Engineers: Carbon capture and storage must be widely deployed to meet emission targets
Energy.gov: U.S. Department of Energy Announces $131 Million for CCUS Technologies
Strategy CCUS: Partner profile: ‘Industrial symbiosis’ will open up promising regions to CCUS
The Chemical Engineer: Japanese consortium to study CCU
Blog post: CSAG: Lebogang Matlakala: Is Solar Radiation Management a practical solution?
SRMGI: Interview with Dr. Izidine Pinto
Mining.com: Mining technologies could capture ‘billions of tonnes of CO2 per year,’ says UBC prof
Bloomberg: The Best Way to Slow Global Warming? You Decide in This Climate Simulator
Ethanol Producer Magazine: DOE funds CCUS project at ethanol plant, opens new CCUS FOA
Video: Carnegie Council for Ethics in International Affairs: Prospects for Global Coordination in an Age of Pandemics and Emerging Climate Technologies
Video: ICRLP Explainer Webinar: Direct Air Capture
ICRLP: Carbon Removal Glossary




 



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