Wildlife Action Plan Section IIIB: Alaska's 32 Ecoregions
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Aquatic Behaviour of Polar Bears (Ursus Maritimus) in an Increasingly Ice-Free Arctic Received: 8 December 2017 Karen Lone 1, Kit M
www.nature.com/scientificreports OPEN Aquatic behaviour of polar bears (Ursus maritimus) in an increasingly ice-free Arctic Received: 8 December 2017 Karen Lone 1, Kit M. Kovacs1, Christian Lydersen1, Mike Fedak 2, Magnus Andersen1, Accepted: 13 June 2018 Philip Lovell2 & Jon Aars1 Published: xx xx xxxx Polar bears are ice-associated marine mammals that are known to swim and dive, yet their aquatic behaviour is poorly documented. Reductions in Arctic sea ice are clearly a major threat to this species, but understanding polar bears’ potential behavioural plasticity with respect to the ongoing changes requires knowledge of their swimming and diving skills. This study quantifed time spent in water by adult female polar bears (n = 57) via deployment of various instruments bearing saltwater switches, and in some case pressure sensors (79 deployments, 64.8 bear-years of data). There were marked seasonal patterns in aquatic behaviour, with more time spent in the water during summer, when 75% of the polar bears swam daily (May-July). Females with cubs-of-the-year spent less time in the water than other females from den emergence (April) until mid-summer, consistent with small cubs being vulnerable to hypothermia and drowning. Some bears undertook notable long-distance-swims. Dive depths up to 13.9 m were recorded, with dives ≥5 m being common. The considerable swimming and diving capacities of polar bears might provide them with tools to exploit aquatic environments previously not utilized. This is likely to be increasingly important to the species’ survival in an Arctic with little or no persistent sea ice. -
Great Lakes Pine Barrens
Rapid Assessment Reference Condition Model The Rapid Assessment is a component of the LANDFIRE project. Reference condition models for the Rapid Assessment were created through a series of expert workshops and a peer-review process in 2004 and 2005. For more information, please visit www.landfire.gov. Please direct questions to [email protected]. Potential Natural Vegetation Group (PNVG) R6JAPIop Great Lakes Pine Barrens General Information Contributors (additional contributors may be listed under "Model Evolution and Comments") Modelers Reviewers Joshua Cohen [email protected] Vegetation Type General Model Sources Rapid AssessmentModel Zones Woodland Literature California Pacific Northwest Local Data Great Basin South Central Dominant Species* Expert Estimate Great Lakes Southeast Northeast S. Appalachians PIBA2 VAAN LANDFIRE Mapping Zones ANGE Northern Plains Southwest CAPE6 51 40 PIRE N-Cent.Rockies QUEL 50 SCSC 41 Geographic Range System occurs in northern Lower Michigan, northern Wisconsin, northern Minnesota, and eastern Ontario, north of the climatic tension zone (Curtis 1959 and is concentrated in the High Plains Subsection in northern Lower Michigan and in central Wisconsin (Vora 1993). Also occurs in several locations in the Upper Peninsula of Michigan and is associated with the upper Mississippi and St. Croix Rivers in Minnesota and Wisconsin (Comer 1996). Biophysical Site Description The Great Lakes pine barrens system is endemic to very dry, nutrient-impoverished landscape ecosystems. These ecosystems occur in landforms deposited by high-energy glacial melt waters, principally outwash plains and glacial lakebeds, underlain by well-sorted, coarse-textured sandy soils with low water retaining capacity. They also occur in bedrock-controlled landforms with shallow soils of limited moisture storage capacity (Cleland et al. -
The Exchange of Water Between Prince William Sound and the Gulf of Alaska Recommended
The exchange of water between Prince William Sound and the Gulf of Alaska Item Type Thesis Authors Schmidt, George Michael Download date 27/09/2021 18:58:15 Link to Item http://hdl.handle.net/11122/5284 THE EXCHANGE OF WATER BETWEEN PRINCE WILLIAM SOUND AND THE GULF OF ALASKA RECOMMENDED: THE EXCHANGE OF WATER BETWEEN PRIMCE WILLIAM SOUND AND THE GULF OF ALASKA A THESIS Presented to the Faculty of the University of Alaska in partial fulfillment of the Requirements for the Degree of MASTER OF SCIENCE by George Michael Schmidt III, B.E.S. Fairbanks, Alaska May 197 7 ABSTRACT Prince William Sound is a complex fjord-type estuarine system bordering the northern Gulf of Alaska. This study is an analysis of exchange between Prince William Sound and the Gulf of Alaska. Warm, high salinity deep water appears outside the Sound during summer and early autumn. Exchange between this ocean water and fjord water is a combination of deep and intermediate advective intrusions plus deep diffusive mixing. Intermediate exchange appears to be an annual phen omenon occurring throughout the summer. During this season, medium scale parcels of ocean water centered on temperature and NO maxima appear in the intermediate depth fjord water. Deep advective exchange also occurs as a regular annual event through the late summer and early autumn. Deep diffusive exchange probably occurs throughout the year, being more evident during the winter in the absence of advective intrusions. ACKNOWLEDGMENTS Appreciation is extended to Dr. T. C. Royer, Dr. J. M. Colonell, Dr. R. T. Cooney, Dr. R. -
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. -
Bathymetry and Geomorphology of Shelikof Strait and the Western Gulf of Alaska
geosciences Article Bathymetry and Geomorphology of Shelikof Strait and the Western Gulf of Alaska Mark Zimmermann 1,* , Megan M. Prescott 2 and Peter J. Haeussler 3 1 National Marine Fisheries Service, Alaska Fisheries Science Center, National Oceanic and Atmospheric Administration (NOAA), Seattle, WA 98115, USA 2 Lynker Technologies, Under contract to Alaska Fisheries Science Center, Seattle, WA 98115, USA; [email protected] 3 U.S. Geological Survey, 4210 University Dr., Anchorage, AK 99058, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-206-526-4119 Received: 22 May 2019; Accepted: 19 September 2019; Published: 21 September 2019 Abstract: We defined the bathymetry of Shelikof Strait and the western Gulf of Alaska (WGOA) from the edges of the land masses down to about 7000 m deep in the Aleutian Trench. This map was produced by combining soundings from historical National Ocean Service (NOS) smooth sheets (2.7 million soundings); shallow multibeam and LIDAR (light detection and ranging) data sets from the NOS and others (subsampled to 2.6 million soundings); and deep multibeam (subsampled to 3.3 million soundings), single-beam, and underway files from fisheries research cruises (9.1 million soundings). These legacy smooth sheet data, some over a century old, were the best descriptor of much of the shallower and inshore areas, but they are superseded by the newer multibeam and LIDAR, where available. Much of the offshore area is only mapped by non-hydrographic single-beam and underway files. We combined these disparate data sets by proofing them against their source files, where possible, in an attempt to preserve seafloor features for research purposes. -
Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
Curriculum Vitae
Curriculum Vitae Robin Hardy, Ph.D. Department of History and Philosophy 2-155 Wilson Hall Montana State University Bozeman, Montana 59717 [email protected] Special Interests Atlantic studies (Europe/Africa) Colonialism and post-colonialism in Africa: social justice, politics, economy, religion, culture Western presence/influence in Africa Jihād in the Sahel West African ethnic culture Diplomacy / Conflict Resolution Education Ph. D. – Modern European History. Montana State University - Bozeman, Montana. Focus: French colonialism in West Africa. Political/cultural contact zone. M.A. – European History (Diplomacy). University California at Santa Cruz – Santa Cruz, California. B.A. – Political Science (International Relations). University California at Los Angeles – Los Angeles, California. Professional Experience Faculty Lecturer/Instructor: Department of History and Philosophy - Montana State University. Bozeman, Montana (2010-Present). Courses: Modern Africa, HSTR 483 Colonial Africa, HSTR 491 History of Morocco: From antiquity to post-colonization (in-country), HSTR 492 Robin Hardy Curriculum Vitae - 2 Identity in North Africa, HSTR 492 Post-colonial Sudan and the problems of the refugee diaspora, HSTR 492 Nineteenth century Europe, HSTR 322 European intellectual history, HSTR 423 Twentieth century Europe, HSTR 324 Origins of European anarchism, HSTR 492 European language and culture in the Middle Ages, HSTR 492 Western Civilization I, HSTR 101IH Western Civilization II, HSTR 102IH Knowledge and Community, CLS 101 Papers, Publications, Professional Leadership Conference paper: “The Future of Militant Islam in the Western Sahel,” Association for the Study of the Middle East and Africa, Washington D.C., October 21, 2017. Moderator/Discussant: Progress and Problems in Post-Colonial Sub-Saharan Africa, Association for the Study of the Middle East and Africa, Washington D.C., October 20, 2017. -
Surficial Geology Investigations in Wellesley Basin and Nisling Range, Southwest Yukon J.D
Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon J.D. Bond, P.S. Lipovsky and P. von Gaza Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon Jeffrey D. Bond1 and Panya S. Lipovsky2 Yukon Geological Survey Peter von Gaza3 Geomatics Yukon Bond, J.D., Lipovsky, P.S. and von Gaza, P., 2008. Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon. In: Yukon Exploration and Geology 2007, D.S. Emond, L.R. Blackburn, R.P. Hill and L.H. Weston (eds.), Yukon Geological Survey, p. 125-138. ABSTRACT Results of surficial geology investigations in Wellesley basin and the Nisling Range can be summarized into four main highlights, which have implications for exploration, development and infrastructure in the region: 1) in contrast to previous glacial-limit mapping for the St. Elias Mountains lobe, no evidence for the late Pliocene/early Pleistocene pre-Reid glacial limits was found in the study area; 2) placer potential was identified along the Reid glacial limit where a significant drainage diversion occurred for Grayling Creek; 3) widespread permafrost was encountered in the study area including near-continuous veneers of sheet-wash; and 4) a monitoring program was initiated at a recently active landslide which has potential to develop into a catastrophic failure that could damage the White River bridge on the Alaska Highway. RÉSUMÉ Les résultats d’études géologiques des formations superficielles dans le bassin de Wellesley et la chaîne Nisling peuvent être résumés en quatre principaux faits saillants qui ont des répercussions pour l’exploration, la mise en valeur et l’infrastructure de la région. -
THE POLAR THAW: an Analysis of the Impacts of Climate Change on the Environment and Geopolitics of the Arctic Polar Region
THE POLAR THAW: An Analysis Of The Impacts Of Climate Change On The Environment And Geopolitics Of The Arctic Polar Region Alexandra Stoicof Spring 2008 ________________________________________________________________________ SIT Geneva: International Studies, Organizations and Social Justice Adrian Herrera, Arctic Power Alexandre Lambert, School for International Training The George Washington University International Affairs and Geography Stoicof 2 Copyright permission The author hereby does grant the School for International Training the permission to electronically reproduce and transmit this document to the students, alumni, staff, and faculty of the World Learning Community. The author hereby does grant the School for International Training the permission to electronically reproduce and transmit this document to the public via the World Wide Web or other electronic means. The author hereby does grant the School for International Training the permission to reproduce this document to the public in print format. Student (please print name): Alexandra Stoicof Signature: Date: Abstract The issues facing the Arctic region today are of relatively new importance on the agendas of environmentalists, lawyers, and national governments. Global warming is affecting the polar regions at a faster pace than the rest of the world, and is drastically changing the ecosystem and viability of the indigenous groups who depend on the environment of the tundra. The forced adaptation of the natives has lead to convictions of human rights and debates over the accountability of the world to affected communities. The retreat of Arctic sea-ice also exposes another area of controversy; the claims to the resources and passageways that are becoming increasingly accessible. The beginnings of an international race to claim sea territory has lead to interpretations of the law of the sea. -
Arctic Climate Change Implications for U.S
Arctic Climate Change Implications for U.S. National Security Perspective - Laura Leddy September 2020 i BOARD OF DIRECTORS The Honorable Gary Hart, Chairman Emeritus Scott Gilbert Senator Hart served the State of Colorado in the U.S. Senate Scott Gilbert is a Partner of Gilbert LLP and Managing and was a member of the Committee on Armed Services Director of Reneo LLC. during his tenure. Vice Admiral Lee Gunn, USN (Ret.) Governor Christine Todd Whitman, Chairperson Vice Admiral Gunn is Vice Chairman of the CNA Military Christine Todd Whitman is the President of the Whitman Advisory Board, Former Inspector General of the Department Strategy Group, a consulting firm that specializes in energy of the Navy, and Former President of the Institute of Public and environmental issues. Research at the CNA Corporation. The Honorable Chuck Hagel Brigadier General Stephen A. Cheney, USMC (Ret.), Chuck Hagel served as the 24th U.S. Secretary of Defense and President of ASP served two terms in the United States Senate (1997-2009). Hagel Brigadier General Cheney is the President of ASP. was a senior member of the Senate Foreign Relations; Banking, Housing and Urban Affairs; and Intelligence Committees. Matthew Bergman Lieutenant General Claudia Kennedy, USA (Ret.) Matthew Bergman is an attorney, philanthropist and Lieutenant General Kennedy was the first woman entrepreneur based in Seattle. He serves as a Trustee of Reed to achieve the rank of three-star general in the United States College on the Board of Visitors of Lewis & Clark Law Army. School. Ambassador Jeffrey Bleich The Honorable John F. Kerry The Hon. -
Paleolithic Fish from Southern Poland: a Paleozoogeographical Approach
10. ARCH. VOL. 22 (2ª)_ARCHAEOFAUNA 04/09/13 18:05 Página 123 Archaeofauna 22 (2013): 123-131 Paleolithic Fish from Southern Poland: A Paleozoogeographical Approach LEMBI LÕUGAS1, PIOTR WOJTAL2, JAROSŁAW WILCZYń SKI2 & KRZYSZTOF STEFANIAK3 1Department of Archaeobiology and Ancient Technology, Institute of History, University of Tallinn, Rüütli 6, EE10130 Tallinn, Estonia [email protected] 2Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Slawkowska 17, 31-016 Cracow, Poland [email protected], [email protected] 3Institute of Zoology, University of Wrocław, Sienkiewicza 21, 50-335 Wrocław, Poland [email protected] (Received 5 August 2012; Revised 31 October 2012; Accepted 17 July 2013) ABSTRACT: The area covered by glaciers during the Last Glacial Maximum (LGM) includes a large territory in northern Europe. In this region, Paleolithic finds are rare and fish bones fair- ly unique. Analysis of Paleolithic fish bones outside of the LGM range was carried out with the intention of reconstructing the paleozoogeographical distribution of this animal group before the retreat of the ice cap from the Baltic Basin. This research focuses on an archaeological fish bone assemblage from Obłazowa Cave, southern Poland. Other samples examined are from Krucza Skała Rock Shelter (Kroczyckie Rocks), Biśnik Cave (Wodąca Valley), Borsuka Cave (Szklarka Valley), and Nad Tunelem Cave (Prądnik Valley). The latter sites are considered natu- rally accumulated deposits, but, at Obłazowa and Krucza Skała, anthropogenic factors also played an important role. The fish bones from the Paleolithic cave deposits of Obłazowa inclu- ded at least six fish genera: Thymallus, Coregonus, Salmo, Salvelinus, Esox, and Cottus. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program.