Landscape impacts of 3D-seismic surveys in the Arctic National Wildlife Refuge, Alaska
Although three-dimensional (3D) seismic surveys have improved the success rate of exploratory drilling for oil and gas, the impacts have received little scientific scrutiny, despite affecting more area than any other oil and gas activity. To aid policy-makers and scientists, we reviewed studies of t...
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description | Although three-dimensional (3D) seismic surveys have improved the success rate of exploratory drilling for oil and gas, the impacts have received little scientific scrutiny, despite affecting more area than any other oil and gas activity. To aid policy-makers and scientists, we reviewed studies of the landscape impacts of 3D-seismic surveys in the Arctic. We analyzed a proposed 3D-seismic program in northeast Alaska, in the northern Arctic National Wildlife Refuge, which includes a grid 63,000 km of seismic trails and additional camp-move trails. Current regulations are not adequate to eliminate impacts from these activities. We address issues related to the high-density of 3D trails compared to 2D methods, with larger crews, more camps, and more vehicles. We focus on consequences to the hilly landscapes, including microtopography, snow, vegetation, hydrology, active layers, and permafrost. Based on studies of 2D-seismic trails created in 1984–1985 in the same area by similar types of vehicles, under similar regulations, approximately 122 km² would likely sustain direct medium- to high-level disturbance from the proposed exploration, with possibly expanded impacts through permafrost degradation and hydrological connectivity. Strong winds are common, and snow cover necessary to minimize impacts from vehicles is windblown and inadequate to protect much of the area. Studies of 2D-seismic impacts have shown that moist vegetation types, which dominate the area, sustain longer-lasting damage than wet or dry types, and that the heavy vehicles used for mobile camps caused the most damage. The permafrost is ice rich, which combined with the hilly topography, makes it especially susceptible to thermokarst and erosion triggered by winter vehicle traffic. The effects of climate warming will exacerbate the impacts of winter travel due to warmer permafrost and a shift of precipitation from snow to rain. The cumulative impacts of 3D-seismic traffic in tundra areas need to be better assessed, together with the effects of climate change and the industrial development that would likely follow. Current data needs include studies of the impacts of 3D-seismic exploration, better climate records for the Arctic National Wildlife Refuge, especially for wind and snow; and high-resolution maps of topography, ground ice, hydrology, and vegetation. |
doi_str_mv | 10.1002/eap.2143 |
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Torre ; Kanevskiy, Mikhail ; Liljedahl, Anna K. ; Nolan, Matthew ; Sturm, Matthew ; Walker, Donald A.</creator><creatorcontrib>Raynolds, Martha K. ; Jorgenson, Janet C. ; Jorgenson, M. Torre ; Kanevskiy, Mikhail ; Liljedahl, Anna K. ; Nolan, Matthew ; Sturm, Matthew ; Walker, Donald A.</creatorcontrib><description>Although three-dimensional (3D) seismic surveys have improved the success rate of exploratory drilling for oil and gas, the impacts have received little scientific scrutiny, despite affecting more area than any other oil and gas activity. To aid policy-makers and scientists, we reviewed studies of the landscape impacts of 3D-seismic surveys in the Arctic. We analyzed a proposed 3D-seismic program in northeast Alaska, in the northern Arctic National Wildlife Refuge, which includes a grid 63,000 km of seismic trails and additional camp-move trails. Current regulations are not adequate to eliminate impacts from these activities. We address issues related to the high-density of 3D trails compared to 2D methods, with larger crews, more camps, and more vehicles. We focus on consequences to the hilly landscapes, including microtopography, snow, vegetation, hydrology, active layers, and permafrost. Based on studies of 2D-seismic trails created in 1984–1985 in the same area by similar types of vehicles, under similar regulations, approximately 122 km² would likely sustain direct medium- to high-level disturbance from the proposed exploration, with possibly expanded impacts through permafrost degradation and hydrological connectivity. Strong winds are common, and snow cover necessary to minimize impacts from vehicles is windblown and inadequate to protect much of the area. Studies of 2D-seismic impacts have shown that moist vegetation types, which dominate the area, sustain longer-lasting damage than wet or dry types, and that the heavy vehicles used for mobile camps caused the most damage. The permafrost is ice rich, which combined with the hilly topography, makes it especially susceptible to thermokarst and erosion triggered by winter vehicle traffic. The effects of climate warming will exacerbate the impacts of winter travel due to warmer permafrost and a shift of precipitation from snow to rain. The cumulative impacts of 3D-seismic traffic in tundra areas need to be better assessed, together with the effects of climate change and the industrial development that would likely follow. Current data needs include studies of the impacts of 3D-seismic exploration, better climate records for the Arctic National Wildlife Refuge, especially for wind and snow; and high-resolution maps of topography, ground ice, hydrology, and vegetation.</description><identifier>ISSN: 1051-0761</identifier><identifier>EISSN: 1939-5582</identifier><identifier>DOI: 10.1002/eap.2143</identifier><identifier>PMID: 32335990</identifier><language>eng</language><publisher>United States: John Wiley and Sons, Inc</publisher><subject>1002 Area ; 3D seismic ; Alaska ; Arctic National Wildlife Refuge ; Arctic Regions ; Camps ; Climate change ; Climate effects ; cumulative impacts ; Drilling ; Earthquake damage ; Exploratory drilling ; Global warming ; Ground ice ; Heavy vehicles ; Hydrology ; ice‐rich permafrost ; Industrial development ; Landscape ; oil and gas exploration ; Permafrost ; Polar environments ; Rainfall ; Regulations ; Seismic exploration ; Seismic surveys ; Snow ; Snow cover ; Topography ; Traffic ; Trails ; Tundra ; Vegetation ; Vehicles ; Wildlife ; Wildlife conservation ; Wildlife refuges ; Wildlife sanctuaries ; Winter</subject><ispartof>Ecological applications, 2020-10, Vol.30 (7), p.1-20</ispartof><rights>2020 The Authors</rights><rights>2020 The Authors. published by Wiley Periodicals LLC on behalf of Ecological Society of America</rights><rights>2020 The Authors. Ecological Applications published by Wiley Periodicals LLC on behalf of Ecological Society of America.</rights><rights>Copyright Ecological Society of America Oct 2020</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4603-8ff264d95b8b644c468e2eec0f4643a2c9649767efd09cd55203f187543a98133</citedby><cites>FETCH-LOGICAL-c4603-8ff264d95b8b644c468e2eec0f4643a2c9649767efd09cd55203f187543a98133</cites><orcidid>0000-0001-9581-7811</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/27029112$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/27029112$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,315,781,785,804,886,1418,27925,27926,45575,45576,58018,58251</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32335990$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Raynolds, Martha K.</creatorcontrib><creatorcontrib>Jorgenson, Janet C.</creatorcontrib><creatorcontrib>Jorgenson, M. Torre</creatorcontrib><creatorcontrib>Kanevskiy, Mikhail</creatorcontrib><creatorcontrib>Liljedahl, Anna K.</creatorcontrib><creatorcontrib>Nolan, Matthew</creatorcontrib><creatorcontrib>Sturm, Matthew</creatorcontrib><creatorcontrib>Walker, Donald A.</creatorcontrib><title>Landscape impacts of 3D-seismic surveys in the Arctic National Wildlife Refuge, Alaska</title><title>Ecological applications</title><addtitle>Ecol Appl</addtitle><description>Although three-dimensional (3D) seismic surveys have improved the success rate of exploratory drilling for oil and gas, the impacts have received little scientific scrutiny, despite affecting more area than any other oil and gas activity. To aid policy-makers and scientists, we reviewed studies of the landscape impacts of 3D-seismic surveys in the Arctic. We analyzed a proposed 3D-seismic program in northeast Alaska, in the northern Arctic National Wildlife Refuge, which includes a grid 63,000 km of seismic trails and additional camp-move trails. Current regulations are not adequate to eliminate impacts from these activities. We address issues related to the high-density of 3D trails compared to 2D methods, with larger crews, more camps, and more vehicles. We focus on consequences to the hilly landscapes, including microtopography, snow, vegetation, hydrology, active layers, and permafrost. Based on studies of 2D-seismic trails created in 1984–1985 in the same area by similar types of vehicles, under similar regulations, approximately 122 km² would likely sustain direct medium- to high-level disturbance from the proposed exploration, with possibly expanded impacts through permafrost degradation and hydrological connectivity. Strong winds are common, and snow cover necessary to minimize impacts from vehicles is windblown and inadequate to protect much of the area. Studies of 2D-seismic impacts have shown that moist vegetation types, which dominate the area, sustain longer-lasting damage than wet or dry types, and that the heavy vehicles used for mobile camps caused the most damage. The permafrost is ice rich, which combined with the hilly topography, makes it especially susceptible to thermokarst and erosion triggered by winter vehicle traffic. The effects of climate warming will exacerbate the impacts of winter travel due to warmer permafrost and a shift of precipitation from snow to rain. The cumulative impacts of 3D-seismic traffic in tundra areas need to be better assessed, together with the effects of climate change and the industrial development that would likely follow. 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Torre</au><au>Kanevskiy, Mikhail</au><au>Liljedahl, Anna K.</au><au>Nolan, Matthew</au><au>Sturm, Matthew</au><au>Walker, Donald A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Landscape impacts of 3D-seismic surveys in the Arctic National Wildlife Refuge, Alaska</atitle><jtitle>Ecological applications</jtitle><addtitle>Ecol Appl</addtitle><date>2020-10</date><risdate>2020</risdate><volume>30</volume><issue>7</issue><spage>1</spage><epage>20</epage><pages>1-20</pages><issn>1051-0761</issn><eissn>1939-5582</eissn><abstract>Although three-dimensional (3D) seismic surveys have improved the success rate of exploratory drilling for oil and gas, the impacts have received little scientific scrutiny, despite affecting more area than any other oil and gas activity. To aid policy-makers and scientists, we reviewed studies of the landscape impacts of 3D-seismic surveys in the Arctic. We analyzed a proposed 3D-seismic program in northeast Alaska, in the northern Arctic National Wildlife Refuge, which includes a grid 63,000 km of seismic trails and additional camp-move trails. Current regulations are not adequate to eliminate impacts from these activities. We address issues related to the high-density of 3D trails compared to 2D methods, with larger crews, more camps, and more vehicles. We focus on consequences to the hilly landscapes, including microtopography, snow, vegetation, hydrology, active layers, and permafrost. Based on studies of 2D-seismic trails created in 1984–1985 in the same area by similar types of vehicles, under similar regulations, approximately 122 km² would likely sustain direct medium- to high-level disturbance from the proposed exploration, with possibly expanded impacts through permafrost degradation and hydrological connectivity. Strong winds are common, and snow cover necessary to minimize impacts from vehicles is windblown and inadequate to protect much of the area. Studies of 2D-seismic impacts have shown that moist vegetation types, which dominate the area, sustain longer-lasting damage than wet or dry types, and that the heavy vehicles used for mobile camps caused the most damage. The permafrost is ice rich, which combined with the hilly topography, makes it especially susceptible to thermokarst and erosion triggered by winter vehicle traffic. The effects of climate warming will exacerbate the impacts of winter travel due to warmer permafrost and a shift of precipitation from snow to rain. The cumulative impacts of 3D-seismic traffic in tundra areas need to be better assessed, together with the effects of climate change and the industrial development that would likely follow. Current data needs include studies of the impacts of 3D-seismic exploration, better climate records for the Arctic National Wildlife Refuge, especially for wind and snow; and high-resolution maps of topography, ground ice, hydrology, and vegetation.</abstract><cop>United States</cop><pub>John Wiley and Sons, Inc</pub><pmid>32335990</pmid><doi>10.1002/eap.2143</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0001-9581-7811</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | 1002 Area 3D seismic Alaska Arctic National Wildlife Refuge Arctic Regions Camps Climate change Climate effects cumulative impacts Drilling Earthquake damage Exploratory drilling Global warming Ground ice Heavy vehicles Hydrology ice‐rich permafrost Industrial development Landscape oil and gas exploration Permafrost Polar environments Rainfall Regulations Seismic exploration Seismic surveys Snow Snow cover Topography Traffic Trails Tundra Vegetation Vehicles Wildlife Wildlife conservation Wildlife refuges Wildlife sanctuaries Winter |
title | Landscape impacts of 3D-seismic surveys in the Arctic National Wildlife Refuge, Alaska |
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