Navigating the Arctic Meltdown
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Contamination of Four Ivory Gull (Pagophila
Contamination of four ivory gull (Pagophila eburnea) colonies in Svalbard in link with their trophic behaviour Magali Lucia, Hallvard Strøm, Paco Bustamante, Dorte Herzke, Geir Gabrielsen To cite this version: Magali Lucia, Hallvard Strøm, Paco Bustamante, Dorte Herzke, Geir Gabrielsen. Contamination of four ivory gull (Pagophila eburnea) colonies in Svalbard in link with their trophic behaviour. Polar Biology, Springer Verlag, 2017, 40, pp.917-929. 10.1007/s00300-016-2018-7. hal-01683806 HAL Id: hal-01683806 https://hal.archives-ouvertes.fr/hal-01683806 Submitted on 14 Jan 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Contamination of four ivory gull (Pagophila eburnea) colonies in Svalbard in link with their trophic behaviour Magali Lucia1*, Hallvard Strøm1, Paco Bustamante2, Dorte Herzke3, Geir W. Gabrielsen1 1 Norwegian Polar Institute, FRAM High North Research Centre for Climate and the Environment, 9296 Tromsø, Norway 2 Littoral, Environnement et Sociétés (LIENSs), UMR 7266 CNRS-Université de La Rochelle, 2 rue Olympe de Gouges, 17000 La Rochelle, France. 3 Norwegian Institute for Air Research, FRAM High North Research Centre for Climate and the Environment, 9296 Tromsø, Norway *Corresponding author: Magali LUCIA Email: [email protected] Address: Norwegian Polar Institute, Fram Centre Hjalmar Johansens gt. -
New Longevity Record for Ivory Gulls (Pagophila Eburnea) and Evidence of Natal Philopatry M.L
ARCTIC VOL. 65, NO. 1 (MARCH 2012) P. 98 – 101 New Longevity Record for Ivory Gulls (Pagophila eburnea) and Evidence of Natal Philopatry M.L. MALLORY,1 K.A. ALLARD,2 B.M. BRAUNE,3 H.G. GILCHRIST3 and V.G. THOMAS4 (Received 25 April 2011; accepted in revised form 2 August 2011) ABSTRACT. Ivory gulls (Pagophila eburnea) have been listed as “endangered” in Canada and “near threatened” interna- tionally. In June 2010, we visited Seymour Island, Nunavut, Canada, where gulls were banded in the 1970s and 1980s. We recaptured and released two breeding gulls banded as chicks in 1983, confirming natal philopatry to this breeding colony. These gulls are more than 28 years old, making the ivory gull one of the longest-living marine bird species known in North America. Key words: ivory gull, Pagophila eburnea, Nunavut, banding RÉSUMÉ. La mouette blanche (Pagophila eburnea) figure sur la liste des espèces « en voie de disparition » sur la scène canadienne et des espèces « quasi menacées » sur la scène internationale. En juin 2010, nous sommes allés à l’île Seymour, au Nunavut, Canada, où des mouettes avaient été baguées dans le courant des années 1970 et 1980. Nous avons recapturé et relâché deux mouettes reproductrices qui étaient considérées comme des oisillons en 1983, ce qui nous a permis de confirmer la philopatrie natale de cette colonie de nidification. Ces mouettes blanches ont plus de 28 ans, ce qui en fait l’un des oiseaux aquatiques vivant le plus longtemps en Amérique du Nord. Mots clés : mouette blanche, Pagophila eburnea, Nunavut, baguage Traduit pour la revue Arctic par Nicole Giguère. -
Seabirds of Spitsbergen Ivory Gull (Pagophila Eburnea) Sabine's Gull
Seabirds of Spitsbergen Although only one species of bird (the ptarmigan) is able to withstand the harsh Svalbard winters, this Arctic archipelago is a hub for many species of visiting breeding birds, especially sea birds. As you explore the ancient fjords and sail along the untamed coastal waters, you are likely to encounter a range of beautiful and fascinating species which visit Spitsbergen during the summer months. Whether watching the comic mishaps of little auks bouncing off the waves, admiring the carefree glide of the fulmar or watching the startling ivory gull to see whether it will lead you to a polar bear, the seabirds are an enigmatic aspect of any Arctic experience. Ivory gull (Pagophila eburnea ) This striking and surprisingly agile gull is distinctive in its brilliant white plumage. Immature ivory gulls also have white plumage but have a scattering of brownish-black spots on the body and the tips of the wing feathers. Like many other gulls, this Arctic species is an opportunistic feeder, consuming a wide range of foods that it encounters but it is commonly associated with scavenging from kills and these gulls will often follow polar bears and even human hunters to feed on the scraps from their kills. In parts of its range, ivory gull numbers have fallen rapidly. For example, surveys of breeding colonies in Canada in 2002 and 2003 revealed that populations had declined by 80 percent since the early 1980s. Sabine's gull ( Xema sabini ) The rare Sabine’s gull is a small species of gull, which breeds in the Arctic and has a circumpolar distribution. -
A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations
1AUGUST 2021 W A T T S E T A L . 6399 A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations a a a a MATTHEW WATTS, WIESLAW MASLOWSKI, YOUNJOO J. LEE, JACLYN CLEMENT KINNEY, AND b ROBERT OSINSKI a Department of Oceanography, Naval Postgraduate School, Monterey, California b Institute of Oceanology of Polish Academy of Sciences, Sopot, Poland (Manuscript received 29 June 2020, in final form 28 April 2021) ABSTRACT: The Arctic sea ice response to a warming climate is assessed in a subset of models participating in phase 6 of the Coupled Model Intercomparison Project (CMIP6), using several metrics in comparison with satellite observations and results from the Pan-Arctic Ice Ocean Modeling and Assimilation System and the Regional Arctic System Model. Our study examines the historical representation of sea ice extent, volume, and thickness using spatial analysis metrics, such as the integrated ice edge error, Brier score, and spatial probability score. We find that the CMIP6 multimodel mean captures the mean annual cycle and 1979–2014 sea ice trends remarkably well. However, individual models experience a wide range of uncertainty in the spatial distribution of sea ice when compared against satellite measurements and reanalysis data. Our metrics expose common and individual regional model biases, which sea ice temporal analyses alone do not capture. We identify large ice edge and ice thickness errors in Arctic subregions, implying possible model specific limitations in or lack of representation of some key physical processes. We postulate that many of them could be related to the oceanic forcing, especially in the marginal and shelf seas, where seasonal sea ice changes are not adequately simulated. -
Thinking About the Arctic's Future
By Lawson W. Brigham ThinkingThinking aboutabout thethe Arctic’sArctic’s Future:Future: ScenariosScenarios forfor 20402040 MIKE DUNN / NOAA CLIMATE PROGRAM OFFICE, NABOS 2006 EXPEDITION The warming of the Arctic could These changes have profound con- ing in each of the four scenarios. mean more circumpolar sequences for the indigenous people, • Transportation systems, espe- for all Arctic species and ecosystems, cially increases in marine and air transportation and access for and for any anticipated economic access. the rest of the world—but also development. The Arctic is also un- • Resource development—for ex- an increased likelihood of derstood to be a large storehouse of ample, oil and gas, minerals, fish- yet-untapped natural resources, a eries, freshwater, and forestry. overexploited natural situation that is changing rapidly as • Indigenous Arctic peoples— resources and surges of exploration and development accel- their economic status and the im- environmental refugees. erate in places like the Russian pacts of change on their well-being. Arctic. • Regional environmental degra- The combination of these two ma- dation and environmental protection The Arctic is undergoing an jor forces—intense climate change schemes. extraordinary transformation early and increasing natural-resource de- • The Arctic Council and other co- in the twenty-first century—a trans- velopment—can transform this once- operative arrangements of the Arctic formation that will have global im- remote area into a new region of im- states and those of the regional and pacts. Temperatures in the Arctic are portance to the global economy. To local governments. rising at unprecedented rates and evaluate the potential impacts of • Overall geopolitical issues fac- are likely to continue increasing such rapid changes, we turn to the ing the region, such as the Law of throughout the century. -
Some Aspects of the Thermal Energy Exchange on the South Polar Snow Field and Arctic Ice Pack'
MAY 1961 MONTHLY WEATHER REVIEW 173 SOME ASPECTS OF THE THERMAL ENERGY EXCHANGE ON THE SOUTH POLAR SNOW FIELD AND ARCTIC ICE PACK' KIRBY J. HANSON Po!ar Meteorology Research Project, US. Weather Bureau, Washington, D.C. [Manuscript received September 13, 1960; revised February 21, 1961 ] ABSTRACT Solar and terrestrial radiation measurements that were obtained at Amundsen-Scot>t (South Pole) Station and on Ice lsland (Bravo) T-3 are presented for representative summer and winter months. Of the South Polar net radiation loss during April 1958, approximately20 percent of the energy came from the snow and80 percent from the air. The actual atmospheric cooling rate during that period was only about lj6 of the suggested radiative cooling rate. The annual net radiation at various places in Antarctica is presented. During 1058, the South Polar atmos- phere transmitted about 73 percent of the annual extraterrestrial radiation, while at T-3 the Arctic atmosphere transmitted about 56 percent. The albedo of melting sea ice is discussed. Measurements on T-3 during July 1958 indicate that the net radiation is positive on both clear and overcast days but greatest on overcast days. Refreezing of the surface with clear skies, as observed by Untersteiner and Badglep, is discussed. 1. INTRODUCTION Ocean.ThisIsland wasabout by 5 11 miles in size and The elliptical orbit of the earthbrings it about 3 million about 52 meters thick (Crary et al. [2]) in 1953 when it miles farther from the sun at aphelion than at perihelion; drifted near 88' N., looo W. In the years that followed, consequently,during midsummer, about 7 percent less this it drifted southward and in July 1958 was located solar radiation impinges on the top of the Arctic atrnos- 79.5' N., 118' W. -
Downloaded 10/01/21 10:31 PM UTC 874 JOURNAL of CLIMATE VOLUME 12
MARCH 1999 VAVRUS 873 The Response of the Coupled Arctic Sea Ice±Atmosphere System to Orbital Forcing and Ice Motion at 6 kyr and 115 kyr BP STEPHEN J. VAVRUS Center for Climatic Research, Institute for Environmental Studies, University of WisconsinÐMadison, Madison, Wisconsin (Manuscript received 2 February 1998, in ®nal form 11 May 1998) ABSTRACT A coupled atmosphere±mixed layer ocean GCM (GENESIS2) is forced with altered orbital boundary conditions for paleoclimates warmer than modern (6 kyr BP) and colder than modern (115 kyr BP) in the high-latitude Northern Hemisphere. A pair of experiments is run for each paleoclimate, one with sea-ice dynamics and one without, to determine the climatic effect of ice motion and to estimate the climatic changes at these times. At 6 kyr BP the central Arctic ice pack thins by about 0.5 m and the atmosphere warms by 0.7 K in the experiment with dynamic ice. At 115 kyr BP the central Arctic sea ice in the dynamical version thickens by 2±3 m, accompanied bya2Kcooling. The magnitude of these mean-annual simulated changes is smaller than that implied by paleoenvironmental evidence, suggesting that changes in other earth system components are needed to produce realistic simulations. Contrary to previous simulations without atmospheric feedbacks, the sign of the dynamic sea-ice feedback is complicated and depends on the region, the climatic variable, and the sign of the forcing perturbation. Within the central Arctic, sea-ice motion signi®cantly reduces the amount of ice thickening at 115 kyr BP and thinning at 6 kyr BP, thus serving as a strong negative feedback in both pairs of simulations. -
Educator Guide
E DUCATOR GUIDE This guide, and its contents, are Copyrighted and are the sole Intellectual Property of Science North. E DUCATOR GUIDE The Arctic has always been a place of mystery, myth and fascination. The Inuit and their predecessors adapted and thrived for thousands of years in what is arguably the harshest environment on earth. Today, the Arctic is the focus of intense research. Instead of seeking to conquer the north, scientist pioneers are searching for answers to some troubling questions about the impacts of human activities around the world on this fragile and largely uninhabited frontier. The giant screen film, Wonders of the Arctic, centers on our ongoing mission to explore and come to terms with the Arctic, and the compelling stories of our many forays into this captivating place will be interwoven to create a unifying message about the state of the Arctic today. Underlying all these tales is the crucial role that ice plays in the northern environment and the changes that are quickly overtaking the people and animals who have adapted to this land of ice and snow. This Education Guide to the Wonders of the Arctic film is a tool for educators to explore the many fascinating aspects of the Arctic. This guide provides background information on Arctic geography, wildlife and the ice, descriptions of participatory activities, as well as references and other resources. The guide may be used to prepare the students for the film, as a follow up to the viewing, or to simply stimulate exploration of themes not covered within the film. -
Arctic Report Card 2017
Arctic Report Card 2017 Arctic Report Card 2017 Arctic shows no sign of returning to reliably frozen region of recent past decades 2017 Headlines 2017 Headlines Video Executive Summary Contacts Arctic shows no sign of returning to reliably frozen Vital Signs region of recent past decades Surface Air Temperature Despite relatively cool summer temperatures, Terrestrial Snow Cover observations in 2017 continue to indicate that the Greenland Ice Sheet Arctic environmental system has reached a 'new Sea Ice normal', characterized by long-term losses in the Sea Surface Temperature extent and thickness of the sea ice cover, the extent Arctic Ocean Primary Productivity and duration of the winter snow cover and the mass of ice in the Greenland Ice Sheet and Arctic glaciers, Tundra Greenness and warming sea surface and permafrost Other Indicators temperatures. Terrestrial Permafrost Groundfish Fisheries in the Highlights Eastern Bering Sea Wildland Fire in High Latitudes • The average surface air temperature for the year ending September 2017 is the 2nd warmest since 1900; however, cooler spring and summer temperatures contributed to a rebound in snow cover in the Eurasian Arctic, slower summer sea ice loss, Frostbites and below-average melt extent for the Greenland ice sheet. Paleoceanographic Perspectives • The sea ice cover continues to be relatively young and thin with older, thicker ice comprising only 21% of the ice cover in on Arctic Ocean Change 2017 compared to 45% in 1985. Collecting Environmental • In August 2017, sea surface temperatures in the Barents and Chukchi seas were up to 4° C warmer than average, Intelligence in the New Arctic contributing to a delay in the autumn freeze-up in these regions. -
Arctic Report Card 2018 Effects of Persistent Arctic Warming Continue to Mount
Arctic Report Card 2018 Effects of persistent Arctic warming continue to mount 2018 Headlines 2018 Headlines Video Executive Summary Effects of persistent Arctic warming continue Contacts to mount Vital Signs Surface Air Temperature Continued warming of the Arctic atmosphere Terrestrial Snow Cover and ocean are driving broad change in the Greenland Ice Sheet environmental system in predicted and, also, Sea Ice unexpected ways. New emerging threats Sea Surface Temperature are taking form and highlighting the level of Arctic Ocean Primary uncertainty in the breadth of environmental Productivity change that is to come. Tundra Greenness Other Indicators River Discharge Highlights Lake Ice • Surface air temperatures in the Arctic continued to warm at twice the rate relative to the rest of the globe. Arc- Migratory Tundra Caribou tic air temperatures for the past five years (2014-18) have exceeded all previous records since 1900. and Wild Reindeer • In the terrestrial system, atmospheric warming continued to drive broad, long-term trends in declining Frostbites terrestrial snow cover, melting of theGreenland Ice Sheet and lake ice, increasing summertime Arcticriver discharge, and the expansion and greening of Arctic tundravegetation . Clarity and Clouds • Despite increase of vegetation available for grazing, herd populations of caribou and wild reindeer across the Harmful Algal Blooms in the Arctic tundra have declined by nearly 50% over the last two decades. Arctic • In 2018 Arcticsea ice remained younger, thinner, and covered less area than in the past. The 12 lowest extents in Microplastics in the Marine the satellite record have occurred in the last 12 years. Realms of the Arctic • Pan-Arctic observations suggest a long-term decline in coastal landfast sea ice since measurements began in the Landfast Sea Ice in a 1970s, affecting this important platform for hunting, traveling, and coastal protection for local communities. -
Field Identification of West Palearctic Gulls P
British Birds VOLUME 71 NUMBER 4 APRIL 1978 Field identification of west Palearctic gulls P. J. Grant The west Palearctic list includes 23 species of gulls: more than half the world total. Field guides—because of their concise format—provide inad equate coverage of identification and ageing, which has probably fostered the indifference felt by many bird watchers towards gulls. This five- part series aims to change that attitude nterest in identifying gulls is growing, as part of the recent general I improvement in identification standards, but doubtless also stimulated by the addition to the British and Irish list of no less than three Nearctic species in little over a decade (Laughing Gull Larus atricilla in 1966, Franklin's Gull L. pipixcan in 1970 and Ring-billed Gull L. delaivarensis in 1973). The realisation is slowly dawning that regular checking through flocks of gulls can be worthwhile. Just as important as identification is the ability to recognise the age of individual immatures. This is obviously necessary in studies of popula tion, distribution and migration, but is also a challenge in its own right to the serious bird-identifier. Indeed, identification and ageing go hand- in-hand, for it is only by practising his recognition skills on the common species—of all ages—that an observer will acquire the degree of familiarity necessary for the confident identification of the occasional rarity. The enormous debt owed to D.J. Dwight's The Gulls of the World (1925) is readily acknowledged. That work, however, has long been out of print and its format was designed for the museum and taxonomic worker; the present series of papers will provide a reference more suited to field observers. -
Interannual Variability in Transpolar Drift Ice Thickness and Potential Impact of Atlantification
https://doi.org/10.5194/tc-2020-305 Preprint. Discussion started: 22 October 2020 c Author(s) 2020. CC BY 4.0 License. Interannual variability in Transpolar Drift ice thickness and potential impact of Atlantification H. Jakob Belter1, Thomas Krumpen1, Luisa von Albedyll1, Tatiana A. Alekseeva2, Sergei V. Frolov2, Stefan Hendricks1, Andreas Herber1, Igor Polyakov3,4,5, Ian Raphael6, Robert Ricker1, Sergei S. Serovetnikov2, Melinda Webster7, and Christian Haas1 1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany 2Arctic and Antarctic Research Institute, St. Petersburg, Russian Federation 3International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, US 4College of Natural Science and Mathematics, University of Alaska Fairbanks, Fairbanks, US 5Finnish Meteorological Institute, Helsinki, Finland 6Thayer School of Engineering at Dartmouth College, Hanover, US 7Geophysical Institute, University of Alaska Fairbanks, Fairbanks, US Correspondence: H. Jakob Belter ([email protected]) Abstract. Changes in Arctic sea ice thickness are the result of complex interactions of the dynamic and variable ice cover with atmosphere and ocean. Most of the sea ice exits the Arctic Ocean through Fram Strait, which is why long-term measurements of ice thickness at the end of the Transpolar Drift provide insight into the integrated signals of thermodynamic and dynamic influences along the pathways of Arctic sea ice. We present an updated time series of extensive ice thickness surveys carried 5 out at the end of the Transpolar Drift between 2001 and 2020. Overall, we see a more than 20% thinning of modal ice thickness since 2001. A comparison with first preliminary results from the international Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) shows that the modal summer thickness of the MOSAiC floe and its wider vicinity are consistent with measurements from previous years.