National Progress Reports Greenland – 2020 & 2019
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Naalakkersuisoq Karl-Kristian Kruses Tale Nordatlantisk
Naalakkersuisoq Karl-Kristian Kruses tale Nordatlantisk Fiskeriministerkonference i Shediac 29. august 2017 Dear friends and colleagues I would like to thank our hosts for this chance to visit beautiful New Brunswick and appreciate the hospitality we have been greeted with here. For Greenland, Canada is our closest neighbour and especially with Nunavut, we share a strong sense of culture. We experience similar challenges. We have strong partnerships on many issues as we share a like-minded approach to a safe and sustainable Arctic development with respect for local culture and traditional ways of life. Together Greenland and Nunavut communicate the cultural and social values of the indigenous peoples of the Arctic. Through cooperation we are able to promote greater understanding of the issues that are important to the people of the Arctic. Therefore, it is indeed a pleasure for us to meet with our friends and colleagues here in New Brunswick to talk about measures to protect our Arctic and North Atlantic Oceans. Intro The protection of the marine environment in Greenland falls under the remit of different ministries. The Ministry of Nature and Environment is responsible for the international agreements and conventions regarding biodiversity and overall nature conservation in Greenland, including protection of the marine environment. The Ministry of Fisheries and Hunting is responsible for the management of all living resources. It is therefore essential, when we talk about ocean governance, that we have close cooperation across sectors. It is also essential that we work across borders as we share marine ecosystems and resources among us. What we have done to protect the marine environment We have in Greenland almost 5 % marine protected areas according to IUCN standards. -
Balaenoptera Bonaerensis – Antarctic Minke Whale
Balaenoptera bonaerensis – Antarctic Minke Whale compared to B. bonaerensis. This smaller form, termed the “Dwarf” Minke Whale, may be genetically different from B. bonaerensis, and more closely related to the North Pacific Minke Whales, and thus has been classified B. acutorostrata (Wada et al. 1991; IWC 2001). This taxonomic position, although somewhat controversial, has been accepted by the Convention on International Trade in Endangered Species of Wild Fauna and Flora (CITES), and the Convention on Migratory Species (CMS). Assessment Rationale The current IWC global estimate of abundance of Antarctic Dr. Meike Scheidat Minke Whales is about 500,000 individuals. The abundance estimates declined from about 700,000 for the second circumpolar set of abundance survey cruises Regional Red List status (2016) Least Concern* (1985/86 to 1990/91) to about 500,000 for the third National Red List status (2004) Least Concern (1991/92 to 2003/04). Although this decline was not statistically significant, the IWC Scientific Committee does Reasons for change No change consider these results to reflect a change. However, Global Red List status (2008) Data Deficient whether this change is genuine or attributed to greater proportions of pack ice limiting the survey extent, has not TOPS listing (NEMBA) (2007) None yet been determined. More detailed results from an CITES listing (1986) Appendix I assessment model are available for the mid-Indian to the mid-Pacific region, and suggest that the population Endemic No increased to a peak in 1970 and then declined, with it *Watch-list Data being unclear whether this decline has levelled off or is still continuing past 2000. -
Order CETACEA Suborder MYSTICETI BALAENIDAE Eubalaena Glacialis (Müller, 1776) EUG En - Northern Right Whale; Fr - Baleine De Biscaye; Sp - Ballena Franca
click for previous page Cetacea 2041 Order CETACEA Suborder MYSTICETI BALAENIDAE Eubalaena glacialis (Müller, 1776) EUG En - Northern right whale; Fr - Baleine de Biscaye; Sp - Ballena franca. Adults common to 17 m, maximum to 18 m long.Body rotund with head to 1/3 of total length;no pleats in throat; dorsal fin absent. Mostly black or dark brown, may have white splotches on chin and belly.Commonly travel in groups of less than 12 in shallow water regions. IUCN Status: Endangered. BALAENOPTERIDAE Balaenoptera acutorostrata Lacepède, 1804 MIW En - Minke whale; Fr - Petit rorqual; Sp - Rorcual enano. Adult males maximum to slightly over 9 m long, females to 10.7 m.Head extremely pointed with prominent me- dian ridge. Body dark grey to black dorsally and white ventrally with streaks and lobes of intermediate shades along sides.Commonly travel singly or in groups of 2 or 3 in coastal and shore areas;may be found in groups of several hundred on feeding grounds. IUCN Status: Lower risk, near threatened. Balaenoptera borealis Lesson, 1828 SIW En - Sei whale; Fr - Rorqual de Rudolphi; Sp - Rorcual del norte. Adults to 18 m long. Typical rorqual body shape; dorsal fin tall and strongly curved, rises at a steep angle from back.Colour of body is mostly dark grey or blue-grey with a whitish area on belly and ventral pleats.Commonly travel in groups of 2 to 5 in open ocean waters. IUCN Status: Endangered. 2042 Marine Mammals Balaenoptera edeni Anderson, 1878 BRW En - Bryde’s whale; Fr - Rorqual de Bryde; Sp - Rorcual tropical. -
Chlorinated Organic Contaminants in Blubber Biopsies from Northwestern Atlantic Balaenopterid Whales Summering in the Gulf of St Lawrence
Marine Environmental Research, Vol. 44, No. 2, pp. 201-223, 1997 0 1997 Elsevier Science Ltd All rights reserved. Printed in Great Britain PII: SOl41-1136(97)00004-4 0141-1136/97 $17.00+0.00 Chlorinated Organic Contaminants in Blubber Biopsies from Northwestern Atlantic Balaenopterid Whales Summering in the Gulf of St Lawrence J. M. Gauthier,a* C. D. Metcalfe” & R. Sear@ “Environmental and Resources Studies, Trent University, Peterborough, Ontario, Canada K9J 7B8 bMingan Island Cetacean Study (MICS), 285 Green, St. Lambert, Quebec, Canada J4P IT3 (Received 16 May 1996; revised version received 16 December 1996; accepted 29 December 1996. Published June 1997) ABSTRACT Concentrations and patterns of chlorinated biphenyls (CBS) and other persistent organochlorine compounds (OCs) were determined from small blubber biopsy samples collected from northwestern Atlantic minke (Balaenoptera acuros- trata) , fin (Balaenoptera physalus), blue (Balaenoptera musculus) , and humpback (Megaptera novaeangliae) whales summering in the Gurf of St. Lawrence, Quebec. Concentrations of CPCB (sum of 19 congeners) in biopsy samples ranged from 0.2-10 pg g-’ lipid, and congeners 52, 101, 118, 153, 138 and 180 accounted for 79% of CPCB. Mean concentration of the sum of non- ortho CB congeners in selected biopsy samples was 2 ng g-t lipid, and relative concentrations of these analytes were: 77 > 126 > 81> 169. Concentrations of XDDT ranged from 0.613 pg g-t lipid, and the average proportion of DDE to CDDT was 72%. All other organochlorine analytes were present at concentra- tions below 2 pg g-t lipid. On average, cis-nonachlor, trans-nonachlor and oxy- chlordane accounted for 27, 26 and 23%, respectively, of the chlordane-related analytes, and cl-hexachlorocyclohexane (HCH) comprised 67% of XHCH. -
Lunge Filter Feeding Biomechanics Constrain Rorqual Foraging Ecology Across Scale S
© 2020. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2020) 223, jeb224196. doi:10.1242/jeb.224196 RESEARCH ARTICLE Lunge filter feeding biomechanics constrain rorqual foraging ecology across scale S. R. Kahane-Rapport1,*, M. S. Savoca1, D. E. Cade1,2, P. S. Segre1, K. C. Bierlich3, J. Calambokidis4, J. Dale3, J. A. Fahlbusch1, A. S. Friedlaender2, D. W. Johnston3, A. J. Werth5 and J. A. Goldbogen1 ABSTRACT morphological scaling (Haldane, 1926), resulting in functional Fundamental scaling relationships influence the physiology of vital trade-offs that ultimately impact evolution and ecology. rates, which in turn shape the ecology and evolution of organisms. For The physiological advantages and disadvantages associated with diving mammals, benefits conferred by large body size include different body sizes have wide-ranging effects, from behavior to life reduced transport costs and enhanced breath-holding capacity, history. For example, the smallest animals have the lowest absolute thereby increasing overall foraging efficiency. Rorqual whales feed energetic demands (Kelt and Van Vuren, 1999), yet they may also by engulfing a large mass of prey-laden water at high speed and struggle with thermoregulation and be forced to compensate by filtering it through baleen plates. However, as engulfment capacity increasing their metabolism (Scholander et al., 1950; Taylor et al., increases with body length (engulfment volume∝body length3.57), the 1980). Small size enables high performance maneuverability and surface area of the baleen filter does not increase proportionally agility (Domenici, 2001), but may limit maximum attainable speeds (baleen area∝body length1.82), and thus the filtration time of larger (Carrier, 1994; Hirt et al., 2017). -
A Brief Review of the Genetic Studies on Dwarf Minke Whale Based on Jarpa Samples
SC/D06/J8 A BRIEF REVIEW OF THE GENETIC STUDIES ON DWARF MINKE WHALE BASED ON JARPA SAMPLES Luis A. Pastene Institute of Cetacean Research, Toyomi-cho 4-5, Chuo-ku, Tokyo 104-0055, Japan ABSTRACT Prior to the JARPA surveys ‘dwarf’ minke whales were only believed to be found between 7-41°S. However the locality of the JARPA catches in Areas IV and V was mainly between 55-62°S (one animal was caught at 65°S), showing that the ‘dwarf’ minke whale is found much further south than shown by the previous data. A total of 16 ‘dwarf’ minke whales were sampled by JARPA and these animals were examined genetically with the purpose to investigate their relationship to the southern ‘ordinary’ minke whale and to minke whales in the Northern Hemisphere. Early studies showed that the degree of mtDNA divergence between both southern minke whales was large and similar to that found between southern ‘ordinary’ minke whale and Northern Hemisphere minke whales. Phylogenetic analyses showed that the ‘dwarf’ minke whale was more closely related to Northern Hemisphere minke whales. In 1993 the Scientific Committee recommended the inclusion of the ‘dwarf’ minke whale in the Schedule, so that catch limits for Antarctic minke whales recognise the distinction between the two southern minke whales. The genetic analysis conducted using JARPA samples of the southern ‘ordinary’ and ‘dwarf’ minke whales assisted greatly to the taxonomic review of minke whale conducted by Rice (1998), which confirmed the existence of two species, the larger, Antarctic minke whale Balaenoptera bonaerensis confined to the Southern Hemisphere, and the smaller, common minke whale B. -
Ilulissat Icefjord
World Heritage Scanned Nomination File Name: 1149.pdf UNESCO Region: EUROPE AND NORTH AMERICA __________________________________________________________________________________________________ SITE NAME: Ilulissat Icefjord DATE OF INSCRIPTION: 7th July 2004 STATE PARTY: DENMARK CRITERIA: N (i) (iii) DECISION OF THE WORLD HERITAGE COMMITTEE: Excerpt from the Report of the 28th Session of the World Heritage Committee Criterion (i): The Ilulissat Icefjord is an outstanding example of a stage in the Earth’s history: the last ice age of the Quaternary Period. The ice-stream is one of the fastest (19m per day) and most active in the world. Its annual calving of over 35 cu. km of ice accounts for 10% of the production of all Greenland calf ice, more than any other glacier outside Antarctica. The glacier has been the object of scientific attention for 250 years and, along with its relative ease of accessibility, has significantly added to the understanding of ice-cap glaciology, climate change and related geomorphic processes. Criterion (iii): The combination of a huge ice sheet and a fast moving glacial ice-stream calving into a fjord covered by icebergs is a phenomenon only seen in Greenland and Antarctica. Ilulissat offers both scientists and visitors easy access for close view of the calving glacier front as it cascades down from the ice sheet and into the ice-choked fjord. The wild and highly scenic combination of rock, ice and sea, along with the dramatic sounds produced by the moving ice, combine to present a memorable natural spectacle. BRIEF DESCRIPTIONS Located on the west coast of Greenland, 250-km north of the Arctic Circle, Greenland’s Ilulissat Icefjord (40,240-ha) is the sea mouth of Sermeq Kujalleq, one of the few glaciers through which the Greenland ice cap reaches the sea. -
Exceptional 20Th Century Glaciological Regime of a Major SE Greenland Outlet Glacier Received: 18 January 2017 Camilla S
www.nature.com/scientificreports OPEN Exceptional 20th century glaciological regime of a major SE Greenland outlet glacier Received: 18 January 2017 Camilla S. Andresen1, Ulla Kokfelt1, Marie-Alexandrine Sicre2, Mads Faurschou Knudsen3, Accepted: 21 September 2017 Laurence M. Dyke1, Vincent Klein2, Fanny Kaczmar2, Martin W. Miles4,5 & David Wangner1 Published: xx xx xxxx The early 2000s accelerated ice-mass loss from large outlet glaciers in W and SE Greenland has been linked to warming of the subpolar North Atlantic. To investigate the uniqueness of this event, we extend the record of glacier and ocean changes back 1700 years by analyzing a sediment core from Sermilik Fjord near Helheim Glacier in SE Greenland. We show that multidecadal to centennial increases in alkenone-inferred Atlantic Water SSTs on the shelf occurred at times of reduced solar activity during the Little Ice Age, when the subpolar gyre weakened and shifted westward promoted by atmospheric blocking events. Helheim Glacier responded to many of these episodes with increased calving, but despite earlier multidecadal warming episodes matching the 20th century high SSTs in magnitude, the glacier behaved diferently during the 20th century. We suggest the presence of a foating ice tongue since at least 300 AD lasting until 1900 AD followed by elevated 20th century glacier calving due to the loss of the tongue. We attribute this regime shift to 20th century unprecedented low sea-ice occurrence in the East Greenland Current and conclude that properties of this current are important for the stability of the present ice tongues in NE Greenland. In the last two decades there has been a rapid increase in the loss of ice from the Greenland Ice Sheet1. -
Fall Feeding Aggregations of Fin Whales Off Elephant Island (Antarctica)
SC/64/SH9 Fall feeding aggregations of fin whales off Elephant Island (Antarctica) BURKHARDT, ELKE* AND LANFREDI, CATERINA ** * Alfred Wegener Institute for Polar and Marine research, Am Alten Hafen 26, 256678 Bremerhaven, Germany ** Politecnico di Milano, University of Technology, DIIAR Environmental Engineering Division Pza Leonardo da Vinci 32, 20133 Milano, Italy Abstract From 13 March to 09 April 2012 Germany conducted a fisheries survey on board RV Polarstern in the Scotia Sea (Elephant Island - South Shetland Island - Joinville Island area) under the auspices of CCAMLR. During this expedition, ANT-XXVIII/4, an opportunistic marine mammal survey was carried out. Data were collected for 26 days along the externally preset cruise track, resulting in 295 hrs on effort. Within the study area 248 sightings were collected, including three different species of baleen whales, fin whale (Balaenoptera physalus), humpback whale ( Megaptera novaeangliae ), and Antarctic minke whale (Balaenoptera bonaerensis ) and one toothed whale species, killer whale ( Orcinus orca ). More than 62% of the sightings recorded were fin whales (155 sightings) which were mainly related to the Elephant Island area (116 sightings). Usual group sizes of the total fin whale sightings ranged from one to five individuals, also including young animals associated with adults during some encounters. Larger groups of more than 20 whales, and on two occasions more than 100 individuals, were observed as well. These large pods of fin whales were observed feeding in shallow waters (< 300 m) on the north-western shelf off Elephant Island, concordant with large aggregations of Antarctic krill ( Euphausia superba ). This observation suggests that Elephant Island constitutes an important feeding area for fin whales in early austral fall, with possible implications regarding the regulation of (krill) fisheries in this area. -
Natural Resources in the Nanortalik District
National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 2001 Christain M. Glahder Department of Arctic Environment Data sheet Title: Natural resources in the Nanortalik district Subtitle: An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Arktisk Miljø – Arctic Environment. Author: Christian M. Glahder Department: Department of Arctic Environment Serial title and no.: NERI Technical Report No. 384 Publisher: Ministry of Environment National Environmental Research Institute URL: http://www.dmu.dk Date of publication: December 2001 Referee: Peter Aastrup Greenlandic summary: Hans Kristian Olsen Photos & Figures: Christian M. Glahder Please cite as: Glahder, C. M. 2001. Natural resources in the Nanortalik district. An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Na- tional Environmental Research Institute, Technical Report No. 384: 81 pp. Reproduction is permitted, provided the source is explicitly acknowledged. Abstract: The interview study was performed in the Nanortalik municipality, South Green- land, during March-April 2001. It is a part of an environmental baseline study done in relation to the Nalunaq gold project. 23 fishermen, hunters and others gave infor- mation on 11 fish species, Snow crap, Deep-sea prawn, five seal species, Polar bear, Minke whale and two bird species; moreover on gathering of mussels, seaweed etc., sheep farms, tourist localities and areas for recreation. -
Whale Watching New South Wales Australia
Whale Watching New South Wales Australia Including • About Whales • Humpback Whales • Whale Migration • Southern Right Whales • Whale Life Cycle • Blue Whales • Whales in Sydney Harbour • Minke Whales • Aboriginal People & Whales • Dolphins • Typical Whale Behaviour • Orcas • Whale Species • Other Whale Species • Whales in Australia • Other Marine Species About Whales The whale species you are most likely to see along the New South Wales Coastline are • Humpback Whale • Southern Right Whale Throughout June and July Humpback Whales head north for breading before return south with their calves from September to November. Other whale species you may see include: • Minke Whale • Blue Whale • Sei Whale • Fin Whale • False Killer Whale • Orca or Killer Whale • Sperm Whale • Pygmy Right Whale • Pygmy Sperm Whale • Bryde’s Whale Oceans cover about 70% of the Earth’s surface and this vast environment is home to some of the Earth’s most fascinating creatures: whales. Whales are complex, often highly social and intelligent creatures. They are mammals like us. They breath air, have hair on their bodies (though only very little), give birth to live young and suckle their calves through mammary glands. But unlike us, whales are perfectly adapted to the marine environment with strong, muscular and streamlined bodies insulated by thick layers of blubber to keep them warm. Whales are gentle animals that have graced the planet for over 50 million years and are present in all oceans of the world. They capture our imagination like few other animals. The largest species of whales were hunted almost to extinction in the last few hundred years and have survived only thanks to conservation and protection efforts. -
Measures Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 1
MEaSURES Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 1 USER GUIDE How to Cite These Data As a condition of using these data, you must include a citation: Howat, I. 2016. MEaSURES Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 1. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. https://doi.org/10.5067/EYV1IP7MUNSV. [Date Accessed]. FOR QUESTIONS ABOUT THESE DATA, CONTACT [email protected] FOR CURRENT INFORMATION, VISIT https://nsidc.org/data/nsidc-0646 USER GUIDE: MEaSURES Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 1 TABLE OF CONTENTS 1 DATA DESCRIPTION ................................................................................................................. 2 1.1 Parameters ............................................................................................................................................ 2 1.1.1 Parameter Description ................................................................................................................. 2 1.2 File Information ...................................................................................................................................... 2 1.2.1 Format.......................................................................................................................................... 2 1.2.2 Directory Structure ......................................................................................................................