SvalGlac Scientific Steering Committee Meeting Oslo, 30th October 2011 Ground Penetrating Radar Working Group Report 2011 Fot. T. Budzik Sites studied:

Slides:

Advertisements

Similar presentations

M.H Young 1, C.J. Abolt 1,2, T.G. Caldwell 1, T.E. Larson 2 High-Resolution Carbon Inventory and Dynamics in Permafrost Soils: North Slope, Alaska 1 Bureau.

Advertisements

Toward Enterprise GIS in Total E&P Indonesie Puguh SARWANTO (TOTAL E&P INDONESIE)

Estimates of Arctic Wetland Extent Using Ground Penetrating Radar Stefan Schultheiss 1 ; Christoph E. Geiss 2 ; Phil Camill 5 ; Mark B. Edlund 4 ; Charles.

Antarctic Ice Shelf 3D Cross-sectional Imaging using MIMO Radar A. Hari Narayanan UCL Electronic and Electrical Engineering, UK P. Brennan UCL Electronic.

Will Norway Arrange the International Geological Congress (IGC) in 2008? – Chances and Consequences! Presentation at the 18th Winter Conference Oslo 6.-8.

Collaborative Investigation of Climate Cryosphere Interaction 3 (CICCI 3) Rune Storvold, Norut/NTNU NySMAC, Helsinki, April 7 th -8 th, 2014.

Raw Data Saturated Ground Less Saturated Ground Transect 3 GEOPHYSICAL INVESTIGATION OF THE BURD-RUN BURIED STREAM CHANNEL IN COLLUVIAL FILL OF THE CUMBERLAND.

Spatial variability of interior ice-sheet accumulation determined with an FM-CW radar and connections to the NAO David Braaten, Prasad Gogineni, Claude.

Global warming and polar tidewater glacier response: A Canadian IPY project on Belcher Glacier, Nunavut B.Beauchamp Sarah Boon(1); Dave Burgess(2); Luke.

Using Ground Penetrating Radar to Detect Oil in Ice and Snow

electromagnetic method

SEAT Traverse The Satellite Era Accumulation Traverse (SEAT) collected near-surface firn cores and Ultra High Frequency (UHF) Frequency Modulated.

Ice studies off West Greenland 2006 Bureau of Minerals and Petroleum Government of Greenland Data compiled by Sine M Hvidegaard, Rene Forsberg, Susanne.

Climate history near the divide between the Ross and Amundsen Seas by H. Conway, Ed Waddington, Tom Neumann, Ginny Catania, Erin Pettit, Felix Ng and Dave.

Subglacial conditions of inland West Antarctica from US-ITASE deep radar reflection analysis WAIS Workshop September 30, 2005 Brian Welch, Bob Jacobel.

IceBridge Science Objectives The following are the major science objectives of Operation IceBridge in priority.

Coda attenuation analysis of Zagreb area, Croatia Iva Dasović, Marijan Herak and Davorka Herak Andrija Mohorovičić Geophysical Institute Department of.

Ventures Proposal Science Objectives and Requirements.

ICESat dH/dt Thinning Thickening ICESat key findings.

Ice Lenses at KAN-U, SW Greenland Credit: Karen Alley, University of ColoradoCredit: Babis Charalampidis, GEUS.

Report on National activities, 2012 Poland Waldemar Walczowski SAON Board Meeting, 1-2 October 2012 Potsdam.

GEOPHYSICAL SERVICES Presented By: Hans van de Vrugt, CEG, RGp Patrick F. Lehrmann, PG, RGp SOUTHWEST GEOPHYSICS.

Global Inter-agency IPY Polar Snapshot Year (GIIPSY): Goals and Accomplishments Katy Farness & Ken Jezek, The Ohio State University Mark Drinkwater, European.

Application of Near-Surface Geophysics to Agricultural Drainage Pipe Detection.

Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.

A Monitoring Program for Ny-Ålesund Christina A. Pedersen Norwegian Polar Institute.

Sea-ice freeboard heights in the Arctic Ocean from ICESat and airborne laser H. Skourup, R. Forsberg, S. M. Hvidegaard, and K. Keller, Department of Geodesy,

GIS Tools For Digital Field Geology: from paper to PDA Dr. Ben Crosby, ISU, Department of Geosciences.

Monitoring Earths ice sheets from space Andrew Shepherd School of Geosciences, Edinburgh.

Electrical Resistance Imaging Looking beneath the surface… Or Finding where the bodies are buried without a backhoe… And Looking for buried ice on the.

Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Center for Satellite Applications.

Video of wet core. Forster et al., 2014 Mapped with GPR and NASA airborne radar.

Shear wave velocity structure estimation using surface waves of different wavelengths Petr Kolínský Department of Seismology Institute of Rock Structure.

Plus an Introduction to the: Institute of Earth Science & Engineering RESOURCE INDEX MAPPING: Getting the Right Data for the Right Model.

Ground Penetrating Radar for Utilities mapping and Detection ์

8/12/201514th RHESSI Workshop 1 Dale E. Gary, Center for Solar-Terrestrial Research, Physics Department, NJIT.

A Decade of Frontier Oceanography Achievements during WAIS.

The McGill Arctic Research Station (MARS), Expedition Fjord, Axel Heiberg Island: Scientific and Logistical Overview.

SCADM report Arto Vitikka Arctic Centre, University of Lapland Rovaniemi Finland

1 Lawrence Berkeley National Laboratory, University of California, Earth Sciences Division 2 University of Oslo, Department of Geophysics,

Susceptibility models for pipe collapse in loess-derived soils in a temperate humid climate* A. Logistic regression Els Verachtert (1), Miet Van Den Eeckhaut.

Evolution of northern wetlands since the Last Glacial Maximum Pirita Oksanen, University of Bristol, School of Geographical Sciences Contact

Energy in the Earth System Surface Temperature measurements.

Inferred accumulation and thickness histories near the Ross/Amundsen divide, West Antarctica T. A. Neumann 1,2, H. Conway 2, S.F. Price 2, E. D. Waddington.

MULTIPLE LOW FREQUENCY (MLF) ANTENNA Authors: Almelu Mangamma V. Hebsur M.Tech (Remote Sensing) ‏ Department of Civil Engineering Indian Institute of Technology.

This material is based upon work supported by the National Science Foundation under Grant No. ANT Any opinions, findings, and conclusions or recommendations.

Using instrumented aircraft to bridge the observational gap between ICESat and ICESat-2.

An Overview of Glaciers and Icesheets Mapping Orbiter (GISMO) & Global Ice Sheet Interferometric Radar (GISIR) Ohio State University University of Kansas.

WAIS in ANDRILL Future Planning Frank R. Rack, David Harwood, Steve Fischbein ANDRILL Science Management Office University of Nebraska-Lincoln

Variations in mass balance and snow and firn densities along a transect in the percolation zone of the Greenland Ice Sheet Vicki Parry (1), Peter Nienow.

Polar Ice Sheets and Ice Shelves: Mass Balance, Uncertainties, and Potential Improvements Robert H Thomas…etc.

University of Kansas S. Gogineni, P. Kanagaratnam, R. Parthasarathy, V. Ramasami & D. Braaten The University of Kansas Wideband Radars for Mapping of Near.

Timing of high latitude peatland initiation since the Last Glacial Maximum Pirita Oksanen, University of Bristol, School of Geographical Sciences Contact.

Is mechanical heterogeneity controlling the stability of the Larsen C ice shelf? Bernd Kulessa 1, Daniela Jansen 1, Edward King 2, Adrian Luckman 1, Peter.

Environmental and Exploration Geophysics II tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,

Alpine Hydrogeology: Storage and Flow of Groundwater in Moraine and Talus Deposits Masaki Hayashi, Jaime Hood, Greg Langston, Danika Muir, Alastair McClymont,

 Obruchev Glacier is located in the Polar Urals. It is a typical temperate cirque glacier and it covers an area of 0.3 km 2. The glacier is 0.9 km long.

Mapping Greenland Using NASA’s Full- Waveform, Medium/High-Altitude, LVIS Lidar System: Potential 2009 Coverage and Expected Performance Michelle Hofton.

MARSIS Overview J. J. Plaut G. Picardi and the MARSIS Team.

A Combined Radar-Radiometer Approach to Estimate Rain Rate Profile and Underlying Surface Wind Speed over the Ocean Shannon Brown and Christopher Ruf University.

Sea ice thickness from airborne laser scanning Sine M. Hvidegaard, Rene Forsberg, Henriette Skourup, and others.

Spatial and temporal variability of the unsaturated zone characterised by geophysical and conventional methods H.K. French, Centre for Soil and Environmental.

Central Mining Institute

Measuring sea ice thickness using satellite radar altimetry

Compact Probe for In-Situ Optical Snow Grain Size Stratigraphy

SIOS (Svalbard Integrated

GPR Keren Engoltz and Semion Polinov Prof. Ammatzia Peled

NPOESS Airborne Sounder Testbed (NAST)

Summary of GPR Systems for Mars Exploration

Radar Methods – General Overview

Presentation transcript:

SvalGlac Scientific Steering Committee Meeting Oslo, 30th October 2011 Ground Penetrating Radar Working Group Report 2011 Fot. T. Budzik Sites studied: Teams involved: Departamento de Matemática Aplicada Departamento de Matemática Aplicada ETSI de Telecomunicación, Universidad Politécnica de Madrid Department of Geosciences, University of Oslo Department of Geosciences, University of Oslo Department of Earth Sciences, Uppsala University Department of Earth Sciences, Uppsala University Institute of Geography, Russian Academy of Sciences Institute of Geography, Russian Academy of Sciences Institute of Geophysics, Polish Academy of Sciences Institute of Geophysics, Polish Academy of Sciences Department of Geomorphology, University of Silesia Department of Geomorphology, University of Silesia

VIRL-6 radar with central frequency 20 MHz Gleditschfonna: 19.5 km of RES profiles performed 19.5 km of RES profiles performed Maximal ice thickness is 63.6 m, average ~30 m Maximal ice thickness is 63.6 m, average ~30 m Ice thickness Tungebreen : 12.5 km of RES profiles performed 12.5 km of RES profiles performed Maximal ice thickness is 88 m, average 43.4 m Maximal ice thickness is 88 m, average 43.4 m Ice thickness Fridtjovbreen: a few RES profiles to examine hydrothermal state a few RES profiles to examine hydrothermal state Fot. I. Lavrentiev

Department of Earth Sciences, Uppsala University Vestfonna (Nordaustlandet): low-frequency data and compilation a new bedrock map. low-frequency data and compilation a new bedrock map. Source: Pettersson et al. (in press). Ice thickness and basal conditions of Vestfonna ice cap eastern Svalbard. Geografiska Annaler. Department of Geosciences, University of Oslo Austfonna (Nordaustlandet): snow radar surveys across several profiles over the ice cap (ca. 400 km), with 800 MHz Ramac and with a 12 GHz radar for CryoSat calibration. snow radar surveys across several profiles over the ice cap (ca. 400 km), with 800 MHz Ramac and with a 12 GHz radar for CryoSat calibration.

Hansbreen Amundsenisen Laser altimetry profile 1996, 2002 Department of Geomorphology, University of Silesia Institute of Geophysics, Polish Academy of Sciences Hansbreen & Amundsenisen: Shallow soundings with 800 MHz cental frequency Shallow soundings with 800 MHz cental frequency Total lenght of GPR profiles: c.80 km (Hansbreen) and 66 km (Amundsenisen) Total lenght of GPR profiles: c.80 km (Hansbreen) and 66 km (Amundsenisen) Snow structure and depth supported by shallow coring and snow pits study Snow structure and depth supported by shallow coring and snow pits study Werenskioldbreen: profiling of frontal part and forefield with 100 MHz central frequency profiling of frontal part and forefield with 100 MHz central frequency Study of basal conditions (in connection with AWAKE project). Study of basal conditions (in connection with AWAKE project). Werenskioldbreen Fot. T. Budzik

Fieldwork carried out in Svalbard spring 2011 Joint venture Spain-Russia- Poland-Finland - Ground Penetrating Radar - Field Campaign Hornsund 2011 processed data non processed data* * Profiles made from helicopter EquipmentVIRL 7 antenae 20 MHz Participants (Spain/Russia) Francisco Navarro Evgeny Vasilenko Date April- May 2011 Logistics Polish Polar Station Profiles length Amundsenisen: 52.5 km Recherchebreen: 48.8 km Fligth*: km

Inventory of radio-echo sounded glaciers in Svalbard Database GPR glaciers Database glaciers with available thickness data