Marine Geology

Multi-Year Sea Ice Thins in the Arctic

Professor David Barber of the University of Manitoba Center for Earth Observation Science recently spoke at the International Polar Year conference in Oslo. An excerpt from his talk refers to the sea ice cover satellite data produced by the National Snow and Ice Data Center, which describes areal extent only:

“Scientists spend a lot of energy discussing the ‘squiggly line’ generated by satellite data on sea ice extent,” Dr. Barber told the audience, showing a graph from the National Snow and Ice Data Center. “But extent alone does not reflect the real condition of the sea ice. I think we are all looking forward to getting reliable data on thickness from CryoSat. Because what really matters is the condition and thickness of the multiyear ice.”

“We are losing 70 000 square kilometres of sea ice (the size of Lake Superior) every year. That adds up to 2.5 million square kilometres over the last 30 years. The reality is even worse,” continued Dr Barber. “Even though the extent of the sea ice – both the winter maximum and the summer minimum – increased in 2008 and 2009, the amount of multiyear ice continued to decline rapidly.”

Barber’s observations came from over-wintering in the Arctic aboard a research ice-breaker. Expecting to be stopped by thick multi-year ice up to 12-meters thick, the icebreaker cut through ice only a couple inches thick at 13-knots.

The entire talk is available here.

Wetland Scientists Wade into Deepwater Horizon Disaster

Wetland Scintists call for inspection of all offshore oil operations, moratorium on new drilling and extraction.

In response to the Deepwater Horizon disaster, the following is a statement released by the Society of Wetland Scientists.

Statement from the Environmental Concerns Committee
Society of Wetland Scientists
Dennis F. Whigham, Chair
Stephen W. Broome
Curtis J. Richardson
Robert L. Simpson
Loren M. Smith
May 18, 2010

Coastal wetlands are essential components of healthy and productive coastal fisheries, and nowhere within the lower 48 states has the critical linkage between wetlands and fisheries resources been more clearly demonstrated than in the Gulf Mexico (e.g., Chesney et al. 2000, Crain et al. 1979). Louisiana alone, for example, generates 30% of the nation’s seafood production (Day et. al., 2005) and accounts for 40% of the total wetlands in the conterminous United States (Richardson and Pahl 2006). The ongoing loss of wetland resources in the Gulf of Mexico and the potential economic and environmental costs, especially in Louisiana and Florida, is an issue of international concern. The impacts of the current oil spill are unknown but the potential for direct and indirect environmental damage to coastal ecosystem services are extraordinary. Both the oil and the activities used in the cleanup have the potential to adversely affect wetland flora and fauna.

Thus far, most of the oil has remained offshore but reports of oil reaching the coast have been geographically extensive ranging from Florida to Louisiana. The potential geographic extent of the spill could result in the exposure of many types of coastal wetlands to oil, ranging from mangroves in Florida, Texas, Mexico and islands in the Caribbean basin to tidal freshwater wetlands along the Gulf Coast.

Most wetlands that will potentially be exposed to oil are saline and brackish tidal wetlands, which are nursery grounds for economically important coastal fish and shellfish. Seagrass beds are also at risk.
Experimental and monitoring studies around the world have found that oil commonly has a negative impact on emergent wetlands and the biota that reside in them (e.g., Lin et al. 2002). However, the degrees of impacts are variable and complex (Pezeshki et al. 2000), depending on the species composition of the wetland vegetation (e.g., Lin and Mendelssohn 1996), the amount and characteristics of the oil, the extent of weathering, and the geographic location of the wetland. Tropical and subtropical mangroves seem especially vulnerable to oil spills (e.g., Garrity and Levings 1993, Proffittt et al. 1995), as was demonstrated along the Persian Gulf following the Gulf War and in Panama following a major spill in 1986. Coastal wetlands in the Gulf of Mexico are also sensitive to oil as are species-rich tidal freshwater wetlands, although long term impacts span the gamut from rapid recovery within a growing season to delayed recovery for several years (Hester and Mendelssohn 2000).

In addition to direct impacts on emergent plants, oil that reaches wetlands also impacts animals that utilize the wetlands, especially benthic organisms that reside in the substrate.

Studies of impacted wetlands have demonstrated that wetlands can recover from the impacts of oil spills but the recovery process varies from extremely slow in mangroves swamps (e.g., Burns et al. 1993, 1994) to relatively rapid in grass-dominated marshes (Pahl et al. 2003). The recovery of coastal wetlands from the current oil spill will be further complicated due to current stress on wetland plant productivity from the ongoing 1 cm yr-1 relative sea level rise (Stumpf and Haines 1998) and land subsidence due to natural and human-related factors within the Louisiana coastal zone (Richardson and Pahl 2006).

The current oil spill in the Gulf of Mexico has also focused discussion on where offshore drilling should be allowed. The disaster at the Deepwater Horizon platform demonstrates that the placement of oil wells in deep offshore waters has the potential to have far-reaching geographic impact. The disaster has also demonstrated that current technologies are not adequate to assure that an accident of this magnitude in deep ocean areas can be effectively managed without enormous economic and environmental costs.

While the short- and long-term impacts of the current oil spill on ecosystem services unfold, the Society of Wetlands Scientists supports (1) the immediate inspection of all offshore oil facilities and remediation, if required, to ensure that an accident of this type does not happen again and (2) a moratorium on all new deep-water oil exploration and extraction until further technological advances are available and tested to assure that the impacts of accidents of this sort can be managed efficiently to assure minimal negative impacts to coastal resources.

References
Burns, K.A., S.D. Garrity, and S.C. Levings. 1993. How many years until mangrove ecosystems recover from catastrophic oil spills? Marine Pollution Bulletin 26: 239-248.
Burns, K.A., S.D. Garrity, D. Jorissen, J. MacPherson, M. Stoelting, J. Tierney, and L. Yelle-Simmons. 1994. The Galeta Oil Spill. II. Unexpected persistence of oil trapped in mangrove sediments. Estuarine, Coastal and Shelf Science 38: 349-364.
Chesney, E.J., D.M. Baltz, and R. G. Thomas. 2000. Louisiana estuarine and coastal fisheries and habitats: perspectives from a fishse eye view. Ecological Applications 10: 350-366.
Craig, N.J. R.E. Turner, and J.W. Day Jr. 1979. Land loss in coastal Louisiana (U.S.A.) Environmental Management 3: 133-144.
Day, J.W., Jr., J. Barras, E. Clairain, J. Johnston, D. Justic, G.P. Kemp, J. Ko, R. Lane, W.J. Mitsch, G. Steyer, P. Templet, and A. Yañez-Arancibia. 2005. Implications of global climatic change and energy cost and availability for the restoration of the Mississippi delta. Ecological Engineering 24: 253-265.
Garrity, S.D. and S.C. Levings. 1993. Effecs of an oil spill on some organisms living on mangrove (Rhizophora mangle L.) roots in Caribbean Panama. Marine Environmental Research 35: 251-271.
Hester, M. W. and I. A. Mendelssohn. 2000. Long-term recovery of a Louisiana brackish marsh plant community from oil-spill impact: vegetation response and mitigating effects of marsh surface elevation. Marine Environmental Research 49:233-254.
Lin, Q. and I.A. Mendelssohn, 1996. A comparative investigation of the effects of South Louisiana crude oil on the vegetation of fresh, brackish, and salt marshes. Marine Pollution Bulletin 32: 202-209.
Lin, Q., I.A. Mendelssohn, M.T. Suidan, K. Lee, and A.D. Venosa. 2002. The dose-response relationship between No. 2 fuel oil and the growth of the salt marsh grass, Spartina alterniflora. Marine Pollution Bulletin 44. 897-902.
Pahl, J. W., I. A. Mendelssohn, C. B. Henry, and T. J. Hess. 2003. Recovery trajectories after in-situ burning of an oiled wetland in coastal Louisiana, USA. Environmental Management 31:236-251.
Pezeshki, S.R., M.W. Hester, Q. Lin, and J.A. Nyman. 2000. The effects of oil spill and clean-up on dominant US Gulf coast marsh macrophytes: a review. Environmental Pollution 108: 129-139.
Proffitt, C.E., D.J. Devlin, and M. Lindsey. 1995. Effects of oil on mangrove seedlings grown under different environmental conditions. Marine Pollution Bulletin 30: 788-793.
Richardson, C. J. and J. W. Pahl. 2006. Katrina consequences assessment and projection Report. Chapter 23, in FEMA Report on Impacts of Hurricane Katrina. February 2006. Washington, D. C.
Stumpf, R. P. and J. W. Haines. 1998. Variations in tidal level in the Gulf of Mexico and implications for tidal wetlands. Estuarine, Coastal, and Shelf Science 46:165–173.
Society of Wetland Scientists Mission
The mission of the Society of Wetland Scientists is to promote understanding, scientifically based management, and sustainable use of wetlands. The current oil spill in the Gulf of Mexico has the potential to impact coastal wetlands and cause enormous short- and long-term damage to ecosystem services they provide. The potential short- and long-term economic costs are therefore massive and unprecedented.

Coast of Alaska: Accelerated Erosion 2002-2007

Alaskan coastal erosion (USGS).

Alaskan coastal erosion (USGS).

A five-year study in Alaska led by the U.S. Geological Survey (USGS) found that shoreline erosion along a 40-mile stretch of the Beaufort Sea has been accelerating from about 20-feet per year fifty years ago, to 45-feet per year by 2007. The research makes obvious the importance of considering the specific properties of the earthen materials exposed to erosive forces. In this case, the land contains permafrost, a consituent of the soil order called Gelisol.

An excerpt:

The authors proposed that these recent shifts in the rate and pattern of land loss along this coastline segment are potentially a result of changing arctic conditions, including declining sea ice extent, increasing summertime sea-surface temperature, rising sea level, and increases in storm power and corresponding wave action.

“Taken together, these factors may be leading to a new era in ocean-land interactions that seem to be repositioning and reshaping the Arctic coastline,” wrote (Benjamin) Jones and his colleagues. “And any increases in the current rates of coastal retreat will have further ramifications on Arctic landscapes – including losses in freshwater and terrestrial wildlife habitats, and in disappearing cultural sites, as well as adversely impacting coastal villages and towns. In addition, oil test wells are threatened.”

Alaskan permafrost erosion (USGS)

Alaskan permafrost erosion (USGS)

For most of us who live on the relative “terra firma” of the mid-latitude continents, global warming may seem like a fairly benign process, one that might result in better weather to play golf. The Arctic and Antarctic environments, by contrast, are very different, very fragile worlds. The authors are careful with their words, using the standard qualifiers, but it’s pretty clear they think climate change is a factor as the waves pound that coast.

Research Paper:
Jones, B.M., Arp, C.D., Jorgenson, M.T., Hinkel, K.M., Schmutz, J.A., and Flint, P.L. Increase in the rate and uniformity of coastline erosion in arctic Alaska. Geophysical Research Letters, February 14, 2009. http://www.agu.org/journals/gl/gl0903/2008GL036205/.

Photos source: USGS

Methane Venting From East Siberian Arctic Shelf

As a greenhouse gas, methane is 30 times more potent than carbon dioxide.

According to University of Alaska Arctic researchers Natalia Shakhova and Igor Semiletov, methane gas is venting from the East Siberian Arctic Shelf (ESAS) at a surprisingly high rate. The vents are coming through leaks in permafrost, which forms a cap over methane stored in deeper sediments.

While permafrost is generally viewed as a terrestrial soil, it actually extends offshore beneath a broad area of shallow marine sediments. This area of marine permafrost, about 2 million square kilometers, is the most unstable in the Arctic after several years of warming temperatures.

In the video Shakhova indicates the rate of methane venting at the ESAS equals the methane emitted currently by the rest of the global ocean.

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