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Report on 2014 Minister's Round Table on Parks Canada
Minister’s Round Table on Parks Canada 2 014 Building Urban to Arctic Connections INTRODUCTION On June 2, 2014, The Honourable Leona Aglukkaq, Participants in the MRT were asked to consider the Canada’s Minister of the Environment and Minister following questions: responsible for Parks Canada, hosted the seventh 1. How can we collectively increase Minister’s Round Table (MRT) on Parks Canada in visitation in Parks Canada places in the Ottawa, Ontario. This MRT, which focused on Canada’s North and provide a fuller experience of its North, included twenty stakeholders whose perspectives unique culture in ways that strengthen the represented a broad range of northern interests, such as traditional economy? tourism, education, arts and culture, conservation, and economic development, as well as representatives from 2. How can we collectively better connect Inuit and other Aboriginal organizations, other levels of urban Canadians with Parks Canada government, and the not-for-profit, public, and private places in the North? sectors. The MRT was structured as a one-day facili- Many ideas were put forward during the discussions. tated discussion designed to seek participants’ ideas The input of participants has been regrouped under and input on two topics related to the overarching theme three recommendations, which are detailed below, of “Building Urban to Arctic Connections.” along with Minister Aglukkaq’s responses to these The two discussion topics, “Connecting Urban recommendations. Canadians to Arctic places: Tourism and Traditional Economy,” and “Connecting the North to Urban Centres through Stories and Gateways,” reflect the intercon- nectedness of Parks Canada’s commitments to reaching Canadians where they live, work, and play and to celebrating the natural and cultural heritage of the North as an integral element of our national identity. -
07-08 November No. 2 Contents
THE ANTARCTICAN SOCIETY NEWSLETTER “BY AND FOR ALL ANTARCTICANS” VOL. 07-08 NOVEMBER NO. 2 CONTENTS PRESIDENT ANNOUNCEMENTS.............................cover SOUTH GEORGIA ASSOCIATION.................... 5 Dr. Arthur B. Ford 400 Ringwood Avenue BRASH ICE................................................. 1 BRITISH SEABED CLAIM................................... 5 Menlo Park, CA 94025 Phone: (650) 851-1532 SPEAKER FOR JOINT MEETING........... 2 JERRY KOOYMAN AWARD............................... 6 [email protected] SOUTH POLE DEDICATION.................. 2 PHYLACTERIES AT THE SOUTH POLE.......... 6 VICE PRESIDENT Robert B. Flint, Jr. CD ROM STILL AVAILABLE.................... 2 CAM CRADDOCK TRIBUTE.............................. 7 185 Bear Gulch Road Woodside, CA 94062 ANTARCTIC MUSIC................................ 3 I KNEW YOUR FATHER...................................... 8 Phone: (650) 851-1532 [email protected] Type to enter text CONVERSATION WITH AMUNDSEN............. 8 Type to enter text TREASURER Type to enter text Dr. Paul C. Dalrymple Box 325, Port Clyde, ME 04855 Phone: (207) 372-6523 [email protected] ANNOUNCEMENTS SECRETARY Charles Lagerbom YOU NOW HAVE A CHOICE, NEWSLETTER WILL BECOME AVAILABLE 83 Achorn Rd. Belfast, ME 04915 ELECTRONICALLY. Starting with our next issue, anticipated in late January 2008, you (207)548-0923 can pick up your Newsletter on our new web site which will be up and running the first of [email protected] the year, Members who choose to receive issues on the website will be given a password WEBMASTER -
Variability in Krill Biomass Links Harvesting and Climate Warming to Penguin Population Changes in Antarctica
Variability in krill biomass links harvesting and climate warming to penguin population changes in Antarctica Wayne Z. Trivelpiecea,1, Jefferson T. Hinkea,b, Aileen K. Millera, Christian S. Reissa, Susan G. Trivelpiecea, and George M. Wattersa aAntarctic Ecosystem Research Division, Southwest Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, La Jolla, CA, 92037; and bScripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093 Edited by John W. Terborgh, Duke University, Durham, NC, and approved March 11, 2011 (received for review November 5, 2010) The West Antarctic Peninsula (WAP) and adjacent Scotia Sea terns of population change observed before and after 1986 are support abundant wildlife populations, many of which were nearly explained by recruitment trends. During the first decade of our extirpated by humans. This region is also among the fastest- studies, 40–60% of the penguins banded as fledglings recruited warming areas on the planet, with 5–6 °C increases in mean winter back to natal colonies, and first-time breeders constituted 20– air temperatures and associated decreases in winter sea-ice cover. 25% of the breeding population annually (Fig. 1 C and D). These biological and physical perturbations have affected the eco- Subsequently, survival to first breeding dropped precipitously in system profoundly. One hypothesis guiding ecological interpreta- the 1980s, and the recruitment rates of both species have de- tions of changes in top predator populations in this region, the clined (7). Less than 10% of Adélie penguins banded as chicks “sea-ice hypothesis,” proposes that reductions in winter sea ice survive to breed (Fig. -
Concentrations, Particle-Size Distributions, and Dry Deposition fluxes of Aerosol Trace Elements Over the Antarctic Peninsula in Austral Summer
Atmos. Chem. Phys., 21, 2105–2124, 2021 https://doi.org/10.5194/acp-21-2105-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Concentrations, particle-size distributions, and dry deposition fluxes of aerosol trace elements over the Antarctic Peninsula in austral summer Songyun Fan1, Yuan Gao1, Robert M. Sherrell2, Shun Yu1, and Kaixuan Bu2 1Department of Earth and Environmental Sciences, Rutgers University, Newark, NJ 07102, USA 2Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, USA Correspondence: Yuan Gao ([email protected]) Received: 1 July 2020 – Discussion started: 26 August 2020 Revised: 3 December 2020 – Accepted: 8 December 2020 – Published: 12 February 2021 Abstract. Size-segregated particulate air samples were col- sition processes may play a minor role in determining trace lected during the austral summer of 2016–2017 at Palmer element concentrations in surface seawater over the conti- Station on Anvers Island, western Antarctic Peninsula, to nental shelf of the western Antarctic Peninsula. characterize trace elements in aerosols. Trace elements in aerosol samples – including Al, P, Ca, Ti, V, Mn, Ni, Cu, Zn, Ce, and Pb – were determined by total digestion and a 1 Introduction sector field inductively coupled plasma mass spectrometer (SF-ICP-MS). The crustal enrichment factors (EFcrust) and Aerosols affect the climate through direct and indirect ra- k-means clustering results of particle-size distributions show diative forcing (Kaufman et al., 2002). The extent of such that these elements are derived primarily from three sources: forcing depends on both physical and chemical properties (1) regional crustal emissions, including possible resuspen- of aerosols, including particle size and chemical composi- sion of soils containing biogenic P, (2) long-range transport, tion (Pilinis et al., 1995). -
South Georgia and Antarctic Odyssey
South Georgia and Antarctic Odyssey 30 November – 18 December 2019 | Greg Mortimer About Us Aurora Expeditions embodies the spirit of adventure, travelling to some of the most wild opportunity for adventure and discovery. Our highly experienced expedition team of and remote places on our planet. With over 28 years’ experience, our small group voyages naturalists, historians and destination specialists are passionate and knowledgeable – they allow for a truly intimate experience with nature. are the secret to a fulfilling and successful voyage. Our expeditions push the boundaries with flexible and innovative itineraries, exciting Whilst we are dedicated to providing a ‘trip of a lifetime’, we are also deeply committed to wildlife experiences and fascinating lectures. You’ll share your adventure with a group education and preservation of the environment. Our aim is to travel respectfully, creating of like-minded souls in a relaxed, casual atmosphere while making the most of every lifelong ambassadors for the protection of our destinations. DAY 1 | Saturday 30 November 2019 Ushuaia, Beagle Channel Position: 20:00 hours Course: 83° Wind Speed: 20 knots Barometer: 991 hPa & steady Latitude: 54°49’ S Wind Direction: W Air Temp: 6° C Longitude: 68°18’ W Sea Temp: 5° C Explore. Dream. Discover. —Mark Twain in the soft afternoon light. The wildlife bonanza was off to a good start with a plethora of seabirds circling the ship as we departed. Finally we are here on the Beagle Channel aboard our sparkling new ice-strengthened vessel. This afternoon in the wharf in Ushuaia we were treated to a true polar welcome, with On our port side stretched the beech forested slopes of Argentina, while Chile, its mountain an invigorating breeze sweeping the cobwebs of travel away. -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
Chinstrap Penguin Declines
Author's personal copy Polar Biol DOI 10.1007/s00300-012-1230-3 ORIGINAL PAPER First direct, site-wide penguin survey at Deception Island, Antarctica, suggests significant declines in breeding chinstrap penguins Ron Naveen • Heather J. Lynch • Steven Forrest • Thomas Mueller • Michael Polito Received: 18 April 2012 / Revised: 25 July 2012 / Accepted: 31 July 2012 Ó Springer-Verlag 2012 Abstract Deception Island (62°570S, 60°380W) is one of 1986/1987. A comparative analysis of high-resolution satel- the most frequently visited locations in Antarctica, prompt- lite imagery for the 2002/2003 and the 2009/2010 seasons ing speculation that tourism may have a negative impact suggests a 39 % (95th percentile CI = 6–71 %) decline on the island’s breeding chinstrap penguins (Pygoscelis (from 85,473 ± 23,352 to 52,372 ± 14,309 breeding pairs) antarctica). Discussions regarding appropriate management over that 7-year period and provides independent confirma- of Deception Island and its largest penguin colony at Baily tion of population decline in the abundance of breeding Head have thus far operated in the absence of concrete chinstrap penguins at Baily Head. The decline in chinstrap information regarding the current size of the penguin popu- penguins at Baily Head is consistent with declines in this lation at Deception Island or long-term changes in abun- species throughout the region, including sites that receive dance. In the first ever field census of individual penguin little or no tourism; as a consequence of regional environ- nests at Deception Island (December 2–14, 2011), we find mental changes that currently represent the dominant influ- 79,849 breeding pairs of chinstrap penguins, including ence on penguin dynamics, we cannot ascribe any direct link 50,408 breeding pairs at Baily Head and 19,177 breeding between chinstrap declines and tourism from this study. -
Ice Core Records As Sea Ice Proxies: an Evaluation from the Weddell Sea Region of Antarctica Nerilie J
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, D15101, doi:10.1029/2006JD008139, 2007 Click Here for Full Article Ice core records as sea ice proxies: An evaluation from the Weddell Sea region of Antarctica Nerilie J. Abram,1 Robert Mulvaney,1 Eric W. Wolff,1 and Manfred Mudelsee2,3 Received 12 October 2006; revised 2 May 2007; accepted 5 June 2007; published 3 August 2007. [1] Ice core records of methanesulfonic acid (MSA) from three sites around the Weddell Sea are investigated for their potential as sea ice proxies. It is found that the amount of MSA reaching the ice core sites decreases following years of increased winter sea ice in the Weddell Sea; opposite to the expected relationship if MSA is to be used as a sea ice proxy. It is also shown that this negative MSA-sea ice relationship cannot be explained by the influence that the extensive summer ice pack in the Weddell Sea has on MSA production area and transport distance. A historical record of sea ice from the northern Weddell Sea shows that the negative relationship between MSA and winter sea ice exists over interannual (7-year period) and multidecadal (20-year period) timescales. National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data suggest that this negative relationship is most likely due to variations in the strength of cold offshore wind anomalies traveling across the Weddell Sea, which act to synergistically increase sea ice extent (SIE) while decreasing MSA delivery to the ice core sites. Hence our findings show that in some locations atmospheric transport strength, rather than sea ice conditions, is the dominant factor that determines the MSA signal preserved in near-coastal ice cores. -
Variability in Krill Biomass Links Harvesting and Climate Warming to Penguin Population Changes in Antarctica
Variability in krill biomass links harvesting and climate warming to penguin population changes in Antarctica Wayne Z. Trivelpiecea,1, Jefferson T. Hinkea,b, Aileen K. Millera, Christian S. Reissa, Susan G. Trivelpiecea, and George M. Wattersa aAntarctic Ecosystem Research Division, Southwest Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, La Jolla, CA, 92037; and bScripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093 Edited by John W. Terborgh, Duke University, Durham, NC, and approved March 11, 2011 (received for review November 5, 2010) The West Antarctic Peninsula (WAP) and adjacent Scotia Sea terns of population change observed before and after 1986 are support abundant wildlife populations, many of which were nearly explained by recruitment trends. During the first decade of our extirpated by humans. This region is also among the fastest- studies, 40–60% of the penguins banded as fledglings recruited warming areas on the planet, with 5–6 °C increases in mean winter back to natal colonies, and first-time breeders constituted 20– air temperatures and associated decreases in winter sea-ice cover. 25% of the breeding population annually (Fig. 1 C and D). These biological and physical perturbations have affected the eco- Subsequently, survival to first breeding dropped precipitously in system profoundly. One hypothesis guiding ecological interpreta- the 1980s, and the recruitment rates of both species have de- tions of changes in top predator populations in this region, the clined (7). Less than 10% of Adélie penguins banded as chicks “sea-ice hypothesis,” proposes that reductions in winter sea ice survive to breed (Fig. -
Observation of Ocean Tides Below the Filchner
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. C8, PAGES 19,615-19,630,AUGUST 15, 2000 Observation of ocean tides below the Filchher and Ronne Ice Shelves, Antarctica, using synthetic aperture radar interferometry' Comparison with tide model predictions E. Rignot,1 L. Padman,•' D. R. MacAyeal,3 and M. Schmeltz1 Abstract. Tides near and under floating glacial ice, such as ice shelvesand glacier termini in fjords, can influence heat transport into the subice cavity, mixing of the under-ice water column, and the calving and subsequentdrift of icebergs. Free- surface displacementpatterns associatedwith ocean variability below glacial ice can be observedby differencingtwo syntheticaperture radar (SAR) interferograms, each of which representsthe combination of the displacement patterns associated with the time-varying vertical motion and the time-independent lateral ice flow. We present the pattern of net free-surface displacement for the iceberg calving regions of the Ronne and Filchher Ice Shelves in the southern Weddell Sea. By comparing SAR-based displacementfields with ocean tidal models, the free-surface displacementvariability for these regions is found to be dominated by ocean tides. The inverse barometer effect, i.e., the ocean's isostatic responseto changing atmospheric pressure, also contributes to the observed vertical displacement. The principal value of using SAR interferometry in this manner lies in the very high lateral resolution(tens of meters) obtainedover the large regioncovered by each SAR image. Small features that are not well resolvedby the typical grid spacing of ocean tidal models may contribute to such processesas iceberg calving and cross-frontalventilation of the ocean cavity under the ice shelf. -
Distribution and Abundance of Breeding Birds at Deception Island, South Shetland Islands, Antarctica, February to April 2000
Bó & Copello: Deception Island breeding birds’ distribution and abundance 39 DISTRIBUTION AND ABUNDANCE OF BREEDING BIRDS AT DECEPTION ISLAND, SOUTH SHETLAND ISLANDS, ANTARCTICA, FEBRUARY TO APRIL 2000 MARÍA SUSANA BÓ & SOFÍA COPELLO Universidad Nacional de Mar del Plata, Facultad de Ciencias Exactas y Naturales, Departamento de Biología, Laboratorio de Vertebrados, Funes 3350, 7600 Mar del Plata, Argentina ([email protected]) Received 20 September 2000, accepted 15 January 2001 SUMMARY BÓ, M.S. & COPELLO, S. 2000. Distribution and abundance of breeding birds at Deception Island, South Shetland Islands, Antarctica, February to April 2000. Marine Ornithology 29: 39–42. A survey of breeding birds during the brooding stage was carried out from February to April 2000 in the southern portion of Deception Island, South Shetland Islands, Antarctica. This island supports two Sites of Special Scien- tific Interest (SSSI Nos. 21 and 27). Nine species were found breeding in the study area: Chinstrap Penguin Pygoscelis antarctica (an estimated 6820 breeding pairs at two colonies surveyed), Pintado or Cape Petrel Daption capense (36), Wilson’s Storm Petrel Oceanites oceanicus (3), Antarctic Cormorant Phalacrocorax atriceps bransfieldensis (9), Greater Sheathbill Chionis alba (2), Subantarctic Skua Catharacta antarctica (4), South Polar Skua C. maccormicki (11), Kelp Gull Larus dominicanus (49) and Antarctic Tern Sterna vittata (5). Due to the increasing tourist activity at Deception Island, better information on the location and size of breeding populations is a particular requirement if effective precautionary conservation actions are to be taken. Key words: seabird censuses, Deception Island, Antarctica INTRODUCTION tal Protection to the Antarctic Treaty and the Convention on the Conservation of Antarctic Marine Living Resources (CCAMLR) Populations of most seabird species in Antarctica are stable or (Walton & Dingwall 1995). -
Reconnaissance of the Filchner Ice Shelf and Berkner Island, Weddell Sea, Antarctica
Indian Expedition to Weddell Sea Antarctica, Scientific Report, 1995 Department of Ocean Development, Technical Publication No. 7, pp.1-14 Reconnaissance of the Filchner Ice Shelf and Berkner Island, Weddell Sea, Antarctica V.K. RAINA, S.MUKERJI, A.S. GILL AND F. DOTIWALA* Geological Survey of India; Oil & Natural Gas Commission Introduction Antarctic continent is surrounded, all around by a permanent ice shelf, at places almost 100 km wide. Besides this circum-continental shelf, there also exist three major ice shelves, Fig.1. The area along south Weddell Sea reconnoitred by the Expedition. 2 V.K. Rainaetal. namely: Ross ice shelf; Amery ice shelf and the Filchner-Ronne ice shelf, which cover the embayments (inlets) within the physiographic domain of this continent. The Filchner and Ronne ice shelves exist along the southern and the south-western limits of the Weddell Sea within the longitudes 34° W and 63° W and latitudes 78° S to 82° S and cover an area of about 5,00,000 km including some large ice rises. This shelf, as the name suggests, comprises the Filchner shelf, in the east, and larger of the two, Ronne shelf in the west, separated, along the northern extremity i.e. north of 81° S latitude, by the largest ice rise in Antarctica - the Berkner island. Southward, the two shelves merge into one. Filchner Shelf is named after Wilhelm Filchner, the Leader of the German Expedition that landed and established a field station on it, for the first time, way back in 1912. This shelf differs from the circum-continental shelf in being more rugged, crevassed and rumpled with large escarpments, and is primarily the extension of the Polar ice.