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Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands. -
Arctic Ocean Outflow and Glacier-Ocean Interaction Modify Water Over the Wandel Sea Shelf
Ocean Sci. Discuss., doi:10.5194/os-2017-28, 2017 Manuscript under review for journal Ocean Sci. Discussion started: 20 April 2017 c Author(s) 2017. CC-BY 3.0 License. Arctic Ocean outflow and glacier-ocean interaction modify water over the Wandel Sea shelf, northeast Greenland Igor A. Dmitrenko1*, Sergei A. Kirillov1, Bert Rudels2, David G. Babb1, Leif Toudal Pedersen3, Søren 5 Rysgaard1,4,5, Yngve Kristoffersen6,7 and David G. Barber1 1Centre for Earth Observation Science, University of Manitoba, Winnipeg, Canada 2Finnish Meteorological Institute, Helsinki, Finland 3Danish Meteorological Institute, Copenhagen, Denmark 10 4Greenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland 5Arctic Research Centre, Aarhus University, Aarhus, Denmark 6Department of Earth Science, University of Bergen, Bergen, Norway 7 Nansen Environmental and Remote Sensing Centre, Bergen, Norway 15 *Corresponding author, e-mail: [email protected] Abstract: The first-ever conductivity-temperature-depth (CTD) observations on the Wandel Sea shelf in North Eastern Greenland were collected in April-May 2015. They were complemented by CTD profiles taken along the continental slope during the Norwegian FRAM 2014-15 drift. The CTD profiles 1 Ocean Sci. Discuss., doi:10.5194/os-2017-28, 2017 Manuscript under review for journal Ocean Sci. Discussion started: 20 April 2017 c Author(s) 2017. CC-BY 3.0 License. 20 are used to reveal the origin of water masses and interactions with ambient water from the continental slope and the outlet glaciers. The subsurface water is associated with the Pacific Water outflow from the Arctic Ocean. The underlying Halocline separates the Pacific Water from a deeper layer of Polar Water that has interacted with the warm Atlantic water outflow through Fram Strait recorded below 140 m. -
Neo-Colonial Continuities in the Mediterranean Infrastructure Projects of Atlantropa and Desertec
Ardeth A magazine on the power of the project 7 | 2020 Europe Neo-colonial Continuities in the Mediterranean Infrastructure Projects of Atlantropa and Desertec Alexander Stumm Electronic version URL: https://journals.openedition.org/ardeth/1883 ISSN: 2611-934X Publisher Rosenberg & Sellier Printed version Date of publication: 1 December 2020 Number of pages: 127-140 ISSN: 2532-6457 Electronic reference Alexander Stumm, “Neo-colonial Continuities in the Mediterranean Infrastructure Projects of Atlantropa and Desertec”, Ardeth [Online], 7 | 2020, Online since 01 June 2021, connection on 29 July 2021. URL: http://journals.openedition.org/ardeth/1883 CC BY-NC-ND 4.0 Neo-colonial Continuities in the Mediterranean Infrastructure Projects of Atlantropa and Desertec Alexander Stumm Abstract Affiliatio Herman Sörgel’s gigantic project “Atlantropa” is a Technische Universität Berlin, prominent European project in terms of infrastruc- Institut für ture and territory in the first half of the 20th century. Architektur It is an example of a modernity that is necessarily Contacts: believing in progress through technology – as will stumm [at] tu-berlin be shown the first section of this essay, but it is also [dot] de profitable in that it historically locates Europe’s cur- Received: rent energy policy infrastructure projects in Africa, 8 July 2020 to which the second section of the essay is dedicated. The vision pursued under the name Destertec envis- Accepted: 23 February 2021 ages the large-scale implementation of renewable energy power plants, especially solar thermal power DOI: plants in Northern Africa. Both projects share an 10.17454/ARDETH07.08 unshakeable belief in ecomodernist ideas, meaning ARDETH #07 the solution of socio-economic and ecological chal- lenges through technology (Gall, 2014). -
Interpolar Transnational Art Science States
ART I N AN TA R C T I C A , A SE R I E S O F CO N F E R E N C E S … P. 4 @rt Outsiders September 2008 - 9th year www.art-outsiders.com Tel : +33 (0)1 44 78 75 00 Maison Européenne de la Photographie 5-7 rue de Fourcy – 75 004 Paris M° Saint-Paul ou Pont-Marie / Bus 67, 69, 96 ou 76 I N T E R P O L A R A RT 24 September 2008 - 12 October 2008 with Marko Peljhan and Annick Bureaud, Bureau d’études, Ewen Chardronnet, Andrea Polli, Catherine Rannou. The extreme in the centre by Annick Bure a u d rom the very first polar expeditions, artists have contributed to the imaginary surrounding the FEarth’s “extremities” and their work has fed a sense of the sublime and of romanticism. Such a romantic vision endures, fuelled by adventurers of the extreme, who set out crossing, alone, the antarctic continent, the touching (and a n t h ropomorphic) image of penguins, the deadly beauty of the environment conveyed by thousands of images of “icy white”, and by the fact that Antarctica is now threatened by global warming and our pollution, that this last huge, supposedly virg i n , territory is in danger. To create in or about Antarctica today is as much a political as an artistic act, just as it was in the 19th or early 20th century. Except today the continent faces quite a diff e r ent reality and our approaches are p r obably more varied, more contradictory, more complex; burdened with numerous clichés all the I-TASC - The Arctic Perspective more enduring for being mostly true. -
Arctic Ocean Outflow and Glacier-Ocean Interaction Modify Water Over the Wandel Sea Shelf
1 1 Arctic Ocean outflow and glacier-ocean interaction modify water over the Wandel Sea shelf 2 (Northeast Greenland) 3 4 5 Igor A. Dmitrenko1*, Sergey A. Kirillov1, Bert Rudels2, David G. Babb1, Leif Toudal Pedersen3, Søren 6 Rysgaard1,4,5, Yngve Kristoffersen6,7 and David G. Barber1 7 8 9 1Centre for Earth Observation Science, University of Manitoba, Winnipeg, Canada 10 2Finnish Meteorological Institute, Helsinki, Finland 11 3 Technical University of Denmark, Lyngby, Denmark 12 4Greenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland 13 5Arctic Research Centre, Aarhus University, Aarhus, Denmark 14 6Department of Earth Science, University of Bergen, Bergen, Norway 15 7 Nansen Environmental and Remote Sensing Centre, Bergen, Norway 16 17 18 19 20 21 22 *Corresponding author, e-mail: [email protected] 2 23 Abstract: The first-ever conductivity-temperature-depth (CTD) observations on the Wandel Sea shelf in 24 North Eastern Greenland were collected in April-May 2015. They were complemented by CTDs taken 25 along the continental slope during the Norwegian FRAM 2014-15 drift. The CTD profiles are used to 26 reveal the origin of water masses and interactions with ambient water from the continental slope and the 27 tidewater glacier outlet. The subsurface water is associated with the Pacific Water outflow from the Arctic 28 Ocean. The underlying Halocline separates the Pacific Water from a deeper layer of Polar Water that has 29 interacted with the warm Atlantic water outflow through Fram Strait recorded below 140 m. Over the outer 30 shelf, the Halocline shows numerous cold density-compensated intrusions indicating lateral interaction with 31 an ambient Polar Water mass across the continental slope. -
Stratigraphy and Depositional Evolution of the Upper Palaeozoic Sedimentary Succession in Eastem Peary Land, North Greenland
Stratigraphy and depositional evolution of the Upper Palaeozoic sedimentary succession in eastem Peary Land, North Greenland Lars Stemmerik, Eckart Håkansson, Lena Madsen, Inger Nilsson, Stefan Piasecke, Sylvie Pinard2 and Jan A. Rasmussen The Upper Palaeozoic Foldedal and Kim Fjelde formations in eastem Peary Land are redefined on the basis of new biostratigraphic data, including fusulinids, conodonts, palynomorps and small foraminifera. The Foldedal Formation in its new definition includes alllate Moscovian to Gzelian deposits in the region. It is separated by a major hiatus from the redefined Kim Fjelde Formation which includes mid-Permian (late Art inskian - Kungurian) carbonates and chert deposits. The Upper Carboniferous succes sion is dominated by cyclically interbedded siliciclastics and carbonates with minor tab- ular build-ups. The mid and Upper Permian succession consists ofcool-water carbonates, spiculitic chert and shales. L. S., S. pI & J. A. R., Geological Survey ofDenmark and Greenland, Thoravej 8, DK 2400 Copenhagen NV, Denmark. E. H. & L. M., Geological Institute, University ofCopenhagen, øster Voldgade IO, DK 1350 Copenhagen K, Denmark. I. N., Saga Petroleum a.s., Postboks /134, N-9400 Harstad, Norway. S. p2, 7146--119th Street N. w., Edmonton T6G 1V6, Canada (formerly ofthe Geological Survey ofCanada). In eastem Peary Land, the marine Upper Palaeozoic tus spanning most ofthe Early Permian, and accordingly, deposits of the Wandel Sea Basin have been included in the originally proposed lithostratigraphic scheme has to the upper Moscovian to Upper Carboniferous Foldedal be revised. Fonnation ofmixed carbonates and siliciclastics, the Upper This paper revises the lithostratigraphy of the Upper Carboniferous to (?) Kungurian carbonate-dominated Kim Palaeozoic deposits in eastem Peary Land in accordance Fjelde Formation and the shale-dominated, mid to Upper with new sedimentological and sequence stratigraphic Permian Midnatfjeld Formation (Håkansson, 1979; Stem information, and provides new biostratigraphic data from merik & Håkansson, 1989). -
Significance of K/Ar Age Determinations from Northern Peary Land
60 Dawes, P. R. & Soper, N. J. 1970: Geological investigations in northern Peary Land. Rapp. Grønlands geol. Unders. 28, 9-15. Escher, A., Escher, J., & Watterson, J. 1970: The Nagssugtoqidian boundary and the deformation of the Kångamiut dyke swarm in the Søndre Strømfjord area. Rapp. Grønlands geol. Unders. 28, 21-23. Escher, A. & Pulvertaft, T. C. R. 1968: The Precambrian rocks of the Upernavik-Kraulshavn area (72°_ 74°15' N), West Greenland. Rapp. Grønlands geol. Unders. 15, 11-14. Henriksen, N., & Jepsen, H. F. 1970: K/Ar age determinations on dolerites from southern Peary Land. Rapp. Grønlands geol. Unders. 28, 55-58. Keto, L. 1970: Isua, a major iron ore discovery in Greenland. Unpublished report from Kryolitselskabet Øresund AIS, Copenhagen. Lambert, R. St. J. & Simons, J. G. 1969: New KlAr age determinations from southern West Greenland. Rapp. Grønlands geol. Unders. 19, 68-71. Larsen, O. & Møller, J. 1968: K/Ar age determinations from western Greenland L Reconnaissance pro gramme. Rapp. Grønlands geol. Unders. 15, 82-86. Sarsadskikh, N. N., Blagul'kina, V. A. & Silin, Yu. L 1966: Absolute age of Yakutian kimberlites. Dokl. Aead. Sei. USSR, Earth Sci. Sect. 168, 48-50. Watterson, J. 1965: Plutonic development of the Ilordleq area, South Greenland. Bul!. Grønlands geol. Unders. 51 (also Meddr Grønland, 172, 7) 147 pp. Wanless, R. K., Stevens, R. D. & Loveridge, W. D. 1970: Anomalous parent-daughter isotopic relation ships in rocks adjacent to the Grenville front near Chibougamau, Quebec. Ec!og. geol. Helv. 63; I, 345 364. Windley, B. F. 1970: Primary quartz ferro-dolerite/garnet amphibolite dykes in the Sukkertoppen region of West Greenland. -
Accelerated Sea Ice Loss in the Wandel Sea Points to a Change in the Arctic’S Last Ice Area
Axel Schweiger, Michael Steele, Jinlun Zhang, G.W.K.Moore, and Kristin Laidre Accelerated Sea Ice Loss in the Wandel Sea Points to a Change in the Arctic’s Last Ice Area Key Points 1. 2. The Wandel Sea, north of Greenland An unexpected record-low in the Arctic Ocean, is the concentration of sea-ice in the easternmost part of what is known Wandel Sea was seen in August as the “Last Ice Area” where thick 2020. multi-year sea-ice has been expected to last the longest. Schweiger et al./Communications Earth & Environment. 3. 4. In the whole Arctic Ocean, sea-ice Study of long-term satellite data (extent, thickness, and age) has and sea ice modeling experiments decreased over the past couple point to climate change as a cause decades. of long-term thinning of Arctic sea- ice. Black line shows percent of sea-ice concentration for the Wandel Sea from 1 June through 31 August 2020. Solid blue line shows the climatological trend from 1979–2020 with 10/90th and 5/95th percentiles shown in dashed and dotted blue lines. Image courtesy of Schweiger et al. 5. 6. Natural changes in winds and At the beginning of the 2020 sea-ice temperatures cause more loss of melt season (spring) the Wandel sea ice in the area: Sea had unusually high amounts of a. Winds move the sea-ice out of thick ice—but it was not enough to the area prevent the record-low b. Warm air and ocean concentration in August. temperatures melt the ice 7. -
Downloaded from the Copernicus Data System Assimilation (I.E., HIST Vs
ARTICLE https://doi.org/10.1038/s43247-021-00197-5 OPEN Accelerated sea ice loss in the Wandel Sea points to a change in the Arctic’s Last Ice Area ✉ Axel J. Schweiger1 , Michael Steele1, Jinlun Zhang1, G. W. K. Moore 2,3 & Kristin L. Laidre1 The Arctic Ocean’s Wandel Sea is the easternmost sector of the Last Ice Area, where thick, old sea ice is expected to endure longer than elsewhere. Nevertheless, in August 2020 the area experienced record-low sea ice concentration. Here we use satellite data and sea ice model experiments to determine what caused this record sea ice minimum. In our simula- tions there was a multi-year sea-ice thinning trend due to climate change. Natural climate variability expressed as wind-forced ice advection and subsequent melt added to this trend. — — 1234567890():,; In spring 2020, the Wandel Sea had a mixture of both thin and unusual for recent years thick ice, but this thick ice was not sufficiently widespread to prevent the summer sea ice concentration minimum. With continued thinning, more frequent low summer sea ice events are expected. We suggest that the Last Ice Area, an important refuge for ice-dependent species, is less resilient to warming than previously thought. 1 Polar Science Center, Applied Physics Laboratory, University of Washington, Seattle, WA, USA. 2 Department of Physics, University of Toronto, Ontario, ON, ✉ Canada. 3 Department of Chemical and Physical Sciences, University of Toronto Mississauga, Mississauga, Ontario, ON, Canada. email: [email protected] COMMUNICATIONS EARTH & ENVIRONMENT -
H-Environment Roundtable Reviews
H-Environment Roundtable Reviews Volume 1, No. 3 (2011) Roundtable Review Editor: www.h-net.org/~environ/roundtables Jacob Darwin Hamblin Publication date: August 5, 2011 James Rodger Fleming, Fixing the Sky: The Checkered History of Weather and Climate Control (Columbia University Press, 2010). ISBN: 978-0-231-14412-4. Hardcover. 344 pages. Stable URL: www.h-net.org/~environ/roundtables/env-roundtable-1-3.pdf Contents Introduction by Jacob Darwin Hamblin, Oregon State University 2 Comments by Ted Steinberg, Case Western Reserve University 4 Comments by R. S. Deese, Northeastern University 6 Comments by Matthew Farish, University of Toronto 9 Comments by Paul N. Edwards, University of Michigan 14 Author’s Response by James Rodger Fleming, Colby College 22 About the Contributors 26 Copyright © 2011 H-Net: Humanities and Social Sciences Online H-Net permits the redistribution and reprinting of this work for nonprofit, educational purposes, with full and accurate attribution to the author, web location, date of publication, H-Environment, and H-Net: Humanities & Social Sciences Online. H-Environment Roundtable Reviews, Vol. 1, No. 3 (2011) 2 Introduction by Jacob Darwin Hamblin, Oregon State University n 1968, the Whole Earth Catalog proclaimed “We are as gods and might as well get good at it.” Amidst the environmental crisis of the 1960s, the publication’s founder II Stewart Brand wanted to provide access to tools, and he was remarkably friendly to technological solutions. His kind of environmentalism drew from human ingenuity and achievement, and unlike many of the commentators of that era, he was optimistic about a future in human hands. -
Thermotectonic Development of the Wandel Sea Basin, North Greenland
Thermotectonic development of the Wandel Sea Basin, North Greenland Peter Japsen1, Paul F. Green2 & James A. Chalmers1 1Geological Survey of Denmark and Greenland (GEUS) 2Geotrack International The Carboniferous – Palaeogene Wandel Sea Basin (WSB) and the Eurekan Orogeny Eurekan Orogeny: Deformation caused by the Palaeogene convergence between Greenland and the High Arctic • Arctic Canada (Okulitch & Trettin 1991; Embry & Beauchamp 2008) • Wandel Sea Basin: Kronprins Christian Land Orogeny (Håkansson & Pedersen 2001) • Svalbard: the West Spitzbergen Orogeny (Steer et al. 1985; Dallmann et al. 1993) Brozena et al. (2003), Oakey & Chalmers (2012), Gaina et al. (2017) The Carboniferous – Palaeogene Wandel Sea Basin (WSB) and the Eurekan Orogeny WSB Piepjohn & von Gosen 2001; Oakey & Chalmers 2012; Piepjohn et al. 2015 Carboniferous – Palaeogene Wandel Sea Basin Oakey & Chalmers 2012; Gion et al. 2017 Escher & Pulvertaft 1995; Hovikoski et al. 2018 Apatite fission-track analysis (AFTA) data in 46 samples Japsen et al. GEUS Bulletin (in revision) Timing of regional episodes of cooling and exhumation estimated from AFTA data Wandel Sea Basin Japsen et al. GEUS Bulletin (in revision) Timing of regional episodes of cooling and exhumation estimated from AFTA data Wandel Sea Basin Pre-Cenozoic episodes Japsen et al. GEUS Bulletin (in revision) Timing of regional episodes of cooling and exhumation estimated from AFTA data Wandel Sea Basin Paleocene episode Japsen et al. GEUS Bulletin (in revision) Timing of regional episodes of cooling and exhumation estimated from AFTA data Wandel Sea Basin Post-Paleocene episodes Japsen et al. GEUS Bulletin (in revision) Palaeotemperatures prior to cooling at ~60 Ma Exhumation affected the major fault zones of the Wandel Sea Basin >3 km Cretaceous to Paleocene sediments were removed within the fault zones HFFZ: Harder Fjord Fault Zone TLFZ: Trolle Land Fault Zone 30°C/km, 20°C at the surface Japsen et al.