The West Greenland Shelf
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Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
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. -
Automated Iceberg Detection Using Landsat: Method and Example Application in Disko Bay, West Greenland
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-73 Manuscript under review for journal The Cryosphere Discussion started: 8 May 2018 c Author(s) 2018. CC BY 4.0 License. Automated iceberg detection using Landsat: method and example application in Disko Bay, west Greenland 1,2 1,2 a,b, Jessica Scheick , Ellyn M. Enderlin , and Gordon Hamilton † 1School of Earth and Climate Sciences, University of Maine, Orono, ME, USA 2Climate Change Institute, University of Maine, Orono, ME, USA aformerly at: School of Earth and Climate Sciences, University of Maine, Orono, ME, USA bformerly at: Climate Change Institute, University of Maine, Orono, ME, USA †deceased Correspondence: Jessica Scheick ([email protected]) Abstract. Over the last two decades, the flux of icebergs into Greenland’s fjords and coastal waters has increased, concurrent with changes in mass loss and dynamics of Greenland’s marine-terminating outlet glaciers. Icebergs impact fjord circulation and stratification, freshwater flux, and ecosystem structure and pose a hazard to marine navigation and infrastructure, yet they remain a relatively understudied component of the ice–ocean system. Icebergs are easily detected in optical satellite imagery, 5 but manual analysis to derive an iceberg size distribution time series is time prohibitive and partially cloudy scenes pose a challenge to automated analysis. Here we present a novel, computationally simple machine learning-based cloud mask for Landsat 7 and 8. This mask is incorporated into a larger iceberg delineation algorithm that allows us to extract iceberg size distributions, including outlines of individual icebergs, for cloud-free and partially cloud-covered Landsat scenes. -
Pinngortitaleriffik Grønlands Naturinstitut Grønlands ■ ■ ■
PINNGORTITALERIFFIK ■ GRØNLANDS NATURINSTITUT ÅRSBERETNING Årsberetning 2008 2008 INDHOLD ÅRSBERETNING Forord ......................................................................................................................... 3 Fagligt arbejde ........................................................................................................... 4 Center for Marinøkologi og Klimaeffekter .............................................................. 4 Afdelingen for Fisk og Rejer ................................................................................. 11 2008 Afdelingen for Pattedyr og Fugle.......................................................................... 14 Informationssekretariatet ..................................................................................... 22 Pinngortitaleriffiks rammer ..................................................................................... 23 Formål, arbejdsopgaver og organisation .............................................................. 23 Finansiering ........................................................................................................... 24 Fysiske rammer ..................................................................................................... 26 Personale ............................................................................................................... 27 Aktiviteter i 2008 ...................................................................................................... 30 Pinngortitaleriffik ■ Grønlands Naturinstitut -
Maphab - Mapping Benthic Habitats in Greenland
MapHab - Mapping Benthic Habitats in Greenland pilot study in Disko Bay Technical report no. 109 GREENLAND INSTITUTE OF NATURAL RESOURCES GEOLOGICAL SURVEY OF DENMARK AND GREENLAND NATIONAL INSTITUTE OF AQUATIC RESOURCES INSTITUTE OF ZOOLOGY 1 Title: MapHab – Mapping Benthic Habitats in Greenland – pilot study in Disko Bay. Project PI: Diana W. Krawczyk & Malene Simon Project consortium: Greenland Institute of Natural Resources (GINR) Geological Survey of Denmark and Greenland (GEUS) Institute of Zoology (IoZ) Institute for Aquatic Resources (DTU Aqua) Author(s): Diana W. Krawczyk, Jørn Bo Jensen, Zyad Al-Hamdani, Chris Yesson, Flemming Hansen, Martin E. Blicher, Nanette H. Ar- boe, Karl Zinglersen, Jukka Wagnholt, Karen Edelvang, Ma- lene Simon ISBN; EAN; ISSN: 87-91214-87-4; 9788791214875 109; 1397-3657 Reference/Citation: Krawczyk et al. (2019) MapHab – Mapping Benthic Habitats in Greenland – pilot study in Disko Bay. Tech- nical report no. 109, Greenland Institute of Natural Resources, Greenland. ISBN 87-91214-87-4, 73 pp. Publisher: Greenland Institute of Natural Resources PO Box 570 3900 Nuuk Greenland Contact: Tel: +299 361200 Email: [email protected] Web: www.natur.gl Web: www.gcrc.gl Web: https://gcrc.gl/research-programs/greenland- benthic-habitats/ Date of publication: 2019 Financial support: The MapHab project was funded by the GINR, the Miljøstøtte til Arktis (Dancea), the Aage V. Jensens fonde and the Ministry of Research in Greenland (IKIIN) 2 Content 1. Introduction ......................................................................................... -
The East Greenland Current North of Denmark Strait: Part I'
The East Greenland Current North of Denmark Strait: Part I' K. AAGAARD AND L. K. COACHMAN2 ABSTRACT.Current measurements within the East Greenland Current during winter1965 showed that above thecontinental slope there were large on-shore components of flow, probably representing a westward Ekman transport. The speed did not decrease significantly with depth, indicatingthat the barotropic mode domi- nates the flow. Typical current speeds were10 to 15 cm. sec.-l. The transport of the current during winter exceeds 35 x 106 m.3 sec-1. This is an order of magnitude greater than previous estimates and, although there may be seasonal fluctuations in the transport, it suggests that the East Greenland Current primarily represents a circulation internal to the Greenland and Norwegian seas, rather than outflow from the central Polarbasin. RESUME. Lecourant du Groenland oriental au nord du dbtroit de Danemark. Aucours de l'hiver de 1965, des mesures effectukes danslecourant du Groenland oriental ont montr6 que sur le talus continental, la circulation comporte d'importantes composantes dirigkes vers le rivage, ce qui reprksente probablement un flux vers l'ouest selon le mouvement #Ekman. La vitesse ne diminue pas beau- coup avec laprofondeur, ce qui indique que le mode barotropique domine la circulation. Les vitesses typiques du courant sont de 10 B 15 cm/s-1. Au cows de l'hiver, le debit du courant dkpasse 35 x 106 m3/s-1. Cet ordre de grandeur dkpasse les anciennes estimations et, malgrC les fluctuations saisonnihres possibles, il semble que le courant du Groenland oriental correspond surtout B une circulation interne des mers du Groenland et de Norvhge, plut6t qu'8 un Bmissaire du bassin polaire central. -
Pdf Dokument
Udskriftsdato: 2. oktober 2021 BEK nr 517 af 23/05/2018 (Historisk) Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland Ministerium: Social og Indenrigsministeriet Journalnummer: Økonomi og Indenrigsmin., j.nr. 20175132 Senere ændringer til forskriften LBK nr 916 af 28/06/2018 Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland I medfør af § 8, stk. 1, i lov om folketingsvalg i Grønland, jf. lovbekendtgørelse nr. 255 af 28. april 1999, fastsættes: § 1. Fortegnelsen over valgkredse i Grønland affattes som angivet i bilag 1 til denne bekendtgørelse. § 2. Bekendtgørelsen træder i kraft den 1. juni 2018. Stk. 2. Bekendtgørelse nr. 476 af 17. maj 2011 om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland, ophæves. Økonomi- og Indenrigsministeriet, den 23. maj 2018 Simon Emil Ammitzbøll-Bille / Christine Boeskov BEK nr 517 af 23/05/2018 1 Bilag 1 Ilanngussaq Fortegnelse over valgkredse i hver kommune Kommuneni tamani qinersivinnut nalunaarsuut Kommune Valgkredse i Valgstedet eller Valgkredsens område hver kommune afstemningsdistrikt (Tilknyttede bosteder) (Valgdistrikt) (Afstemningssted) Kommune Nanortalik 1 Nanortalik Nanortalik Kujalleq 2 Aappilattoq (Kuj) Aappilattoq (Kuj) Ikerasassuaq 3 Narsaq Kujalleq Narsaq Kujalleq 4 Tasiusaq (Kuj) Tasiusaq (Kuj) Nuugaarsuk Saputit Saputit Tasia 5 Ammassivik Ammassivik Qallimiut Qorlortorsuaq 6 Alluitsup Paa Alluitsup Paa Alluitsoq Qaqortoq -
Geological Survey of Denmark and Greenland Bulletin 11, 87-99
Zircon geochronology from the Kangaatsiaq– Qasigiannguit region, the northern part of the 1.9–1.8 Ga Nagssugtoqidian orogen, West Greenland Kristine Thrane and James N. Connelly The Kangaatsiaq–Qasigiannguit region in the northern part of the Palaeoproterozoic Nagssugto- qidian orogen of West Greenland consists of poly-deformed orthogneisses and minor occurrences of interleaved, discontinuous supracrustal belts. Laser ablation ICP-MS 207Pb/206Pb analyses of detrital zircons from four metasedimentary rocks (supplemented by ion probe analysis of one sample) and igneous zircons from six granitoid rocks cutting metasedimentary units indicate that the supracrustal rocks in the Kangaatsiaq–Qasigiannguit (Christianshåb) region are predominantly Archaean in age. Four occurrences of metasedimentary rocks are clearly Archaean, two have equivocal ages, and only one metasedimentary unit, from within the Naternaq (Lersletten) supracrustal belt, is demonstrably Palaeoproterozoic and readily defines a large fold complex of this age at Naternaq. The 2.9–2.8 Ga ages of detrital Archaean grains are compatible with derivation from the local basement orthogneisses within the Nagssugtoqidian orogen. The detrital age patterns are similar to those of metasediments within the central Nagssugtoqidian orogen but distinct from age patterns in metasediments of the Rinkian belt to the north, where there is an additional component of pre-2.9 Ga zircons. Synkine- matic intrusive granitoid rocks constrain the ages of some Archaean deformation at 2748 ± 19 Ma and some -
[BA] COUNTRY [BA] SECTION [Ba] Greenland
[ba] Validity date from [BA] COUNTRY [ba] Greenland 26/08/2013 00081 [BA] SECTION [ba] Date of publication 13/08/2013 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 153 Qaqqatisiaq (Royal Greenland Seagfood A/S) Nuuk Vestgronland [ba] FV 219 Markus (Qajaq Trawl A/S) Nuuk Vestgronland [ba] FV 390 Polar Princess (Polar Seafood Greenland A/S) Qeqertarsuaq Vestgronland [ba] FV 401 Polar Qaasiut (Polar Seafood Greenland A/S) Nuuk Vestgronland [ba] FV 425 Sisimiut (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4406 Nataarnaq (Ice Trawl A/S) Nuuk Vestgronland [ba] FV 4432 Qeqertaq Fish ApS Ilulissat Vestgronland [ba] PP 4469 Akamalik (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4502 Regina C (Niisa Trawl ApS) Nuuk Vestgronland [ba] FV 4574 Uummannaq Seafood A/S Uummannaq Vestgronland [ba] PP 4615 Polar Raajat A/S Nuuk Vestgronland [ba] CS 4659 Greenland Properties A/S Maniitsoq Vestgronland [ba] PP 4660 Arctic Green Food A/S Aasiaat Vestgronland [ba] PP 4681 Sisimiut Fish ApS Sisimiut Vestgronland [ba] PP 4691 Ice Fjord Fish ApS Nuuk Vestgronland [ba] PP 1 / 5 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 4766 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4768 Royal Greenland Seafood A/S Qeqertarsuaq Vestgronland [ba] PP 4804 ONC-Polar A/S Alluitsup Paa Vestgronland [ba] PP 481 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4844 Polar Nanoq (Sigguk A/S) Nuuk Vestgronland -
Holocene Environmental Changes and Climate Development in Greenland
R-10-65 Holocene environmental changes and climate development in Greenland Stefan Engels, Karin Helmens Stockholm University December 2010 Svensk Kärnbränslehantering AB Swedish Nuclear Fuel and Waste Management Co Box 250, SE-101 24 Stockholm Phone +46 8 459 84 00 CM Gruppen AB, Bromma, 2010 CM Gruppen ISSN 1402-3091 Tänd ett lager: SKB R-10-65 P, R eller TR. Holocene environmental changes and climate development in Greenland Stefan Engels, Karin Helmens Stockholm University December 2010 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the authors. SKB may draw modified conclusions, based on additional literature sources and/or expert opinions. A pdf version of this document can be downloaded from www.skb.se. Contents 1 Introduction 5 1.1 Aims and framework 5 1.2 Present-day climatical and biogeographical trends in Greenland 5 1.3 Geology of Greenland 7 2 Late Pleistocene and Early Holocene deglaciation in Greenland 9 2.1 Deglaciation in East Greenland 9 2.2 Deglaciation in West Greenland 11 2.3 Deglaciation in South Greenland 13 2.4 Holocene ice sheet variability 13 3 Holocene climate variability and vegetation development in Greenland 15 3.1 Terrestrial records from East Greenland 15 3.2 Terrestrial records from West Greenland 18 3.3 Terrestrial records from South Greenland 23 3.4 Terrestrial records from North Greenland 25 3.5 Ice-core records 25 3.6 Records from the marine realm 28 4 Training sets and the transfer-function approach 29 4.1 General 29 4.2 Training set development in Greenland 30 5 The period directly after deglaciation 33 5.1 Terrestrial plants and animals 33 5.2 Aquatic plants and animals (lacustrine) 33 6 Summary and concluding remarks 35 References 37 R-10-65 3 1 Introduction 1.1 Aims and framework The primary aim of this report is to give an overview of the Holocene environmental and climatic changes in Greenland and to describe the development of the periglacial environment during the Holocene. -
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. -
Boreal Marine Fauna from the Barents Sea Disperse to Arctic Northeast Greenland
bioRxiv preprint doi: https://doi.org/10.1101/394346; this version posted December 16, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Boreal marine fauna from the Barents Sea disperse to Arctic Northeast Greenland Adam J. Andrews1,2*, Jørgen S. Christiansen2, Shripathi Bhat1, Arve Lynghammar1, Jon-Ivar Westgaard3, Christophe Pampoulie4, Kim Præbel1* 1The Norwegian College of Fishery Science, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Norway 2Department of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Norway 3Institute of Marine Research, Tromsø, Norway 4Marine and Freshwater Research Institute, Reykjavik, Iceland *Authors to whom correspondence should be addressed, e-mail: [email protected], kim.præ[email protected] Keywords: Atlantic cod, Barents Sea, population genetics, dispersal routes. As a result of ocean warming, the species composition of the Arctic seas has begun to shift in a boreal direction. One ecosystem prone to fauna shifts is the Northeast Greenland shelf. The dispersal route taken by boreal fauna to this area is, however, not known. This knowledge is essential to predict to what extent boreal biota will colonise Arctic habitats. Using population genetics, we show that Atlantic cod (Gadus morhua), beaked redfish (Sebastes mentella), and deep-sea shrimp (Pandalus borealis) specimens recently found on the Northeast Greenland shelf originate from the Barents Sea, and suggest that pelagic offspring were dispersed via advection across the Fram Strait. Our results indicate that boreal invasions of Arctic habitats can be driven by advection, and that the fauna of the Barents Sea can project into adjacent habitats with the potential to colonise putatively isolated Arctic ecosystems such as Northeast Greenland.