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FORSYNINGSNIVEAUET I DAG OG I FREMTIDEN Pilersuisoq Savissivik Indbyggere: 62
FORSYNINGSNIVEAUET I DAG OG I FREMTIDEN Pilersuisoq Savissivik Indbyggere: 62 • 66 butikker • Duty-Free i Kangerlussuaq • www.pisisa.gl • 550 ansatte • Pakhuse • Servicekontrakt med Selvstyret • 36 mio. kr. i årligt tilskud • Min. åbningstider • Min. sortiment • www.pisisa.gl Serviceniveau aftalt med Selvstyret Kategori Indbyggere Åbningstid Faktisk åbningstid Basissortiment Faktisk sortiment* Depot 1-29 Min. 2 timer/uge Min. 17 timer/uge 146 357 Kiosk 30-75 Min. 10 timer/uge Min. 17 timer/uge 236 483 Servicebutik 76-120 Min. 20 timer/uge Min. 22 timer/uge 294 506 Bygdebutik 121-600 Min. 20 timer/uge Min. 30 timer/uge 340 1466 Kommerciel butik 601- Fri Min. 60 timer/uge Fri 6778 *KNI råder over 13.887 varenr. som butikkerne kan trække på. • Pilersuisoq varetager udover detailhandel en række services på vegne af myndigheder og virksomheder i Grønland • Årligt overskud på 40-50 mio. kr. • Investeres i nedbringelse af renoveringsefterslæb på 300 mio. kr. • Investeringer øges fra 35-70 mio. kr./år • Vækst – f.eks. ny jagt/fiskeri butik i Tasiusaq i 2018 Budgetår 2017/18 Ikerasak Ilimanaq Isertoq Narsarmijit Nuugaatsiaq Tasiusaq – (Nanortalik) Akunnaaq Ilulissat Tasiusaq – (Upernavik) Aappilattoq (Upernavik) Innaarsuit Upernavik Uummannaq Tasiilaq Budgetår 2018/19 Budgetår 2019/20 Kitsissuarsuit Ikamiut Kuummiut Illorsuit • Årligt overskud på 40-50 mio. kr. Qeqertat Kangersuatsiaq Saarloq Kulusuk • Investeres i nedbringelse af Aappilattoq (Upernavik) Napasoq renoveringsefterslæb på 300 mio. Ikerasak Qeqertarsuatsiaat Nuugaatsiaq Maniitsoq kr. -
Greenland HAZARD SCENARIO SIMULATIONS and 2017 EVENT HINDCAST
REPORT Tsunami hazard screening for the Uummannaq fjord system - Greenland HAZARD SCENARIO SIMULATIONS AND 2017 EVENT HINDCAST DOC.NO. 20200823-01-R REV.NO. 0 / 2021-03-26 Neither the confidentiality nor the integrity of this document can be guaranteed following electronic transmission. The addressee should consider this risk and take full responsibility for use of this document. This document shall not be used in parts, or for other purposes than the document was prepared for. The document shall not be copied, in parts or in whole, or be given to a third party without the owner’s consent. No changes to the document shall be made without consent from NGI. Ved elektronisk overføring kan ikke konfidensialiteten eller autentisiteten av dette dokumentet garanteres. Adressaten bør vurdere denne risikoen og ta fullt ansvar for bruk av dette dokumentet. Dokumentet skal ikke benyttes i utdrag eller til andre formål enn det dokumentet omhandler. Dokumentet må ikke reproduseres eller leveres til tredjemann uten eiers samtykke. Dokumentet må ikke endres uten samtykke fra NGI. Project Project title: Tsunami hazard screening for the Uummannaq fjord system - Greenland Document title: Hazard scenario simulations and 2017 event hindcast Document no.: 20200823-01-R Date: 2021-03-26 Revision no. /rev. date: 0 / Client Client: GEUS - De nationale geologiske undersøgelser for Danmark og Grønland Client contact person: Jens Jørgen Møller Contract reference: Proposal with CTR's 1-2 signed 2/12-2020, signed CTR3 for NGI Project manager: Finn Løvholt Prepared by: Finn Løvholt Reviewed by: Sylfest Glimsdal and Carl Harbitz NORWEGIAN GEOTECHNICAL INSTITUTE Main office Trondheim office T 22 02 30 00 BIC NO. -
The Necessity of Close Collaboration 1 2 the Necessity of Close Collaboration the Necessity of Close Collaboration
The Necessity of Close Collaboration 1 2 The Necessity of Close Collaboration The Necessity of Close Collaboration 2017 National Spatial Planning Report 2017 autumn assembly Ministry of Finances and Taxes November 2017 The Necessity of Close Collaboration 3 The Necessity of Close Collaboration 2017 National Spatial Planning Report Ministry of Finances and Taxes Government of Greenland November 2017 Photos: Jason King, page 5 Bent Petersen, page 6, 113 Leiff Josefsen, page 12, 30, 74, 89 Bent Petersen, page 11, 16, 44 Helle Nørregaard, page 19, 34, 48 ,54, 110 Klaus Georg Hansen, page 24, 67, 76 Translation from Danish to English: Tuluttut Translations Paul Cohen [email protected] Layout: allu design Monika Brune www.allu.gl Printing: Nuuk Offset, Nuuk 4 The Necessity of Close Collaboration Contents Foreword . .7 Chapter 1 1.0 Aspects of Economic and Physical Planning . .9 1.1 Construction – Distribution of Public Construction Funds . .10 1.2 Labor Market – Localization of Public Jobs . .25 1.3 Demographics – Examining Migration Patterns and Causes . 35 Chapter 2 2.0 Tools to Secure a Balanced Development . .55 2.1 Community Profiles – Enhancing Comparability . .56 2.2 Sector Planning – Enhancing Coordination, Prioritization and Cooperation . 77 Chapter 3 3.0 Basic Tools to Secure Transparency . .89 3.1 Geodata – for Structure . .90 3.2 Baseline Data – for Systematization . .96 3.3 NunaGIS – for an Overview . .101 Chapter 4 4.0 Summary . 109 Appendixes . 111 The Necessity of Close Collaboration 5 6 The Necessity of Close Collaboration Foreword A well-functioning public adminis- by the Government of Greenland. trative system is a prerequisite for a Hence, the reports serve to enhance modern democratic society. -
Trafikopgave 1 Qaanaq Distrikt 2011 2012 2013 2014 Passagerer 1168
Trafikopgave 1 Qaanaq distrikt 2011 2012 2013 2014 Passagerer 1168 1131 1188 934 Post i kg 12011 9668 1826 10661 Fragt i kg 37832 29605 28105 41559 Trafikopgave 2 Upernavik distrikt 2011 2012 2013 2014 Passagerer 4571 4882 5295 4455 Post i kg 22405 117272 19335 39810 Fragt i kg 37779 32905 32338 39810 Trafikopgave 3 Uumannaq distrikt 2011 2012 2013 2014 Passagerer 10395 9321 10792 9467 Post i kg 38191 34973 36797 37837 Fragt i kg 72556 56129 75480 54168 Trafikopgave 5 Disko distrikt, vinter 2011 2012 2013 2014 Passagerer 5961 7161 6412 6312 Post i kg 23851 28436 22060 23676 Fragt i kg 24190 42560 32221 29508 Trafikopgave 7 Sydgrønland distrikt 2011 2012 2013 2014 Passagerer 39546 43908 27104 30135 Post i kg 115245 107713 86804 93497 Fragt i kg 232661 227371 159999 154558 Trafikopgave 8 Tasiilaq distrikt 2011 2012 2013 2014 Passagerer 12919 12237 12585 11846 Post i kg 50023 57163 45005 43717 Fragt i kg 93034 115623 105175 103863 Trafikopgave 9 Ittoqqortoormiit distrikt 2011 2012 2013 2014 Passagerer 1472 1794 1331 1459 Post i kg 10574 10578 9143 9028 Fragt i kg 29097 24840 12418 15181 Trafikopgave 10 Helårlig beflyvning af Qaanaaq fra Upernavik 2011 2012 2013 2014 Passagerer 1966 1246 2041 1528 Post i kg 22070 11465 20512 14702 Fragt i kg 44389 18489 43592 20786 Trafikopgave 11 Helårlig beflyvning af Nerlerit Inaat fra Island Nedenstående tal er for strækningen Kulusuk - Nerlerit Inaat baseret på en trekantflyvning Nuuk-Kulusuk-Nerlerit Inaat' 2011 2012 2013 2014 Passagerer 4326 4206 1307 1138 Post i kg 21671 19901 9382 5834 Fragt i kg -
Kitaa Kujataa Avanersuaq Tunu Kitaa
Oodaap Qeqertaa (Oodaaq(Oodaaq Island) Ø) KapCape Morris Morris Jesup Jesup D AN L Nansen Land N IAD ATN rd LS Fjio I Freuchen PEARY LAND ce NR den IAH Land pen Ukioq kaajallallugu / Year-round nde TC Ukioq kaajallallugu / Hele året I IES STATION NORD RC UkiupUkiup ilaannaa ilaannaa / Kun / Seasonal visse perioder Tartupaluk HN (Hans Ø)Island) I RC SP N Wa Mylius-Erichsen IN UkioqUkioq kaajallallugu kaajallallugu / Hele / Year-round året shington Land WR Land OP UkiupUkiup ilaannaa ilaannaa / Kun / Seasonal visse perioder Da RN ugaard -Jense ND CO n Land LA R NS K E n Sermersuaq S rde UllersuaqUllersuaq (Humbolt(Humbolt Gletscher) Glacier) S fjo U rds (Cape(Kap Alexander) Alexander) M lvfje S gha Ingleeld Land RA Nio D Siorapaluk U KN Kitsissut (Carey Islands)Øer) QAANAAQ Moriusaq AVANERSUAQ Ille de France Pitufk Thule (Thule Air Base) LL AAU U G Germania LandDANMARKSHAVN CapeKap York York G E E K Savissivik K O O C C H B Q H i C A ( m Dronning M K O u F Y Margrethe II e s A F l s S Land Shannon v S e I i T N l T l r e i a B B r ZACKENBERG AU s Kullorsuaq a YG u DANEBORG y a ) Clavering Ø T q Nuussuaq Clavering Island Innarsuit Tasiusaq Ymer ØIsland UPERNAVIK Aappilattoq TraillTraill Island Ø Kangersuatsiaq Upernavik Kujalleq Summit MESTERSVIG (3.238 m) Sigguup Nunaa Stauning (Svartenhuk) AlperAlps Nuugaatsiaq Illorsuit Jameson Land Ukkusissat Niaqornat Nerlerit Inaat Qaarsut Saatut (Constable Pynt)Point) Kangertittivaq UUMMANNAQNuussuaq Ikerasak TUNU ITTOQQORTOORMIIT QEQERTARSUAQQEQERTARSUAQ (Disko (Disko Island) Ø) AVANNAA EastØstgrønland -
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ENERGY IN THE WEST NORDICS AND THE ARCTIC CASE STUDIES Energy in the West Nordics and the Arctic Case Studies Jakob Nymann Rud, Morten Hørmann, Vibeke Hammervold, Ragnar Ásmundsson, Ivo Georgiev, Gillian Dyer, Simon Brøndum Andersen, Jes Erik Jessen, Pia Kvorning and Meta Reimer Brødsted TemaNord 2018:539 Energy in the West Nordics and the Arctic Case Studies Jakob Nymann Rud, Morten Hørmann, Vibeke Hammervold, Ragnar Ásmundsson, Ivo Georgiev, Gillian Dyer, Simon Brøndum Andersen, Jes Erik Jessen, Pia Kvorning and Meta Reimer Brødsted ISBN 978-92-893-5703-6 (PRINT) ISBN 978-92-893-5704-3 (PDF) ISBN 978-92-893-5705-0 (EPUB) http://dx.doi.org/10.6027/TN2018-539 TemaNord 2018:539 ISSN 0908-6692 Standard: PDF/UA-1 ISO 14289-1 © Nordic Council of Ministers 2018 Cover photo: Mats Bjerde Print: Rosendahls Printed in Denmark Disclaimer This publication was funded by the Nordic Council of Ministers. However, the content does not necessarily reflect the Nordic Council of Ministers’ views, opinions, attitudes or recommendations. Rights and permissions This work is made available under the Creative Commons Attribution 4.0 International license (CC BY 4.0) https://creativecommons.org/licenses/by/4.0 Translations: If you translate this work, please include the following disclaimer: This translation was not produced by the Nordic Council of Ministers and should not be construed as official. The Nordic Council of Ministers cannot be held responsible for the translation or any errors in it. Adaptations: If you adapt this work, please include the following disclaimer along with the attribution: This is an adaptation of an original work by the Nordic Council of Ministers. -
I'm Not Sure That the Landslide Which Triggered This
Authors response to Professor Don Forbes review – Reviewer 1 1.) Title: I’m not sure that the landslide which triggered this tsunami event was clearly associated with rapid regional warming. It appears to have been a case of an earthquake generated fault rupture leading to gravitational collapse, possibly related to debuttressing 5 with glacial retreat. I understand the argument that warming may contribute to more rapid glacial retreat (debuttressing additional fjord walls) and may trigger slides or slumps in ice- rich permafrost soils, but I’m slightly uncomfortable with the current title. Author’s Response: Thank you for your comment and opinion. We agree that the title was confusing and we did not present any evidence for climatic trigger of the tsunami. 10 We decided to change the title into: Arctic tsunamis threaten coastal communities and landscapes - survey of Karrat fjord 2017 tsunami effects in Nuugaatsiaq, western Greenland. 2.) Abstract: 15 This is too short and insubstantial. Should report major findings, including impacts on buildings and other infrastructure, and some of the social and economic impacts in Table 1, provided the supporting data are provided. It should also report the comparison drawn between effects at Nuugaatsiaq and other similar events in Greenland. Author’s Response: Thank you for your comment. In the revised manuscript we will 20 rewrite the abstract and include more information about the socio-economic impacts and report major findings concentrated on landscape modification and tsunami deposits. On the 17th of June 2017, a massive landslide which mobilized ca. 35–58 million m3 of material entered the Karrat Isfjord in western Greenland. -
GEUS Notat Om Risiko for Fjeldskred Og Tsunamibølger I Karrat Fjorden – Status for Faglig Viden Oktober 2020
GEUS Notat om risiko for fjeldskred og tsunamibølger i Karrat Fjorden – status for faglig viden oktober 2020 Sammendrag Fredag d. 25. september 2020 kontaktede Departement for Natur og Miljø GEUS og bad om en opdateret vurdering af risiko for fjeldskred og tsunamibølger i Karrat Fjorden, og om det observerede i givet fald kan have indflydelse på risikovurderingen. GEUS ser fortsat stor bevægelsesaktivitet ved InSAR analyser af Sentinel-1 radardata og Sentinel-2 satellitbilleder for både 2019 og 2020. GEUS vurderer, at de kritiske områder stadig udgør en uændret meget høj risiko for alvorlige fjeldskred og dermed ligeledes en uændret meget høj risiko for tsunamier. Aktiviteten i fjeldsiden bekræftes ligeledes af registreringer af ikke-tektoniske signaler i de seismologiske data. Feltarbejdet i sommeren 2019 viste, at der er strukturelt betinget potentiale for fjeldskred langs hele den sydvendte kyst ved Karrat. Det er ikke muligt at forudsige hvornår eller præcist hvor, de næste større fjeldskred vil forekomme i Karrat Fjord-området. Da der er flere kritiske områder med meget høj risiko, må det ligeledes fortsat forventes, at der også efter næste større fjeldskred stadig vil være meget høj risiko for nye fjeldskred. Baggrund Karrat Fjorden ligger i det centrale Vestgrønland (figur 1 – se figurer vedlagt) med de nærmeste bygder Nuugaatsiaq ca. 30 km væk og Illorsuit ca. 60 km væk. Notater Ved anvendelse af en række forskellige metoder, primært vurdering af geologiske data, geologiske kort, topografiske kort, historisk såvel som nyere billedmateriale, seismologiske data samt optiske og radar-satellitdata, udarbejdede GEUS i juni 2018, opdateret august 2018, et notat med en vurdering af risiko for fjeldskred og tsunamibølger i Karrat Fjorden. -
Greenland Renewableenergyac
Greenland has been partly self-supplying with energy since 1993 by help of hydropower plants. The national energy production is increasing, but Greenland still depends on imported oil, primarily gas oil, diesel and petrol. Greenland has firm green ambitions – and potentials – in the energy sector. The Government of Greenland is committed to developing new hydropower plants in five communities and to invest in renewable energy for small, isolated settlements (Government of Greenland, coalition agreement 2016-2018). By pairing large-scale industry with renewable energy, Greenland can take a lead position in sustainable business. A central driver for the Government of Greenland’s commitment to renewable energy is an urge for a self-sustained economy and financial independence from subsidies from Denmark. When replacing imported fossil fuels with national energy production, the Government of Greenland supports the national economy while reducing CO2-emissions. Many communities in Greenland are small, and the grid comprises today 69 decentralized, stand-alone energy systems with no option for the distribution of renewable energy. However, two cities – Qaqortoq and Narsaq - are connected to the same hydro power plant in Qorlortorsuaq. Size matters in Greenland, as the country has an area greater than Mexico and with some communities very remote. The potential for hydropower is far from exhausted. New plants are already further analyzed, developed and in pipeline for five communities: Aasiaat, Qasigiannguit, Maniitsoq, Paamiut and Nanortalik. With more hydropower on the local grids, electric and hybrid cars can replace the use of gasoline and diesel. First- movers have already been out for some years, and more power stations are key to leverage. -
GRU Alm.Del Bilag 45: Grønlandsudvalgets Studietur Til
Grønlandsudvalget 2017-18 GRU Alm.del Bilag 45 Offentligt Grønlandsudvalgets studietur til Grønland 10.-17. august 2018 Program 10. august Kl. 07.15 Seneste check-in i Københavns lufthavn i terminal 2. Kl. 09.15 Afrejse fra Københavns lufthavn med GL 779. Kl. 09:55 Ankomst til Kangerlussuaq. Kl. 11.00 og Afrejse til Ilulissat. 11.30 Kl. 11.45 og Ankomst til Ilulissat. 12.15 Kl. 12.30 Tur til Sermermiut/Isfjorden. Kl. 16.10 Afrejse til Qaarsut med GL114. Kl. 17.20 og Afrejse til Uummannaq GL 672 og GL 674 18.04 Kl. 17.30 og Ankomst til Uummannaq 18.16 Modtagelse ved kommunalbestyrelsesmedlemmer Sakio Flesicher, Ane Marie Møller og Karl Markussen. Transport til indkvartering. Kl. 20.00 Aftensmad i B5 (den gamle lægebolig) 11. august Kl. 08.00 Morgenmad i B5 (den gamle lægebolig). Kl. 09.30 Besøg i kirken. Kl. 10.00 Besøg på Uummannaq sygehus. Kl. 11.30 Besøg på børnehjemmet, efterfulgt af frokost. Kl. 13.15 Møde med lokale politikere og erhvervsfolk. Kl. 14.00 Møde med borgere fra Nuugaatsiaq og Illorsuit. Kl. 15.00 Besøg hos Avannaa Seafood. Kl. 16.00 Besøg hos Royal Greenland. Kl. 19.00 Aftensmad i B5 (den gamle lægebolig). 12. august Kl. 07.30 Morgenmad i B5 (den gamle lægebolig). Kl. 08.00 Afgang fra Uummannaq til Saattut 1. hold. Kl. 09.30 Afgang fra Uummannaq til Saattut 2. og 3. hold. Kl. 11.00 Besøg på Vandværket i Saattut. Kl. 11.30 Møde med kommunefoged. Kl. 12.30 Møde med kommunalbestyrelsesmedlemmet i Saattut med frokost på skolen. -
Greenland Pilot
Greenland Pilot Explanations of the place names 1st Edition, 2013 Updatded 2015 2 Greenlandic place names ISBN no. 9788792107855 Preface 3 Preface The purpose of the release of the “Greenland Pilot - Explanations of the place names” has been to bring together all the information about the Greenlandic place names, and to provide users of the newly released West Greenland charts to find out about the significance of the place names. The new charts use new Greenlandic orthography as opposed to the older charts as well as some publications that use old Greenlandic orthography. The “Greenland Pilot - Explanations of the place names” have been prepared on information on place names in ”Den grønlandske Lods I, Vestgrønland“, “Den grønlandske Lods, 2. del, Østgrønland“ and “Den grønlandske Havnelods“. (Only in Danish). All place names have been reviewed and updated by Oqaasileriffik – The Greenland Language Secretariat. The publication includes “translation“ / explanation in English of Greenlandic place names specified with both new and old Greenlandic orthography. Latin names regarding the Greenland fauna is taken from the book ”Grønlands fauna, Fisk- Fugle-Pattedyr”, by B. Muus, F. Salomonsen and C. Vibe. Published by Gyldendal 1981. Latin names regarding Greenlandic flora is taken from the book ”Grønlands blomster, Flo- wers of Greenland”, by J. Feilberg, B. Fredskild and S. Holt. Published by Ahrent Flensburgs Forlag 1984. The publication is published only as an Internet publication and can be downloaded free of charge at www.gst.dk. Corrections to this publication will be published in Danish Chart Corrections on www.gst.dk. Danish Geodata Agency Rentemestervej 8 2400 Copenhagen NV E-mail: [email protected] 4 Greenlandic place names Copyright All charts, harbour charts and nautical publications published by the Danish Geodata Agency are protected by copyright. -
Survey of Karrat Isfjord 2017 Tsunami Effects in Nuugaatsiaq, Western Greenland
Arctic tsunamis threaten coastal landscapes and communities - survey of Karrat Isfjord 2017 tsunami effects in Nuugaatsiaq, western Greenland Mateusz C. Strzelecki1,2, Marek W. Jaskólski1,3,4, 5 1Institute of Geography and Regional Development, University of Wrocław, pl. Uniwersytecki 1, 50-137 Wrocław, Poland, ORCID: 0000-0003-0479-3565 2Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Permafrost Research, 14473 Potsdam, Germany 3 Leibniz Institute of Ecological Urban and Regional Development, Environmental Risks in Urban and Regional 10 Development, Weberplatz 1, 01217 Dresden, Germany 4 Interdisciplinary Centre for Ecological and Revitalizing Urban Transformation, Gottfried-Kiesow-Platz 1 02826 Görlitz, Germany Correspondence: e-mail: [email protected]; [email protected] 15 Abstract On the 17th of June 2017, a massive landslide which mobilized ca. 35–58 million m3 of material entered the Karrat Isfjord in western Greenland. It triggered a tsunami wave with a runup height exceeding 90 m close to the landslide, ca. 50 m on the opposite shore of the fjord. The tsunami travelled ca. 32 km across the fjord and reached the settlement of Nuugaatsiaq with ca. 1-1.5 m high waves, which were powerful enough to destroy the community infrastructure, impact fragile coastal 20 tundra landscape, and unfortunately, injure several inhabitants and cause 4 deaths. Our field survey carried out 25 months after the event results in documentation of previously unreported scale of damages in the settlement (ca. 48% of infrastructure objects including houses and administration buildings were destroyed by tsunami). We have observed a recognizable difference in the concentration of tsunami deposit accumulations between areas of the settlement overwashed by wave and areas where tsunami flooded terrain and return to the fjord.