Arctic geoengineering

Arctic sea ice coverage as of 2007 compared to 2005 and also compared to 1979-2000 average

Temperatures in the Arctic region have tended to increase more rapidly than the global average. Projections of sea ice loss that are adjusted to take account of recent rapid Arctic shrinkage suggest that the Arctic will likely be free of summer sea ice sometime between 2059 and 2078.[1] Various climate engineering schemes have been suggested to reduce the chance of significant and irreversible effects such as Arctic methane release.

Several climate engineering proposals have been made which are specific to the Arctic. They are usually hydrological in nature, and principally centre upon measures to prevent Arctic ice loss.

In addition, other solar radiation management climate engineering techniques, such as stratospheric sulfate aerosols[2] have been proposed. These would cool the Arctic by adjusting the albedo of the atmosphere.

The Arctic region plays an important role in the regulation of the Earth's climate. Conditions in the Arctic may suggest the existence of tipping points, including ice-albedo feedback from melting Arctic sea ice[3] and Arctic methane release from thawing permafrost and methane clathrate.[4] The speed of future retreat of the Arctic sea ice is contentious. The IPCC Fourth Assessment Report of 2007 states that "in some projections, Arctic late-summer sea ice disappears almost entirely by the latter part of the 21st century." However, the ice has since undergone unexpectedly significant retreat, reaching a record low area in summer 2007 before recovering somewhat in 2008.

A tipping point process could potentially commence as the Arctic region warms, if there is positive feedback with sufficient gain. Tim Lenton suggests that the retreat of sea ice is such a process, and the tipping may have started already.[5] Climate engineering has been proposed for preventing or reversing tipping point events in the Arctic, in particular to halt the retreat of the sea ice.

Preventing such ice loss is important for climate control, as the Arctic ice regulates global temperatures by virtue of its albedo, and also by restraining methane emissions from permafrost near the shoreline in the Arctic region.[6][7][unreliable source?] Additionally, the sea ice has a wider regional climatic role, and acts to maintain permafrost more generally in the region, by insulating the cold winter winds from the warm sea.[8]

It has been proposed to actively enhance the polar ice cap by spraying or pumping water onto the top of it which would build thicker sea ice.[5] As ice is an insulator, water on the surface of the ice tends to freeze more quickly than that below.

Thickening ice by spraying seawater onto existing ice has been proposed.[9][1] Sea ice is an effective thermal insulator, and thus freezing takes place much more rapidly on the top surface of the ice sheet than on the bottom. Thicker sea ice is more structurally stable, and is more resistant to melting due to its increased mass. An additional benefit of this method is that the increased salt content of the melting ice will tend to strengthen downwelling currents when the ice re-melts.[2]

Some ice in the sea is frozen seawater. Other ice comes from glaciers, which come from compacted snow, and is thus fresh water ice.

If salt water ice is made on top of fresh water ice, if it melts, it may rapidly perforate the lower layers of the ice sheet.[full citation needed] (Salt water melts at a lower temperature than fresh water does.) Some have speculated that river water could be used to thicken fresh water ice if this problem is deemed important.

Caldeira and Wood analysed the effect of climate engineering in the Arctic using stratospheric sulfate aerosols.[1] This technique is not specific to the Arctic region. He found that At high latitudes, there is less sunlight deflected per unit albedo change but climate system feedbacks operate more powerfully there. These two effects largely cancel each other, making the global mean temperature response per unit top-of-atmosphere albedo change relatively insensitive to latitude.[3]

It has been suggested[4] that locally influencing salinity and temperature of the Arctic Ocean, by changing the ratio of Pacific and fluvial waters entering through the Bering Strait could play a key role in preserving Arctic sea ice. The purpose would be to create a relative increase of fresh water inflow from the Yukon River, while blocking (part) of the warm and saltier waters from the Pacific Ocean. Proposed geoengineering options include a dam[5] connecting St. Lawrence Island and a threshold under the narrow part of the strait.

  1. ^ Boé, Julien; Hall, Alex; Qu, Xin (15 March 2009). "September sea-ice cover in the Arctic Ocean projected to vanish by 2100". Nature Geoscience. Springer Nature. 2 (5): 341–343. Bibcode:2009NatGe...2..341B. doi:10.1038/ngeo467. ISSN 1752-0894.
  2. ^ Crutzen, Paul J. (25 July 2006). "Albedo Enhancement by Stratospheric Sulfur Injections: A Contribution to Resolve a Policy Dilemma?" (PDF). Climatic Change. Springer Nature. 77 (3–4): 211–220. doi:10.1007/s10584-006-9101-y. ISSN 0165-0009.
  3. ^ Winton, Michael (13 December 2006). "Does the Arctic sea ice have a tipping point?". Geophysical Research Letters. American Geophysical Union (AGU). 33 (23): L23504. Bibcode:2006GeoRL..3323504W. doi:10.1029/2006gl028017. ISSN 0094-8276.
  4. ^ Archer, D.; Buffett, B.; Brovkin, V. (18 November 2008). "Ocean methane hydrates as a slow tipping point in the global carbon cycle". Proceedings of the National Academy of Sciences. 106 (49): 20596–20601. Bibcode:2009PNAS..10620596A. doi:10.1073/pnas.0800885105. ISSN 0027-8424. PMC 2584575. PMID 19017807.
  5. ^ Lenton, T. M.; Held, H.; Kriegler, E.; Hall, J. W.; Lucht, W.; Rahmstorf, S.; Schellnhuber, H. J. (7 February 2008). "Tipping elements in the Earth's climate system". Proceedings of the National Academy of Sciences. 105 (6): 1786–1793. Bibcode:2008PNAS..105.1786L. doi:10.1073/pnas.0705414105. ISSN 0027-8424. PMC 2538841. PMID 18258748.
  6. ^ Connor, Steve (23 September 2008). "Exclusive: The methane time bomb - Climate Change, Environment - The Independent". Arctic scientists discover new global warming threat as melting permafrost releases millions of tons of a gas 20 times more damaging than carbon dioxide. Archived from the original on 19 December 2008. Retrieved 2 January 2009.
  7. ^ "Methane from melting Siberian permafrost". Melting permafrost methane emissions: The other threat to climate change. TerraNature Trust. 15 September 2006. Archived from the original on 11 January 2009. Retrieved 2 January 2009.
  8. ^ ACIA (2005). Arctic Climate Impact Assessment - Scientific Report. Cambridge University Press. pp. 216–217. ISBN 978-0-521-86509-8.
  9. ^ Watts, Robert G. (1997). "Cryospheric processes". Engineering Response to Global Climate Change: Planning a Research and Development Agenda. CRC Press. p. 419. ISBN 978-1-56670-234-8.
  10. ^ Rena Marie Pacella (29 June 2007). "Duct Tape Methods to Save the Earth: Re-Ice the Arctic". Popular Science. Retrieved 4 March 2009.
  11. ^ "ASU team proposes restoring Arctic ice with 10 million windmills". Arizona State University. 22 December 2016.
  12. ^ S. Zhou; P. C. Flynn (2005). "Geoengineering Downwelling Ocean Currents: A Cost Assessment". Climatic Change. 71 (1–2): 203–220. doi:10.1007/s10584-005-5933-0.
  13. ^ a b Caldeira, K.; Wood, L. (13 November 2008). "Global and Arctic climate engineering: numerical model studies". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. The Royal Society. 366 (1882): 4039–4056. Bibcode:2008RSPTA.366.4039C. doi:10.1098/rsta.2008.0132. ISSN 1364-503X.
  14. ^ Schuttenhelm, Rolf (2008). "Diomede Crossroads - Saving the North Pole? Thoughts on plausibility". Archived from the original on 25 July 2011.
  15. ^ "Could a Massive Dam Between Alaska and Russia Save the Arctic?". Huffington Post. 27 November 2010. Retrieved 10 March 2011.
  • Steffen, Will; Sanderson, A.; Jäger, Jill; et al. (September 2005). Global Change and the Earth System: A Planet Under Pressure. Springer. p. 150. ISBN 978-3-540-26594-8.

Arctic geoengineering

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