Monitoring Fjord Circulation Using Iceberg-Mounted Gps As
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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 ...................................................................................................................... -
SUPPLEMENTARY INFORMATION Supplementary Information DOI: 10.1038/NGEO1481
SUPPLEMENTARY INFORMATION Supplementary information DOI: 10.1038/NGEO1481 An aerial view of 80 years of climate-related glacier fluctuations in southeast Greenland Anders A. Bjørk1*, Kurt H. Kjær1, Niels J. Korsgaard1, Shfaqat A. Khan2, Kristian K. Kjeldsen1, Camilla S. Andresen3, Jason E. Box4,5, Nicolaj K. Larsen6 and Svend Funder1 1Centre for GeoGenetics, Natural History Museum of Denmark, University of Copenhagen, Copenhagen, Denmark 2DTU Space - National Space Institute, Technical University of Denmark, Department of Geodesy, Copenhagen, Denmark. 3Geological Survey of Denmark and Greenland, Department of Marine Geology and Glaciology, Copenhagen, Denmark. 4Department of Geography, The Ohio State University, Columbus, Ohio, USA 5Byrd Polar Research Center, The Ohio State University, Columbus, Ohio, USA 6Department of Geocience, Aarhus University, Aarhus, Denmark *e-mail: [email protected] 1. Data 2. Methods 2.1 Image selection strategy 2.2 1981/1985 Digital Elevation Models and ortho-mosaics 2.3 Ortho-mosaics from 1981 and 1985 aerial photos 2.4 Control of the imagery 2.5 Digitization and error assessment 2.6 Glacier length measurements 2.7 Land-terminating elevation change 2.8 Regional differentiation and glacier subdivision 3. Additional climate data 4. Results 4.1 List of measured glaciers 4.2 Supplementary regional changes 4.3 Mid-Century advance 4.4 Unknown time of exposure for “1943” images 5. Supplementary information references 1 NATURE GEOSCIENCE | www.nature.com/naturegeoscience 1 © 2012 Macmillan Publishers Limited. All rights reserved. 1. Data 1932/1933 Imagery Images were recorded primarily for cartography during the 7th Thule Expedition to southeast Greenland, led by the Danish/Greenlandic scientist and explorer Knud Rasmussen. -
Helheim Glacier Terminus of More Than 3.8 M W.Eq
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 4, 1195–1224, 2010 The Cryosphere www.the-cryosphere-discuss.net/4/1195/2010/ Discussions TCD doi:10.5194/tcd-4-1195-2010 4, 1195–1224, 2010 © Author(s) 2010. CC Attribution 3.0 License. Freshwater flux to This discussion paper is/has been under review for the journal The Cryosphere (TC). Sermilik Fjord, Please refer to the corresponding final paper in TC if available. SE Greenland S. H. Mernild et al. Freshwater flux to Sermilik Fjord, SE Greenland Title Page Abstract Introduction S. H. Mernild1, G. E. Liston2, I. M. Howat3, Y. Ahn3, K. Steffen4, B. Hasholt5, 5 5 6 B. H. Jakobsen , B. Fog , and D. van As Conclusions References 1 Climate, Ocean, and Sea Ice Modeling Group, Computational Physics and Methods (CCS-2), Tables Figures Los Alamos National Laboratory, New Mexico, USA 2Cooperative Institute for Research in the Atmosphere, Colorado State University, J I Colorado, USA 3 Byrd Polar Research Center and School of Earth Sciences, Ohio State University, Ohio, USA J I 4Cooperative Institute for Research in Environmental Sciences, University of Colorado, Colorado, USA Back Close 5Department of Geography and Geology, University of Copenhagen, Denmark Full Screen / Esc 6Geological Survey of Denmark and Greenland, 1350 Copenhagen K, Denmark Received: 29 June 2010 – Accepted: 6 July 2010 – Published: 30 July 2010 Printer-friendly Version Correspondence to: S. H. Mernild ([email protected]) Interactive Discussion Published by Copernicus Publications on behalf of the European Geosciences Union. 1195 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD Fluctuations in terrestrial surface freshwater flux to Sermilik Fjord, SE Greenland, were simulated and analyzed. -
Freshwater Flux to Sermilik Fjord, SE Greenland
The Cryosphere, 4, 453–465, 2010 www.the-cryosphere.net/4/453/2010/ The Cryosphere doi:10.5194/tc-4-453-2010 © Author(s) 2010. CC Attribution 3.0 License. Freshwater flux to Sermilik Fjord, SE Greenland S. H. Mernild1, I. M. Howat2, Y. Ahn2, G. E. Liston3, K. Steffen4, B. H. Jakobsen5, B. Hasholt5, B. Fog5, and D. van As6 1Climate, Ocean, and Sea Ice Modeling Group, Computational Physics and Methods (CCS-2), Los Alamos National Laboratory, New Mexico, USA 2Byrd Polar Research Center and School of Earth Sciences, Ohio State University, Ohio, USA 3Cooperative Institute for Research in the Atmosphere, Colorado State University, Colorado, USA 4Cooperative Institute for Research in Environmental Sciences, University of Colorado, Colorado, USA 5Department of Geography and Geology, University of Copenhagen, Denmark 6Geological Survey of Denmark and Greenland, Denmark Received: 29 June 2010 – Published in The Cryosphere Discuss.: 30 July 2010 Revised: 13 October 2010 – Accepted: 16 October 2010 – Published: 26 October 2010 Abstract. Terrestrial inputs of freshwater flux to Sermi- 1 Introduction lik Fjord, SE Greenland, were estimated, indicating ice dis- charge to be the dominant source of freshwater. A freshwa- Global atmospheric temperatures showed a warming trend − ter flux of 40.4 ± 4.9×109 m3 y 1 was found (1999–2008), since the 1970s, and all years during the present century with an 85% contribution originated from ice discharge (65% (2001–2008) have been among the warmest since the begin- alone from Helheim Glacier), 11% from terrestrial surface ning of instrumental records (Allison et al., 2009). Surface runoff (from melt water and rain), 3% from precipitation air temperature observations reveal the strongest increase at the fjord surface area, and 1% from subglacial geother- occurring over Northern Hemisphere land areas (40–70◦ N) mal and frictional melting due to basal ice motion. -
1 Rapid Response of Helheim Glacier, Greenland, to Climate Variability
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Woods Hole Open Access Server Rapid response of Helheim Glacier, Greenland, to climate variability over the last century Camilla S. Andresen1*, Fiammetta Straneo2, Mads Hvid Ribergaard3, Anders A. Bjørk4, Thorbjørn J. Andersen5, Antoon Kuijpers1, Niels Nørgaard-Pedersen1, Kurt H. Kjær4, Frands Schjøth6, Kaarina Weckström1, Andreas P. Ahlstrøm1 1Geological Survey of Denmark and Greenland, Department of Marine Geology and Glaciology, Øster Voldgade 10, 1350 Copenhagen K, Denmark 2Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA 3Danish Meterological Institute, Centre for Ocean and Ice, Lyngbyvej 100, 2100 Copenhagen Ø, Denmark 4Centre for GeoGenetics, Natural History Museum, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark 5Institute for Geology and Geography, Øster Voldgade 10, Univ. of Copenhagen, 1350 Copenhagen K, Denmark 6Geological Survey of Denmark and Greenland, Geological Data Centre, Øster Voldgade 10, 1350 Copenhagen K, Denmark * email: [email protected] During the early 2000s the Greenland Ice Sheet experienced the largest ice mass loss observed on the instrumental record1, largely as a result of the acceleration, thinning and retreat of major outlet glaciers in West and Southeast Greenland2-5. The quasi-simultaneous change in 1 the glaciers suggests a common climate forcing and increasing air6 and ocean7-8 temperatures have been indicated as potential triggers. Here, we present a new record of calving activity of Helheim Glacier, East Greenland, extending back to c. 1890 AD. This record was obtained by analysing sedimentary deposits from Sermilik Fjord, where Helheim Glacier terminates, and uses the annual deposition of sand grains as a proxy for iceberg discharge. -
Freshwater Flux to Sermilik Fjord, SE Greenland
The Cryosphere, 4, 453–465, 2010 www.the-cryosphere.net/4/453/2010/ The Cryosphere doi:10.5194/tc-4-453-2010 © Author(s) 2010. CC Attribution 3.0 License. Freshwater flux to Sermilik Fjord, SE Greenland S. H. Mernild1, I. M. Howat2, Y. Ahn2, G. E. Liston3, K. Steffen4, B. H. Jakobsen5, B. Hasholt5, B. Fog5, and D. van As6 1Climate, Ocean, and Sea Ice Modeling Group, Computational Physics and Methods (CCS-2), Los Alamos National Laboratory, New Mexico, USA 2Byrd Polar Research Center and School of Earth Sciences, Ohio State University, Ohio, USA 3Cooperative Institute for Research in the Atmosphere, Colorado State University, Colorado, USA 4Cooperative Institute for Research in Environmental Sciences, University of Colorado, Colorado, USA 5Department of Geography and Geology, University of Copenhagen, Denmark 6Geological Survey of Denmark and Greenland, Denmark Received: 29 June 2010 – Published in The Cryosphere Discuss.: 30 July 2010 Revised: 13 October 2010 – Accepted: 16 October 2010 – Published: 26 October 2010 Abstract. Terrestrial inputs of freshwater flux to Sermi- 1 Introduction lik Fjord, SE Greenland, were estimated, indicating ice dis- charge to be the dominant source of freshwater. A freshwa- Global atmospheric temperatures showed a warming trend − ter flux of 40.4 ± 4.9×109 m3 y 1 was found (1999–2008), since the 1970s, and all years during the present century with an 85% contribution originated from ice discharge (65% (2001–2008) have been among the warmest since the begin- alone from Helheim Glacier), 11% from terrestrial surface ning of instrumental records (Allison et al., 2009). Surface runoff (from melt water and rain), 3% from precipitation air temperature observations reveal the strongest increase at the fjord surface area, and 1% from subglacial geother- occurring over Northern Hemisphere land areas (40–70◦ N) mal and frictional melting due to basal ice motion. -
Measures Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 3
MEaSUREs Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 3 USER GUIDE How to Cite These Data As a condition of using these data, you must include a citation: Howat, I. 2021. MEaSUREs Greenland Ice Velocity: Selected Glacier Site Velocity Maps from Optical Images, Version 3. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. https://doi.org/10.5067/RRFY5IW94X5W. [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 3 TABLE OF CONTENTS 1 DATA DESCRIPTION ................................................................................................................. 2 Parameters ............................................................................................................................................ 2 File Information ...................................................................................................................................... 2 1.2.1 Format.......................................................................................................................................... 2 1.2.2 File Contents ................................................................................................................................ 2 1.2.3 Naming Convention ....................................................................................................................