Spring 2019 Icebridge Arctic Flight Plans 22 March 2019 Draft John Sonntag
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Research Cruise Report: Mission HLY031
Research Cruise Report: Mission HLY031 Conducted aboard USCGC Healy In Northern Baffi n Bay and Nares Strait 21 July –16 August 2003 Project Title: Variability and Forcing of Fluxes through Nares Strait and Jones Sound: A Freshwater Emphasis Sponsored by the US National Science Foundation, Offi ce of Polar Programs, Arctic Division Table of Contents Introduction by Chief Scientist . 4 Science Program Summary . 6 Science Party List . 7 Crew List . 8 Science Component Reports CTD-Rosette Hydrography . 9 Internally recording CTD . 29 Kennedy Channel Moorings . 33 Pressure Array . 41 Shipboard ADCP . 47 Bi-valve Retrieval . 51 Coring . 55 Seabeam Mapping . 65 Aviation Science Report . 71 Ice Report . 79 Weather Summary . 91 Inuit Perspective . 95 Photojournalist Perspective . 101. Website Log . 105 Chief Scientist Log . 111 Recommendations . .125 Introduction Dr. Kelly Kenison Falkner Chief Scientist Oregon State University In the very early hours of July 17, 2003, I arrived at collected via the ship’s Seabeam system and the underway the USCGC Healy moored at the fueling pier in St. John’s thermosalinograph system was put to good use throughout Newfoundland, Canada to assume my role as chief scientist much of the cruise. for an ambitious interdisciplinary mission to Northern Part of our success can be attributed to luck with Mother Baffi n Bay and Nares St. This research cruise constitutes Nature. Winds and ice worked largely in our favor as we the inaugural fi eld program of a fi ve year collaborative wound our way northward. Our winds were generally research program entitled Variability and Forcing of moderate and out of the south and the ice normal to light. -
Postglacial Isobases from Northern Ellesmere Island and Greenland
Document generated on 09/23/2021 9:47 a.m. Géographie physique et Quaternaire Postglacial Isobases from Northern Ellesmere Island and Greenland: New Data Isobases postglaciaires du nord de l’île d’Ellesmere et du Groenland : nouvelles données Postglaziale Isobasen vom Norden der Ellesmere-lnsel und Grönland: neue Daten John England and Jan Bednarski Volume 40, Number 3, 1986 Article abstract Over seventy new 14C dates on former relative sea levels from Hall Land, URI: https://id.erudit.org/iderudit/032650ar northwest Greenland, and Clements Markham Inlet, northern Ellesmere DOI: https://doi.org/10.7202/032650ar Island, are combined with previous data to revise the regional isobases for this area. These isobases show : 1) a centre of maximum postglacial emergence See table of contents over northwest Greenland extending to; 2) an intervening cell of lower emergence over northeast Ellesmere Island which was isostatically-dominated by the Greenland Ice Sheet; in turn, extending to 3) a higher centre of Publisher(s) emergence over the Grant Land Mountains, northernmost Ellesmere Island, associated with the independent history of local ice caps there. Radiocarbon Les Presses de l'Université de Montréal dates from raised marine shorelines show a 2000 year lag between glacial unloading on northwest Greenland and northernmost Ellesmere Island. This ISSN lag in glacioisostatic adjustments suggests a considerable range in the glacier response times and/or glacioclimatic regimes in this area. Throughout the area 0705-7199 (print) the last ice limit was ca. 5-60 km beyond present ice margins. Maximum 1492-143X (digital) emergence at these ice limits is marked by shorelines built into a full glacial sea which range from 124 m asl in Clements Markham Inlet to 150 m asl in Hall Explore this journal Land. -
ARCTIC RIFT COPPER Part of World’S Newest Metallogenic Province: Kiffaanngissuseq
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/346029727 ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Report · November 2020 DOI: 10.13140/RG.2.2.18610.84161 CITATIONS 0 2 authors, including: Jonathan Bell Curtin University 17 PUBLICATIONS 13 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Greenland View project Mineral asset valuation and pricing View project All content following this page was uploaded by Jonathan Bell on 20 November 2020. The user has requested enhancement of the downloaded file. ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Assessment Report Greenfields Exploration Ltd November 2020 This report presents a holistic view of north eastern Greenland’s geology. The empirical evidence of mineralisation and geological record are tied in with mineral system components from global through to prospect scales. The source rocks, geodynamic triggers, pathways, and deposition sites are all identified within a preserved terrane. This work defines the Kiffaanngissuseq metallogenic province, a previously undescribed mineral system. For the first time, we identify a c. 1,250 Ma orogenic event in the basement as the geodynamic trigger related to the basalt- hosted native copper within the Arctic Rift Copper project. A c. 385 Ma fluid migration is identified as the trigger for a second copper-sulphide mineralising event expressed within the project, that also emplaced a distal zinc deposit within Kiffaanngissuseq. This multi-episodal mineral system is supported by a regional geochemical and hydrodynamic framework that is not articulated elsewhere. -
2010-2011 Science Planning Summaries
Find information about current Link to project web sites and USAP projects using the find information about the principal investigator, event research and people involved. number station, and other indexes. Science Program Indexes: 2010-2011 Find information about current USAP projects using the Project Web Sites principal investigator, event number station, and other Principal Investigator Index indexes. USAP Program Indexes Aeronomy and Astrophysics Dr. Vladimir Papitashvili, program manager Organisms and Ecosystems Find more information about USAP projects by viewing Dr. Roberta Marinelli, program manager individual project web sites. Earth Sciences Dr. Alexandra Isern, program manager Glaciology 2010-2011 Field Season Dr. Julie Palais, program manager Other Information: Ocean and Atmospheric Sciences Dr. Peter Milne, program manager Home Page Artists and Writers Peter West, program manager Station Schedules International Polar Year (IPY) Education and Outreach Air Operations Renee D. Crain, program manager Valentine Kass, program manager Staffed Field Camps Sandra Welch, program manager Event Numbering System Integrated System Science Dr. Lisa Clough, program manager Institution Index USAP Station and Ship Indexes Amundsen-Scott South Pole Station McMurdo Station Palmer Station RVIB Nathaniel B. Palmer ARSV Laurence M. Gould Special Projects ODEN Icebreaker Event Number Index Technical Event Index Deploying Team Members Index Project Web Sites: 2010-2011 Find information about current USAP projects using the Principal Investigator Event No. Project Title principal investigator, event number station, and other indexes. Ainley, David B-031-M Adelie Penguin response to climate change at the individual, colony and metapopulation levels Amsler, Charles B-022-P Collaborative Research: The Find more information about chemical ecology of shallow- USAP projects by viewing individual project web sites. -
Cosmogenic-Nuclide Exposure Ages from the Pensacola Mountains Adjacent to the Foundation Ice Stream, Antarctica
[American Journal of Science, Vol. 316, June, 2016,P.542–577, DOI 10.2475/06.2016.02] COSMOGENIC-NUCLIDE EXPOSURE AGES FROM THE PENSACOLA MOUNTAINS ADJACENT TO THE FOUNDATION ICE STREAM, ANTARCTICA GREG BALCO*,†, CLAIRE TODD**, KATHLEEN HUYBERS***, SETH CAMPBELL§, MICHAEL VERMEULEN**, MATTHEW HEGLAND**, BRENT M. GOEHRING§§, AND TREVOR R. HILLEBRAND*** ABSTRACT. We describe glacial-geological observations and cosmogenic-nuclide exposure ages from the Schmidt, Williams, and Thomas Hills in the Pensacola Mountains of Antarctica adjacent to the Foundation Ice Stream (FIS). Our aim is to learn about changes in the thickness and grounding line position of the Antarctic Ice Sheet in the Weddell Sea embayment between the Last Glacial Maximum (LGM) and the present. Glacial-geological observations from all three regions indicate that currently- ice-free areas were covered by ice during one or more past ice sheet expansions, and that this ice was typically frozen to its bed and thus non-erosive, permitting the accumulation of multiple generations of glacial drift. Cosmogenic-nuclide exposure- age data from glacially transported erratics are consistent with this interpretation in that we observe both (i) samples with Holocene exposure ages that display a systematic age-elevation relationship recording LGM-to-present deglaciation, and (ii) samples with older and highly scattered apparent exposure ages that were deposited in previous glacial-interglacial cycles and have experienced multiple periods of surface exposure and ice cover. Holocene exposure ages at the Thomas and Williams Hills, upstream of the present grounding line of the FIS, show that the FIS was at least 500 m thicker prior to 11 ka, and that 500 m of thinning took place between 11 and 4 ka. -
Greenland by the Polar Sea; the Story of the Thule Expedition From
UNIVERSITY OF CALIFORNIA AT LOS ANGELES GREENLAND BY THE POLAK SEA 3 07 SOUTH The story of Shackleton's Last Expedition, 1914-1917. By Sir Ernest Shackleton, C.V.O. Illustrated by many Photographs and Maps. Royal 8vo. 25s. net. Also a Cheaper Edition, Crown 8vo. 10s. 6d. net. THE HEART OF THE ANTARCTIC By Sir Ernest Shackleton, C.V.O. New and Revised Edition, with Illus- trations in colour and black and white. Crown 8vo. 10s. 6d. net. THE HOME OF THE BLIZZARD Being the story of the Australian Ant- arctic Expedition, 1911-1914. By Sir Douglas Mawson, D.Sc, B.E. With over 300 Photographs, Maps, etc. In two vols. Crown 4to. 36s. net. ANTARCTIC PENGUINS By Dr. G. Murray Derick, R.N., Zoolo- gist to the Scott Expedition. Beautifully Illustrated from Photographs. 6s. net. LONDON: WILLIAM HEINEMANN GREENLAND BY THE POLAR SEA THE STORY OF THE. THULE EXPEDITION FROM MELVILLE BAY TO CAPE MORRIS JESUP BY KNUD RASMUSSEN TRANSLATED FROM THE DANISH BY ASTA AND ROWLAND KENNEV WITH PREFACE BY ADMIRAL SIR LEWIS BEAUMONT, G.C.B WITH NUMEROUS ILLUSTRATIONS IN BLACK AM) WHITE, BIGHT COLOUR PLATES, AND MAPS > • • NEW VOHK FREDERICK A. STOKES COMPANY PUBLISHERS 308! Printed m Great Britain V) PREFACE " GREENLAND by the Polar Sea is the story, now intro- duced to English readers, of Mr. Knud Rasmussen's last expedition to the Polar shores of North Greenland. He counts it as his Fourth Thule Expedition, which shows how active and persevering has been his exploration of North Green- land since 1910, when he first formed his base of operations, and pa trading station, at North Star Bay, and gave it the name of r/ Thule. -
Ice-Free Valleys in the Neptune Range of the Pensacola Mountains, Antarctica: Glacial Geomorphology, Geochronology and Potential
Antarctic Science 33(4), 428–455 (2021) © The Author(s), 2021. Published by Cambridge University Press on behalf of Antarctic Science Ltd. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http:// creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. doi:10.1017/S0954102021000237 Ice-free valleys in the Neptune Range of the Pensacola Mountains, Antarctica: glacial geomorphology, geochronology and potential as palaeoenvironmental archives DAVID SMALL 1, MICHAEL J. BENTLEY 1, DAVID J.A. EVANS1, ANDREW S. HEIN 2 and STEWART P.H.T. FREEMAN 3 1Department of Geography, Durham University, Durham, DH1 3LE, UK 2School of Geosciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 3Scottish Universities Environmental Research Centre, East Kilbride, G75 0QF, UK [email protected] Abstract: We describe the glacial geomorphology and initial geochronology of two ice-free valley systems within the Neptune Range of the Pensacola Mountains, Antarctica. These valleys are characterized by landforms associated with formerly more expanded ice sheet(s) that were at least 200 m thicker than at present. The most conspicuous features are areas of supraglacial debris, discrete debris accumulations separated from modern-day ice and curvilinear ridges and mounds. The landsystem bears similarities to debris-rich cold-based glacial landsystems described elsewhere in Antarctica and the Arctic where buried ice is prevalent. Geochronological data demonstrate multiple phases of ice expansion. The oldest, occurring > 3 Ma, overtopped much of the landscape. Subsequent, less expansive advances into the valleys occurred > 2 Ma and > ∼1 Ma. -
Durham Research Online
Durham Research Online Deposited in DRO: 25 October 2018 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Hill, E.A. and Carr, J.R. and Stokes, C.R. and Gudmundsson, G.H. (2018) 'Dynamic changes in outlet glaciers in northern Greenland from 1948 to 2015.', The cryosphere., 12 (10). pp. 3243-3263. Further information on publisher's website: https://doi.org/10.5194/tc-12-3243-2018 Publisher's copyright statement: c Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk The Cryosphere, 12, 3243–3263, 2018 https://doi.org/10.5194/tc-12-3243-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Dynamic changes in outlet glaciers in northern Greenland from 1948 to 2015 Emily A. -
Abstracts of the 12Th Arctic Workshop, University Of
ABSTRACTS OF THE 12TH ANNUAL ARCTIC WORKSHOP MARCH 16, 17, and 18th, 1983 UNIVERSITY OF MASSACHUSETTS AMHERST ....T.U:;r'lV .. "fl'JII"J[ flml.1.l!V!lTl 1rnJ,NIA\ T 2 12th ANNUAL ARCTIC WORKSHOP March 16, 17, 18, 1983 AGENDA Session A, Wednesday, March 16 - Chairman, Ray Bradley 9:00-9:30 am * William Barr, Dept. of Geography, University of Saskatchewan, Saskatoon Pioneer geomorphological investigations from the First International Polar Year, 1882-1883. 9:30-10:00 am Peter Clark, Institute of Arctic and Alpine Research, University of Colorado, Boulder Onshore-off shore correlations of glacial events in Northern Labrador, Part I: the land record. 10:00-10:30 am Heiner Josenshans, Atlantic Geoscience Center, Bedford Institute of Oceanography, Dartmouth, Nova Scotia Onshore-offshore correlations of glacial events in Northern Labrador, Part II: the marine record. 10:30-11:00 am Coffee Break Session B Chairman, John Hollin 11: 00-11: 30 am Detmar Schnitker, Dept. of Geological Sciences and Program in Oceanography, University of Maine, Orono The Norwegian-Greenland Sea: a critical area for global oceanography and climate. 11: 30-12: 00 am S. Lehman, S. Forman and G.H. Miller, Institute of Arctic and Alpine Research, University of Colorado, Boulder Quaternary stratigraphy and ice limits, Forlandsund region, West Spitsbergen, Svalbard. 12:00-12:30 pm G. Jones, Lamont-Doherty Geological Observatory, Palisades, New York A revised time-scale for Late Pleistocene sediments of the Central Arctic Basin: implications for understanding Arctic response to solar insolation variations. 12:30-1:30 LUNCH *All presentations will be given in Campus Center Room 163/164. -
Major Ice Sheet Change in the Weddell Sea Sector of West Antarctica Over the Last 5,000 Years
REVIEW ARTICLE Major Ice Sheet Change in the Weddell Sea Sector 10.1029/2019RG000651 of West Antarctica Over the Last 5,000 Years Martin J. Siegert1 , Jonathan Kingslake2 , Neil Ross3 , Pippa L. Whitehouse4 , John Woodward5 , Stewart S. R. Jamieson4 , Michael J. Bentley4 , Kate Winter5 , Martin Wearing2 , Andrew S. Hein6 , Hafeez Jeofry1 , and David E. Sugden6 1Grantham Institute and Department of Earth Science and Engineering, Imperial College London, London, UK, 2Lamont‐ Doherty Earth Observatory, Columbia University, Palisades, NY, USA, 3School of Geography, Politics and Sociology, Newcastle University, Newcastle, UK, 4Department of Geography, Durham University, Durham, UK, 5Department of Key Points: Geography and Environmental Sciences, Faculty of Engineering and Environment, Northumbria University, Newcastle, 6 • The Weddell Sector has experienced UK, School of GeoSciences, University of Edinburgh, Edinburgh, UK major change since the Late Holocene • It is unclear whether the ice sheet Abstract Until recently, little was known about the Weddell Sea sector of the West Antarctic Ice Sheet. In gradually shrank to its modern size the last 10 years, a variety of expeditions and numerical modelling experiments have improved knowledge of from its full‐glacial state or became smaller here and then regrew its glaciology, glacial geology and tectonic setting. Two of the sector's largest ice streams rest on a steep • Targeted geophysical dating of reverse‐sloping bed yet, despite being vulnerable to change, satellite observations show contemporary buried and exposed surfaces and fi sediment drilling may resolve the stability. There is clear evidence for major ice sheet recon guration in the last few thousand years, however. inconsistencies in glacial history Knowing precisely how and when the ice sheet has changed in the past would allow us to better understand whether it is now at risk. -
Tulaczyk (PDF)
Journal of Glaciology, Vol. 55, No. 192, 2009 573 An inventory of active subglacial lakes in Antarctica detected by ICESat (2003–2008) Benjamin E. SMITH,1 Helen A. FRICKER,2 Ian R. JOUGHIN,1 Slawek TULACZYK3 1Applied Physics Laboratory, University of Washington, 1013 NE 40th Street, Box 355640, Seattle, Washington 98105-6698, USA E-mail: [email protected] 2Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California–San Diego, La Jolla, California 92093-0225, USA 3Department of Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, California 95064, USA ABSTRACT. Through the detection of surface deformation in response to water movement, recent satellite studies have demonstrated the existence of subglacial lakes in Antarctica that fill and drain on timescales of months to years. These studies, however, were confined to specific regions of the ice sheet. Here we present the first comprehensive study of these ‘active’ lakes for the Antarctic ice sheet north of 868 S, based on 4.5 years (2003–08) of NASA’s Ice, Cloud and land Elevation Satellite (ICESat) laser altimeter data. Our analysis has detected 124 lakes that were active during this period, and we estimate volume changes for each lake. The ICESat-detected lakes are prevalent in coastal Antarctica, and are present under most of the largest ice-stream catchments. Lakes sometimes appear to transfer water from one to another, but also often exchange water with distributed sources undetectable by ICESat, suggesting that the lakes may provide water to or withdraw water from the hydrologic systems that lubricate glacier flow. -
Adobe PDF of Proposed Flight Lines
Spring 2012 IceBridge P-3 Flight Plans 12 March 2012 Draft compiled by John Sonntag Introduction to Flight Plans This document is a translation of the NASA Operation IceBridge (OIB) scientific objectives articulated in the Level 1 OIB Science Requirements, at the January IceBridge Greenland planning meeting held at NASA's Goddard Space Flight Center, through official science team telecons and through e-mail communication and iterations into a series of operationally realistic flight plans, intended to be flown by NASA's P-3 aircraft, beginning in mid- March and ending in late May 2012. The material is shown on the following pages in the distilled form of a map and brief text description of each science flight. Google Earth (KML) versions of these flight plans are available via anonymous FTP at the following address: ftp://atm.wff.nasa.gov/outgoing/oibscienceteam/. Note that some users have reported problems connecting to this address with certain browsers. Command-line FTP and software tools such as Filezilla may be of help in such situations. For each planned mission, we give a map and brief text description for the mission, and in the page header we also list the base it is to be flown from. At the end of the document we add an appendix of supplementary information, such as more detailed maps of certain missions and composite maps where several missions are designed to work together. A careful reader may notice that some of the mission maps in the main part of the document highlight flightlines in green, yellow, and red colors, while other only show the black lines.