Safeguarding Important Areas in the U.S. Arctic Ocean
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Beaufort Sea Monitoring Program
Outer Continental Shelf Environmental Assessment Program Beaufort Sea Monitoring Program: Proceedings of a Workshop and Sampling Design Recommendations Beaufort Sea Monitoring Program: Proceedings of a Workshop (September 1983) and Sampling Design Recommendations ; Prepared for the Outer Continental Shelf Environmental Assessment Program Juneau, Alaska by J. P. Houghton Dames & Moore 155 N.E. lOOth Street Seattle, WA 98125 with D. A Segar J. E. Zeh SEAM Ocean Inc. Department of Statistics Po. Box 1627 University of Washington Wheaton, MD 20902 Seattle, WA 98195 April 1984 UNITED STATES UNITED STATES DEPARTMENT OF COMMERCE DEPARTMENT OF THE INTERIOR Malcolm Baldridge, Secretary William P Clark, Secretary NATIONAL OCEANIC AND MINERALS MANAGEMENT SERVICE ATMOSPHERIC ADMINISTRATION William D. Bettenberg, Director John V. Byrne, Administrator r. NOTICES i? I This report has been reviewed by the US. Department of Commerce, National Oceanic and Atmospheric Administration's Outer Continental Shelf Environmental Assessment Program office, and approved for publication. The interpretation of data and opinions expressed in this document are those of the authors and workshop participants. Approval does not necessarily signify that the contents reflect the views and policies of the Department of Commerce or those of the Department of the Interior. The National Oceanic and Atmospheric Administration (NOAA) does not approve, recommend, or endorse any proprietary product or proprietary material mentioned in this publica tion. No reference shall be made to NOAA or to this publication in any advertising or sales promotion which would indicate or imply that NOAA approves, recommends, or endorses any proprietary'product or proprietary material mentioned herein, or which has as its purpose an intent to cause directly or indirectly the advertised product to be used or purchas'ed because of this publication. -
Boreogadus Saida) and Safron Cod (Eleginus Gracilis) Early Life Stages in the Pacifc Arctic
Polar Biology https://doi.org/10.1007/s00300-019-02494-4 ORIGINAL PAPER Spatio‑temporal distribution of polar cod (Boreogadus saida) and safron cod (Eleginus gracilis) early life stages in the Pacifc Arctic Cathleen D. Vestfals1 · Franz J. Mueter2 · Janet T. Dufy‑Anderson3 · Morgan S. Busby3 · Alex De Robertis3 Received: 24 September 2018 / Revised: 15 March 2019 / Accepted: 18 March 2019 © Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract Polar cod (Boreogadus saida) and safron cod (Eleginus gracilis) are key fshes in the Arctic marine ecosystem, serving as important trophic links between plankton and apex predators, yet our understanding of their life histories in Alaska’s Arctic is extremely limited. To improve our knowledge about their early life stages (ELS), we described the spatial and temporal distributions of prefexion larvae to late juveniles (to 65 mm in length) in the Chukchi and western Beaufort seas based on surveys conducted between 2004 and 2013, and examined how their abundances varied in response to environmental factors. Species-specifc diferences in habitat use were found, with polar cod having a more ofshore and northern distribution than safron cod, which were found closer inshore and farther south. Polar cod prefexion and fexion larvae were encountered throughout the sampling season across much of the shelf, which suggests that spawning occurs over several months and at multiple locations, with Barrow Canyon potentially serving as an important spawning and/or retention area. Polar cod ELS were abundant at intermediate temperatures (5.0–6.0 °C), while safron cod were most abundant at the highest temperatures, which suggests that safron cod may beneft from a warming Arctic, while polar cod may be adversely afected. -
2021 Alaska Studies Plan
U.S. Department of the Interior Bureau of Ocean Energy Management Alaska Outer Connental Shelf Region Anchorage, Alaska November 2020 Prepared by U.S. Department of the Interior Bureau of Ocean Energy Management Anchorage, Alaska Office 3801 Centerpoint Drive, Suite 500 Anchorage, Alaska 99503-5823 November 2020 The Environmental Studies Program has chosen to “go green.” This document can be accessed in electronic format at http://www.boem.gov/akstudies/. For assistance accessing the document or for further information about the Studies Program and our planning process, please contact [email protected] or Dr. Heather Crowley at [email protected]. The inclusion of study profiles in this document does not constitute a commitment by the U.S. Department of the Interior, Bureau of Ocean Energy Management to conduct or fund any or all of the studies. Method of procurement may be selected at the discretion of BOEM. The scope of the studies is subject to change prior to initiation of any work. Any use of trade names is for descriptive purposes only and does not constitute endorsement of these products by the Bureau of Ocean Energy Management. Cover Image: Sea urchins in the intertidal zone, Cook Inlet, Alaska. Photo credit: “ShoreZone Imaging and Mapping along the Alaska Peninsula” project team; OCS Study BOEM 2018-037. United States Department of the Interior BUREAU OF OCEAN ENERGY MANAGEMENT Alaska Regional Office 3801 Centerpoint Drive, Suite 500 Anchorage, Alaska 99503-5823 November 2, 2020 Dear Stakeholder: Thank you for your interest in the Environmental Studies Program (ESP) of the Bureau of Ocean Energy Management (BOEM). -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Archaeology Resources
Archaeology Resources Page Intentionally Left Blank Archaeological Resources Background Archaeological Resources are defined as “any prehistoric or historic district, site, building, structure, or object [including shipwrecks]…Such term includes artifacts, records, and remains which are related to such a district, site, building, structure, or object” (National Historic Preservation Act, Sec. 301 (5) as amended, 16 USC 470w(5)). Archaeological resources are either historic or prehistoric and generally include properties that are 50 years old or older and are any of the following: • Associated with events that have made a significant contribution to the broad patterns of our history • Associated with the lives of persons significant in the past • Embody the distinctive characteristics of a type, period, or method of construction • Represent the work of a master • Possess high artistic values • Present a significant and distinguishable entity whose components may lack individual distinction • Have yielded, or may be likely to yield, information important in history These resources represent the material culture of past generations of a region’s prehistoric and historic inhabitants, and are basic to our understanding of the knowledge, beliefs, art, customs, property systems, and other aspects of the nonmaterial culture. Further, they are subject to National Historic Preservation Act (NHPA) review if they are historic properties, meaning those that are on, or eligible for placement on, the National Register of Historic Places (NRHP). These sites are referred to as historic properties. Section 106 requires agencies to make a reasonable and good faith efforts to identify historic properties. Archaeological resources may be found in the Proposed Project Area both offshore and onshore. -
Flow of Pacific Water in the Western Chukchi
Deep-Sea Research I 105 (2015) 53–73 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Flow of pacific water in the western Chukchi Sea: Results from the 2009 RUSALCA expedition Maria N. Pisareva a,n, Robert S. Pickart b, M.A. Spall b, C. Nobre b, D.J. Torres b, G.W.K. Moore c, Terry E. Whitledge d a P.P. Shirshov Institute of Oceanology, 36, Nakhimovski Prospect, Moscow 117997, Russia b Woods Hole Oceanographic Institution, 266 Woods Hole Road, Woods Hole, MA 02543, USA c Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario M5S 1A7, Canada d University of Alaska Fairbanks, 505 South Chandalar Drive, Fairbanks, AK 99775, USA article info abstract Article history: The distribution of water masses and their circulation on the western Chukchi Sea shelf are investigated Received 10 March 2015 using shipboard data from the 2009 Russian-American Long Term Census of the Arctic (RUSALCA) pro- Received in revised form gram. Eleven hydrographic/velocity transects were occupied during September of that year, including a 25 August 2015 number of sections in the vicinity of Wrangel Island and Herald canyon, an area with historically few Accepted 25 August 2015 measurements. We focus on four water masses: Alaskan coastal water (ACW), summer Bering Sea water Available online 31 August 2015 (BSW), Siberian coastal water (SCW), and remnant Pacific winter water (RWW). In some respects the Keywords: spatial distributions of these water masses were similar to the patterns found in the historical World Arctic Ocean Ocean Database, but there were significant differences. -
Beaufort Sea
160°W 159°W 158°W 157°W 156°W 155°W 154°W 153°W 152°W 151°W 150°W 149°W 148°W 147°W 146°W 145°W 144°W 143°W 142°W 141°W 140°W Beaufort Sea !Barrow N ° N 1 ° 14 7 1 7 15 13 12 !Wainwright 16 11 Prudhoe 17 Bay 10 Camden N 9 ° N Bay Kaktovik 0 ° 8 7 !Kaktovik Nuiqsut 7 0 ! 7 6 5 4 3 2 1 N ational P e C troleum Reserv e - Alaska a U n a . S d . a N - ° N - 9 ° A 6 9 s s Y 6 n e d e r l W i l a u s k k o a Index Map 1 of 3 n U.S./Canada Border to Wainwright ife Refuge Final Designation ic National Wildl of Critical Barrier Islands and Arct Denning Habitat Maps N ° N 8 ° 6 8 6 0 10 20 30 40 50 60 70 80 90 100 miles 0 10 20 30 40 50 60 70 80 90 100 km Map N ° N 7 ° Area 6 7 Pacific Ocean 6 158°W 157°W 156°W 155°W 154°W 153°W 152°W 151°W 150°W 149°W 148°W 147°W 146°W 145°W 144°W 143°W 142°W 99-0136 142°20'W 142°10'W 142°W 141°50'W 141°40'W 141°30'W 141°20'W 141°10'W 141°W Beaufort Sea N N ' ' 0 0 5 5 ° ° 9 9 6 6 r e v i R k a sr ak Eg N N ' ' 0 0 4 r Demarcation 4 ° ° 9 e 9 6 v 6 i Bay R t u k a g n o K N N ' ' 0 0 3 3 ° ° 9 9 6 6 C U a n . -
Natural Variability of the Arctic Ocean Sea Ice During the Present Interglacial
Natural variability of the Arctic Ocean sea ice during the present interglacial Anne de Vernala,1, Claude Hillaire-Marcela, Cynthia Le Duca, Philippe Robergea, Camille Bricea, Jens Matthiessenb, Robert F. Spielhagenc, and Ruediger Steinb,d aGeotop-Université du Québec à Montréal, Montréal, QC H3C 3P8, Canada; bGeosciences/Marine Geology, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany; cOcean Circulation and Climate Dynamics Division, GEOMAR Helmholtz Centre for Ocean Research, 24148 Kiel, Germany; and dMARUM Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, 28334 Bremen, Germany Edited by Thomas M. Cronin, U.S. Geological Survey, Reston, VA, and accepted by Editorial Board Member Jean Jouzel August 26, 2020 (received for review May 6, 2020) The impact of the ongoing anthropogenic warming on the Arctic such an extrapolation. Moreover, the past 1,400 y only encom- Ocean sea ice is ascertained and closely monitored. However, its pass a small fraction of the climate variations that occurred long-term fate remains an open question as its natural variability during the Cenozoic (7, 8), even during the present interglacial, on centennial to millennial timescales is not well documented. i.e., the Holocene (9), which began ∼11,700 y ago. To assess Here, we use marine sedimentary records to reconstruct Arctic Arctic sea-ice instabilities further back in time, the analyses of sea-ice fluctuations. Cores collected along the Lomonosov Ridge sedimentary archives is required but represents a challenge (10, that extends across the Arctic Ocean from northern Greenland to 11). Suitable sedimentary sequences with a reliable chronology the Laptev Sea were radiocarbon dated and analyzed for their and biogenic content allowing oceanographical reconstructions micropaleontological and palynological contents, both bearing in- can be recovered from Arctic Ocean shelves, but they rarely formation on the past sea-ice cover. -
Chukchi Sea Itrs 2013
Biological Opinion for Polar Bears (Ursus maritimus) and Conference Opinion for Pacific Walrus (Odobenus rosmarus divergens) on the Chukchi Sea Incidental Take Regulations Prepared by: U.S. Fish and Wildlife Service Fairbanks Fish and Wildlife Field Office 110 12th Ave, Room 110 Fairbanks, Alaska 99701 May 20, 2013 1 Table of Contents Introduction ................................................................................................................................5 Background on Section 101(a)(5) of MMPA ...........................................................................6 The AOGA Petition .................................................................................................................6 History of Chukchi Sea ITRS ..............................................................................................7 Relationship of ESA to MMPA ...........................................................................................7 MMPA Terms: ........................................................................................................................7 ESA Terms: ............................................................................................................................8 The Proposed Action ...................................................................................................................8 Information Required to Obtain a Letter of Authorization .......................................................9 Specific Measures of LOAs .................................................................................................. -
Beaufort Seas Coastal and Ocean Zones Strategic
166° 164° 162° 160° 158° 156° 154° 152° 150° 148° 146° 144° 142° 140° 138° LEGEND North Slope Planning Area Conservation System Unit (Offset for display) Barrow B Trans-Alaska Pipeline ea !. eau hi S fort kc Se 1 Chuc a Subsistence Resource Use (Top Frame) Caribou C h i Wainwright er p Non Salmon Fish Species !. Riv p 70° e R Mead r i Topagoruk River e v v e i r R k u Teshekpuk Lake p Moose ik p !. k Atqasuk I Kaktovik !. Seals and Sea Lions 70° !. Nuiqsut !. Prudhoe Bay 1 r Subsistence Resource Use (Bottom Frame) e iv R k u Brown Bear r a p Point Lay !. Sagavanirktok River u K r e Birds and Eggs v i R g n i n n a C Whales NOTES er iv 1(Bering, Chukchi, and Beaufort Seas Coastal and Ocean Zones Strategic e R ll A lvi Assessment: Data Atlas, National Oceanic and Atmospheric Administration, Co n a November 1988) k It t k u il v l ik u k R R i v i e v r e r 68° er iv R r le d n a h Arctic Village C !. 68° 164° 162° 160° 158° 156° 154° 152° 150° 148° 146° 144° 142° 140° 166° 164° 162° 160° 158° 156° 154° 152° 150° 148° 146° 144° 142° 140° 138° Barrow .! Be Sea au DISCLAIMER hi for This atlas is a graphical representation of digital data from multiple sources. Not ckc t Sea all features indicated on this map have been constructed or physically located. -
1 POLAR BEAR (Ursus Maritimus): Chukchi/Bering Seas Stock STOCK
Revised: 01/01/2010 POLAR BEAR (Ursus maritimus): Chukchi/Bering Seas Stock STOCK DEFINITION AND GEOGRAPHIC RANGE Polar bears are circumpolar in their distribution in the northern hemisphere. They occur in several largely discrete stocks or populations (Harington 1968). Polar bear movements are extensive and individual activity areas are enormous (Garner et al. 1990, Amstrup et al. 2000). The parameters used by Dizon et al. (1992) to classify stocks based on the phylogeographic approach were considered in the determination of stock separation in Alaska. Several polar bear stocks are known to be shared between countries (Amstrup et al. 1986, Amstrup and DeMaster 1988). Lentfer hypothesized that in Alaska two stocks exist, the Southern Beaufort Sea (SBS) and the Chukchi/Bering seas (CBS), based upon: (a) variations in levels of heavy metal contaminants of organ tissues (Lentfer 1976, Figure 1. Map of the Southern Beaufort Sea and the Chukchi/ Lentfer and Galster 1987); (b) morphological Bering seas polar bear stocks. characteristics (Manning 1971, Lentfer 1974, Wilson 1976); (c) physical oceanographic features which segregate the Chukchi Sea and Bering Sea stock from the Beaufort Sea stock (Lentfer 1974); and (d) movement information collected from mark and recapture studies of adult female bears (Lentfer 1974, 1983) (Figure 1). Information on contaminants (Woshner et al. 2001, Evans 2004a, Evans 2004b, Kannan et al. 2005, Smithwick et al. 2005, Verreault et al. 2005, Muir et al. 2006, Smithwick et al. 2006, Kannan et al. 2007, Rush et al. 2008) and movement data using satellite collars (Amstrup et al. 2004, Amstrup et al. 2005) continue to support the presence of these two stocks. -
12 Northern Bering-Chukchi Sea
12/18:&LME&FACTSHEET&SERIES& NORTHERN BERING- CHUKCHI SEA LME tic LMEs Arc NORTHERN'BERING+CHUKCHI'SEA'LME'MAP 18 of Map Russia Bering Strait Alaska Russia LME Canada Iceland Central Arctic Ocean 12 "1 ARCTIC LMEs Large&! Marine& Ecosystems& (LMEs)& are& defined& as& regions& of& work&of&the&ArcMc&Council&in&developing&and&promoMng&the& ocean& space& of& 200,000& km²& or& greater,& that& encompass& Ecosystem& ApproacH& to& management& of& the& ArcMc& marine& coastal& areas& from& river& basins& and& estuaries& to& the& outer& environment.& margins& of& a& conMnental& sHelf& or& the& seaward& extent& of& a& predominant&coastal¤t.&LMEs&are&defined&by&ecological& Joint'EA'Expert'group' criteria,&including&bathymetry,&HydrograpHy,&producMvity,&and& PAME& establisHed& an& Ecosystem& ApproacH& to& Management& tropically& linked& populaMons.& PAME& developed& a& map& expert& group& in& 2011& with& the& parMcipaMon& of& other& ArcMc& delineaMng&17&ArcMc&Large&Marine&Ecosystems&(ArcMc&LME's)& Council&working&groups&(AMAP,&CAFF&and&SDWG).&THis&joint& in&the&marine&waters&of&the&ArcMc&and&adjacent&seas&in&2006.& Ecosystem&ApproacH&Expert&Group&(EAYEG)&Has&developed&a& In&a&consultaMve&process&including&agencies&of&ArcMc&Council& framework& for& EA& implementaMon& wHere& the& first& step& is& member&states&and&other&ArcMc&Council&working&groups,&the& idenMficaMon& of& the& ecosystem& to& be& managed.& IdenMfying& ArcMc& LME& map& was& revised& in& 2012&to&include&18&ArcMc& the&ArcMc&LMEs&represents&this&first&step. LMEs.& THis& is& the& current&