IceBridge MCoRDS L2 Ice Thickness

This data set contains depth sounder measurements of elevation, surface, bottom, and thickness for Greenland and Antarctica taken from the Multichannel Coherent Radar Depth Sounder (MCoRDS). The data were collected as part of Operation IceBridge funded aircraft survey campaigns..

Operation IceBridge products may include test flight data that are not useful for research and scientific analysis. Test flights usually occur at the beginning of campaigns. Users should read flight reports for the flights that collected any of the data they intend to use. Check IceBridge campaign Flight Reports for dates and information about test flights.

Table of Contents

  1. Contacts and Acknowledgments
  2. Detailed Data Description
  3. Data Access and Tools
  4. Data Acquisition and Processing
  5. References and Related Publications
  6. Document Information

Citing These Data

We kindly request that you cite the use of this data set in a publication using the following citation example. For more information, see our Use and Copyright Web page.

Leuschen, Carl, and Chris Allen. 2010, updated 2014. IceBridge MCoRDS L2 Ice Thickness, [indicate subset used]. Boulder, Colorado USA: National Snow and Ice Data Center. http://nsidc.org/data/irmcr2.html.

Overview

Platform

NASA DC-8
NASA P-3B

Sensor

MCoRDS

Spatial Coverage

Antarctica and Greenland

Spatial Resolution

Spatial Resolution ranges from 17.8 m to 965 m dependent on along-track, cross-track, and aircraft height characteristics.

Temporal Coverage

Ongoing, 16 October 2009 to the present.

Temporal Resolution

Seasonal

Parameters

Elevation
Surface
Bottom
Thickness

Data Format

Comma Separated Value (CSV) text

XML

Metadata Access

View Metadata Record

Get Data

FTP

Note: Data for 2009 Antarctica Twin Otter Radar Settings are temporarily available via a separate FTP location.

1. Contacts and Acknowledgments

Investigator(s) Name and Title

Carl Leuschen, Prasad Gogineni, Fernando Rodriguez, John Paden, Chris Allen
CReSIS
Nichols Hall 2335 Irving Hill Road
University of Kansas
Lawrence, Kansas 66045

Technical Contact

NSIDC User Services
National Snow and Ice Data Center
CIRES, 449 UCB
University of Colorado
Boulder, CO 80309-0449  USA
phone: +1 303.492.6199
fax: +1 303.492.2468
form: Contact NSIDC User Services
e-mail: nsidc@nsidc.org

Acknowledgements

The radar depth sounder data and data products from Center for Remote Sensing of Ice Sheets (CReSIS) have been collected on an ongoing basis since 1993 using grant funding from NASA and NSF. The most recent data were collected as part of the NSF Science and Technology Center grant (ANT-0424589) and the NASA Operation IceBridge field campaign (NNX10AT68G).

CReSIS faculty, staff, and students designed, developed, operated, and processed data from the radar systems.

2. Detailed Data Description

The data set includes measurements for Elevation, Surface, Bottom, and Thickness.

Format

The IceBridge MCoRDS L2 files are in CSV text files.

Each data file is paired with an associated XML file. The XML files contain location, platform, and instrument metadata.

The radar data are divided into segments. A segment is a contiguous data set in which the radar settings do not change. A day is divided into segments if the radar settings were changed, hard drives were switched, or other operational constraints required that the radar recording be turned off and on. The segment ID is YYYYMMDD_SS where YYYY is the four-digit year, MM is the two-digit month from 1 to 12, DD is the two-digit day of the month from 1 to 31, and SS is the segment number from 0 to 99. Segments are always sorted in the order in which the data were collected. Generally SS starts with 1 and increments by 1 for each new segment, but this is not always the case; only the ordering is guaranteed to match the order of data collection.

File and Directory Structure

The data set includes measurements for Elevation, Surface, Bottom, and Thickness.

Format

The MCoRDS L2 Ice Thickness files are in Comma-Separated Values (CSV) text files.

File and Directory Structure

CSV files are organized into date-named folders, such as:

/2013.04.20/
/2013.04.23/
/2013.04.25/
/2013.04.26/

File Naming Convention

The CSV and KML files are named according to the following conventions. File name variables are described in Table 1:

IRMCR2_Data_20120517_02.csv

IRMCR2_Data_YYYYMMDD_SS.csv

Where:

Table 1. File Naming Convention
Variable Description
IRMCR2 Short name for IceBridge MCoRDS L2 Ice Thickness
Data Data file
YYYY 4-digit year
MM 2-digit month
DD 2-digit day
SS flight segment number
.csv indicates comma separated value ASCII text file
.xml indicates XML file

File Size

CSV text files range from approximately 44 KB to 456 MB.

XML files range from approximately 4 KB to 165 KB.

Volume

The entire data set is approximately 1.4 GB.

Spatial Coverage

Spatial coverage for the IceBridge MCoRDS campaigns includes Antarctica and Greenland.

Antarctic:
Southernmost Latitude: 90° S
Northernmost Latitude: 63° S
Westernmost Longitude: 180° W
Easternmost Longitude: 180° E

Greenland:
Southernmost Latitude: 59° N
Northernmost Latitude: 83° N
Westernmost Longitude: 74° W
Easternmost Longitude: 12° W

Spatial Resolution

Spatial Resolution varies by surface characteristics and aircraft flown, as shown in Table 2.

Table 2. Spatial Resolution
Surface Characteristics DC-8 Antarctica P-3 Greenland
Smooth surface, across-track 641 m resolution where aircraft height = 500 m and ice thickness = 2000 m.

1518 m resolution where aircraft height = 8000 m and ice thickness = 2000 m.
323 m where height above the air/ice interface = 500 m and ice thickness = 2000 m.
Rough surface, across-track 965 m resolution where aircraft height = 500 m and ice thickness = 2000 m.

5416 m resolution where aircraft height = 8000 m and ice thickness = 2000 m.
651 m where height above the air/ice interface = 500 m, and ice thickness = 2000 m.
Along-track The final product has an along-track resolution of about 25 m and a sample spacing of about 14 m. The final product has an along-track resolution of about 25 m and a sample spacing of about 14 m.
Depth 17.8 m resolution. 4.5 m resolution. Actual target location is ambiguous for a rough surface since the off-nadir returns in the antenna footprint can hide the nadir return. The ice thickness is still close to correct, but may not be for the nadir return.

Projection and Grid Description

These data are provided in WGS-84 geodetic coordinates and WGS-84 ellipsoid elevation reference. Image files are in Operation IceBridge polar stereographic projections for Greenland Standard Parallel 70° N and Longitude of the Origin 45° W, and Antarctica Standard Parallel 71° S and Longitude of the Origin 0° E.

Temporal Coverage

These data were collected as part of Operation IceBridge funded campaigns from 16 October 2009 to the present.

Temporal Resolution

IceBridge campaigns are conducted on an annual repeating basis. Arctic and Greenland campaigns are conducted during March, April, and May, and Antarctic campaigns are conducted during October and November.

Parameter or Variable

The MCoRDS L2 Ice Thickness data set contains measurements for Elevation, Surface, Bottom and Thickness.

Parameter Description

The .CSV ASCII text files contain fields as described in Table 3.

Table 3. CSV ASCII Text File Parameters, Description, and Units
Parameter Description Units
Latitude Latitude Degrees North
Longitude Longitude Degrees East
Time UTC Time Seconds of day
Thickness Ice Thickness: Bottom minus Surface. Constant dielectric of 3.15 (no firn) is assumed for converting propagation delay into range. -9999 indicates no thickness available. Meters
Elevation Elevation referenced to WGS-84 Ellipsoid. Meters
Frame (YYYYMMDDSSFFF) Fixed length numeric field. YYYY = year, MM = month, DD = day, SS = segment
FFF = frame.
N/A
Surface Range to Ice Surface. Actual surface height is Elevation minus this number. Meters
Bottom Range to Ice Bottom. Actual ice bottom height is Elevation minus this number. Constant dielectric of 3.15 (no firn) is assumed for converting propagation delay into range. -9999 indicates no thickness available. Meters
Quality 1: High confidence pick
2: Medium confidence pick
3: Low confidence pick
NA

Note: When aligning with GPS time tagged data, account for leap seconds.

Sample Data Record

Below is an excerpt from data file IRMCR2_Data_20101026_01.csv. The fields in each record correspond to the columns described in Table 3.

3. Data Access and Tools

Get Data

Data are available via FTP.

Note: Data for 2009 Antarctica Twin Otter Radar Settings are temporarily available via a separate FTP location.

Software and Tools

CSV files may be opened by any text viewing program. KML files are read by GIS software packages and earth browsers such as Google Earth or Google Maps.

4. Data Acquisition and Processing

Theory of Measurements

Ice thickness is typically determined using data collected from waveforms with different pulse durations. Generally, all receive channels are used to produce the best result. The two reflections that are of most interest are the ice surface and ice bottom. The difference in the propagation time between the ice surface and ice bottom reflections is then converted into ice thickness using an estimated ice index of refraction of ice (square root of 3.15). The media is assumed to be uniform, i.e. no firn correction is applied.

Data collection modes used for typical operation are described below in the Data Acquisition Methods section.

Data Acquisition Methods

P-3 Low Altitude

A waveform with a 1-µs duration and lower receiver gain settings is used to measure the round-trip signal time for the surface echo, while a waveform with a 10-µs duration and higher receiver gain settings is used to measure the round-trip signal time for the bed echo. The two different waveforms are used because of the large dynamic range of signal powers that are observed. The 10-µs duration and higher receiver gain settings are more sensitive to the bed echo, but the signal is generally saturated from the ice surface and upper internal layers.

DC-8 Low Altitude

The same concept is used as for the P-3. However, during the first two field seasons (2009 Antarctica DC-8 and 2010 Greenland DC-8), extra antennas inside the cabin were used to detect the ice surface delay time because the Transmit/Receive (TR) switches did not meet their switching time specification. The TR switches have not been fixed in subsequent field seasons, but the TR switch control signals have been set so that the surface echo is generally still detectable, although with diminished power, even for very low altitudes down to 600 feet Above Ground Level (AGL).

P-3 High Altitude and DC-8 High Altitude

The dynamic range between the ice surface and ice bottom echoes is much smaller and a single high-gain and long pulse duration waveform is used to capture both echoes.

2009 Antarctica DC-8 Radar Settings

Bandwidth: 180-210 MHz (DC-8 platform restricted to 189.15-198.65 MHz)
Tx power: 550 W
Waveform: eight channel chirp generation, 14 bit ADC at 111 MHz bandpass sampling
Acquisition: eight channels
Dynamic Range: waveform playlist
Rx Aperture: 1.5 wavelength aperture
Tx Aperture: 1.5 wavelength aperture; fully programmable
Monostatic Rx/Tx
Data rate: 12 MB/sec per channel

2009 Antarctica Twin Otter Radar Settings

Bandwidth: 140-160 MHz
Tx power: 500 W
Waveform: eight channel chirp generation
Acquisition: eight channels
Rx Aperture: 3 wavelength aperture
Tx Aperture: 3 wavelength aperture; fully programmable
Bistatic Rx/Tx
Data rate: 12 MB/sec per channel

2010 Antarctica DC-8 Radar Settings

Dynamic Range: waveform playlist coupled with low gain and high gain channels

2010 Greenland P-3 Radar Settings

Bandwidth: 180-210 MHz (EMI restricted to 10 MHz within 180-210 MHz most segments)
Tx power: 600 W
Waveform: eight channel chirp generation
Acquisition: sixteen channels (multiplexed on to 8 channels), 14 bit ADC at 111 MHz bandpass sampling
Rx Aperture: 2 wavelength, 3.5 wavelength, and 2 wavelength apertures, baseline of 6.4 m between each aperture
Tx Aperture: 3.5 wavelength aperture; fully programmable
Mixed monostatic and bistatic tx/rx
Data rate: 6 MB/sec per channel

2011 Antarctica DC-8 Radar Settings

Dynamic Range: waveform playlist coupled with low gain and high gain channels

2011 Antarctica Twin Otter Radar Settings

Tx power: 1500 W
Rx Aperture: two 3 wavelength apertures with 13.8 m baseline
Tx Aperture: 3 wavelength aperture; fully programmable

2011 Greenland Twin Otter Radar Settings

Bandwidth: 180-210 MHz
Tx power: 500 W
Waveform: eight channel chirp generation
Acquisition: sixteen channels (multiplexed onto 8 channels), 14 bit ADC at 111 MHz bandpass sampling
Rx Aperture: two 3 wavelength apertures with 13.8 m baseline
Tx Aperture: 3 wavelength aperture; fully programmable
Mixed monostatic and bistatic tx/rx
Data rate: 6 MB/sec per channel

2011 Greenland P-3 Radar Settings

Bandwidth: 180-210 MHz
Tx power: 1050 W
Waveform: Eight channel chirp generation
Acquisition: sixteen channels, 14 bit ADC at 111 MHz bandpass sampling
Dynamic Range: waveform playlist
Rx Aperture: 2 wavelength, 3.5 wavelength, and 2 wavelength apertures, baseline of 6.4 m between each aperture
Tx Aperture: 3.5 wavelength aperture; fully programmable
Mixed monostatic and bistatic tx/rx
Data rate: 32 MB/sec per channel

Processing Steps

The layer tracking of ice surface and ice bottom reflections are manually driven processes with basic tools for partial automation. The tools used are determined by the operator picking the data and include:

  1. Manual picking and interpolation.
  2. Snake tracker which follows the strongest return within a window centered on the last tracked location from range line to range line.
  3. Leading edge detector searches for the crossing of a threshold beneath the peak return.
  4. Peak detector.

Various processing outputs, for example Minimum Variance Distortionless Response (MVDR), standard, quick look, dynamic range of the image, averaging, and detrending methods are used to better highlight features in the echogram as needed.

For further detail on data processing, including algorithms, see the Data Processing section in the IceBridge MCoRDS L1B Geolocated Radar Echo Strength Profiles documentation.

Version History

On April 12, 2011, the 2009 Antarctica MCoRDS L2 data were replaced by V01.1. The original 2009 Antarctica data were processed through a temporary process with quick look data products only. V01.1 data are produced from full Synthetic Aperture Radar (SAR) processing.

On October 17, 2011, the MCoRDS L2 data were replaced by V01.2. The csv_good and CSARP_layer data were removed from the previous version.

Error Sources

The data are not radiometrically calibrated. This means that they are not converted to some absolute standard for reflectivity or backscattering analysis. The MCoRDS science team is working on data processing and hardware modifications to do this.

The primary error sources for ice penetrating radar data are system electronic noise, multiple reflectors also known as multiples, and off-nadir reflections. Each of these error sources can create spurious reflections in the trace data leading to false echo layers in profile data. Multiple reflectors arise when the radar energy reflects off two surfaces more than once (or resonates) in the vertical dimension, and then returns to the receive antenna. Reflections occur in situations when two or more large reflectors are present with large electromagnetic constitutive property changes, such as the ice surface (air/ground), the bottom of the ice, and the aircraft body which is also a strong reflector. The radar receiver only records time since the radar pulse was emitted, so the radar energy that traveled the additional path length appears later in time, apparently deeper in the ice or even below the ice-bedrock interface. Note that multiples of a strong continuous reflector have a similar shape because the propagation time is a multiple of the resonance cavity. The most common multiple is between the air-ice surface and the aircraft. This "surface" multiple shows up at twice the propagation time as the original surface return and all the slopes are doubled.

Off-nadir reflections can result from crevasse surfaces, water, rock outcrops, or metal structures. Antenna beam structure and processing of the data are designed to reduce these off-nadir reflected energy sources.

2009 Antarctica DC-8 Specific Issues

Transmit/Receive Switch: During the first two field seasons (2009 Antarctica DC-8 and 2010 Greenland DC-8), extra antennas inside the cabin were used to detect the ice surface delay time because the TR switches did not meet their switching time specification. The TR switches have not been fixed in subsequent field seasons, but the TR switch control signals have been set so that the surface echo is generally still detectable, although with diminished power, even for very low altitudes down to 600 ft. AGL.

Some of the data collected during this season are from high altitude. The high altitude data are generally lower quality than the low altitude data. This is because:

  1. the cross-track antenna resolution is proportional to range creating severe layover problems in mountainous terrain, for example 05 November 2009 high altitude peninsula flight.
  2. the sidelobes from the long pulse duration mask out some of the returns that otherwise would have had a high enough signal to noise ratio.
  3. the range to target is greater so the spherical spreading power loss is greater leading to a lower signal to noise ratio.

Monostatic elements: All monostatic elements used for transmit and receive have an unknown fast-time gain profile because the transmit/receive switches take about 10 microseconds to fully switch positions. This fast-time gain profile has not been corrected so that using the surface or shallow layer returns for antenna equalization or for radiometric purposes is not recommended. All five of the antennas on the DC-8 are monostatic antennas.

2010 Antarctica DC-8 Specific Issues

Transmit/Receive Switch: This is a similar problem as with the 2009 Antarctica DC-8 season. However, we were able to set the TR switch control signals so that the surface is recoverable with the regular array down to an altitude of 600 ft. AGL but with very much reduced signal strength. The regular array is preferred over the EMI antenna setup because the radiation pattern characteristics are better. At an altitude of 1500 ft., no degradation in signal detectability is observed.

High altitude data: See 2009 Antarctica DC-8.

Monostatic elements: See 2009 Antarctica DC-8.

2010 Greenland DC-8 Specific Issues

One of the in-cabin Electromagnetic Interference (EMI) antennas is used to produce the quick look data product. The EMI antennas were not designed to receive the surface return. However, the transmit-receive switch for the primary array was set so that the surface returns for platform altitudes below 1500 feet were greatly attenuated. Because of this, the EMI antennas are used for picking the surface return at low altitude.

2010 Greenland P-3 Specific Issues

Monostatic elements: See 2009 Antarctica DC-8. Only the center seven elements are monostatic on the P-3.

EMI: Due to lack of shielding, a noisy switching power supply, and potentially other unidentified sources the radar was operated with 10 MHz bandwidth (190-200 MHz) for most of the field season. The signal quality is still lower than expected in this band due to broadband noise which is present at all times and periodic burst noise from other pulsed instruments on the P-3 and from random burst noise. The noise present at all times manifests itself as an increase in the noise floor and the burst noise manifests itself as smeared point targets.

2011 Greenland P-3 Specific Issues

The MCoRDS2 data acquisition system fielded for the first time this season has a known issue with radar data synchronization with GPS data. The synchronization time correction that must be added to the radar time stamp is either 0 or -1 second. When the radar system is initially turned on, the radar system acquires Universal Time Coordinated (UTC) time from the GPS National Marine Electronics Association (NMEA) string. If this is done too soon after the GPS receiver has been turned on, the NMEA string sometimes returns GPS time rather than UTC time. GPS time is 15 seconds ahead of UTC time during this field season. The corrections for the entire day must include the offset, either -15 or -16 seconds. GPS corrections have been applied to all of the data using a comparison between the accumulation radar and the MCoRDS radar. The accumulation radar from 2011 is known to have only the GPS/UTC problem. The GPS/UTC problem is easily detectable by comparing the data to raster imagery, so the only correction that could be in error is the 0 or -1 second offset and this generally happens when there are no good features in or above the ice to align the accumulation and MCoRDS2 radars. GPS time corrections and frames where no good sync information was available are given in the vector worksheet of the Parameter Spreadsheet.

Two of the missions, SE Glaciers on 11 April 2011 and Helheim/Kanger/Midguard on 19 April 2011, suffered from radar configuration failures and about 40 dB of sensitivity was lost on the high gain channel. Short portions of these data are still good so the datasets are published, but most of the data are not useful.

Sensor or Instrument Description

As described on the CReSIS Sensors Development Radar Page, the Multichannel Coherent Radar Depth Sounder operates over a 180 to 210 MHz frequency range with multiple receivers developed for airborne sounding and imaging of ice sheets. Measurements are made over two frequency ranges: 189.15 to 198.65 MHz, and 180 to 210 MHz. The radar bandwidth is adjustable from 0 to 30 MHz. Multiple receivers permit digital beamsteering for suppressing cross-track surface clutter that can mask weak ice-bed echoes and strip-map SAR images of the ice-bed interface. These radars are flown on twin engine and long-range aircraft including NASA P-3, Twin Otter (TO), and DC-8. GPS time corrections and frames where no good sync information was available are given in the vector worksheet in the Parameter Spreadsheet

5. References and Related Publications

Akins, Torry Lee. 1999. Design and development of an improved data acquisition system for the coherent radar depth sounder, Department of Electrical Engineering and Computer Science: Master's Thesis, University of Kansas.

Allen, Christopher, Lei Shi, Richard Hale, Carl Leuschen, John Paden, Benjamin Panzer, Emily Arnold, William Blake, Fernando Rodriguez-Morales, John Ledford, Sarah Seguin. 2011. Antarctic Ice Depth Sounding Radar Instrumentation for the NASA DC-8, submitted for publication to IEEE Transactions on Aerospace and Electronic Systems, August 2011.

Blake, W., J. Ledford, C. Allen, C. Leuschen, S. Gogineni, F. Rodriguez-Morales, Lei Shi. 2008. A VHF Radar for Deployment on a UAV for Basal Imaging of Polar Ice. Geoscience and Remote Sensing Symposium. IGARSS 2008. IEEE International, 4: IV-498-IV-501, doi: 10.1109/IGARSS.2008.4779767.

Byers, K. J. 2011. Integration of a 15-Element, VHF Bow-Tie Antenna Array into an Aerodynamic Fairing on a NASA P-3 Aircraft, Department of Electrical Engineering and Computer Science: Master's Thesis, University of Kansas.

Byers, K. J. 2011. Integration of a 15-Element, VHF Bow-Tie Antenna Array into an Aerodynamic Fairing on a NASA P-3 Aircraft, Department of Electrical Engineering and Computer Science: Master's Thesis, University of Kansas.

Chuah, T. S. 1997. "Design and Development of a Coherent Radar Depth Sounder for Measurement of Greenland Ice Sheet Thickness", CReSIS Technical Report, 151: 175.

Fujita, Shuji, Takeshi Matsuoka, Toshihiro Ishida, Kenichi Matsuoka, and Shinji Mae. 2000. A Summary of the Complex Dielectric Permittivity of Ice in the Megahertz Range and its Application for Radar Sounding of Polar Ice Sheets. Physics of Ice Core Records, (185-212). T. Hondoh, Editor. Hokkaido University Press, 2000, Sapporo.

Gogineni, S., T. Chuah, C. Allen, K. Jezek, and R. K. Moore. 1998. An Improved Coherent Radar Depth Sounder, Journal of Glaciology 44(148): 659-669.

Gogineni, S., D. Tammana, D. Braaten, C. Leuschen, T. Akins, J. Legarsky, P. Kanagaratnam, J. Stiles, C. Allen, and K. Jezek. 2001. Coherent Radar Ice Thickness Measurements Over the Greenland Ice Sheet, Journal of Geophysical Research-Atmospheres 106(D24): 33761-33772.

Lei Shi; C. T. Allen, J.R. Ledford, F. Rodriguez-Morales, W. A. Blake, B. G. Panzer, S. C. Prokopiack, C. J. Leuschen, and S. Gogineni. 2010. Multichannel Coherent Radar Depth Sounder for NASA Operation Ice Bridge, Geoscience and Remote Sensing Symposium (IGARSS), IEEE International, (1729-1732), doi: 10.1109/IGARSS.2010.5649518.

Leuschen, Carl, Chris Allen, Prasad Gogineni, Fernando Rodriguez, John Paden, and Jilu Li. 2011, updated current year. IceBridge Snow Radar L1B Geolocated Radar Echo Strength Profiles, [list dates of data used]. Boulder, Colorado USA: National Snow and Ice Data Center. Digital media.

Leuschen, Carl, and Chris Allen. 2010, updated current year. IceBridge MCoRDS L1B Geolocated Radar Echo Strength Profiles, [list dates of data used]. Boulder, Colorado USA: National Snow and Ice Data Center. Digital media..

Leuschen, Carl, Chris Allen, Prasad Gogineni, Fernando Rodriguez, John Paden, and Jilu Li. 2011, updated current year. IceBridge MCoRDS L3 Gridded Ice Thickness, Surface, and Bottom, [list dates of data used]. Boulder, Colorado USA: National Snow and Ice Data Center. Digital media.

Li, Jilu, John Paden, Carl Leuschen, Fernando Rodriguez-Morales, Richard Hale, Emily Arnold, Reid Crowe, Daniel Gomez-Garcia and Prasad Gogineni. 2011. High-Altitude Radar Measurements of Ice Thickness over the Antarctic and Greenland Ice Sheets as a part of Operation Ice Bridge, submitted to IEEE Transactions on Geoscience and Remote Sensing, September 2011.

Namburi, S. P. V. 2003. Design and Development of an Advanced Coherent Radar Depth Sounder, Department of Electrical Engineering and Computer Science, Master's Thesis, University of Kansas.

Paden, John, Christopher Allen, Sivaprasad Gogineni, Kenneth Jezek, Dorthe Dahl-Jensen, and Lars Larsen. 2005. Wideband measurements of ice sheet attenuation and basal scattering, IEEE Geoscience and Remote Sensing Letters, (2)2.

Paden, J. 2006. Synthetic Aperture Radar for Imaging the Basal Conditions of the Polar Ice Sheets, Department of Electrical Engineering and Computer Science, PhD Dissertation, University of Kansas.

Paden, J., T. Akins, D. Dunson, C. Allen, and P. Gogineni. 2010. Ice-sheet bed 3-D tomography, Journal of Glaciology 56(195): 3-11.

Player, K., Lei Shi, Chris Allen, Carl Leuschen, John Ledford, Fernando Rodriguez-Morales, William Blake, Ben Panzer, and Sarah Seguin. 2010. A Multi-Channel Depth-Sounding Radar with an Improved Power Amplifier, High-Frequency Electronics, October 2010: 18-29.

Rodriguez-Morales, F., P. Gogineni, C. Leuschen, C. T. Allen, C. Lewis, A. Patel, L. Shi, W. Blake, B. Panzer, K. Byers, R. Crowe, L. Smith, and C. Gifford. 2010. Development of a Multi-Frequency Airborne Radar Instrumentation Package for Ice Sheet Mapping and Imaging, Proc. 2010 IEEE Int. Microwave Symp., Anaheim, CA, 2010: 157 – 160.

Shi, Lei, C.T. Allen, J.R. Ledford, F. Rodriguez-Morales, W.A. Blake, B.G. Panzer, S.C. Prokopiack, C.J. Leuschen, and S. Gogineni. 2010. Multichannel Coherent Radar Depth Sounder for NASA Operation Ice Bridge, Geoscience and Remote Sensing Symposium (IGARSS), 2010 IEEE International, 25-30 July 2010: 1729-1732.

Related Data Collections

Related Web Sites

  • CReSIS Website (https://www.cresis.ku.edu/)
  • CReSIS Sensors Development Radar Web Page (https://cms.cresis.ku.edu/research/sensors-development/radar).
  • IceBridge Data Web site at NSIDC (http://nsidc.org/data/icebridge/index.html).
  • IceBridge Web site at NASA (http://www.nasa.gov/mission_pages/icebridge/index.html).
  • ICESat/GLAS Web site at NASA Wallops Flight Facility (http://glas.wff.nasa.gov/).
  • ICESat/GLAS Web site at NSIDC (http://nsidc.org/daac/projects/lidar/glas.html).

6. Document Information

Acronyms and Abbreviations

The acronyms used in this document are listed in Table 4.

Table 4. Acronyms and Abbreviations
Acronym Description
AGL Above Ground Level
ASCII American Standard Code for Information Interchange
CIRES Cooperative Institute for Research in Environmental Science
CReSIS Center for Remote Sensing of Ice Sheets
CSV Comma Separated Value
DC-8 Douglas DC-8 aircraft
FTP File Transfer Protocol
GPS Global Positioning System
KML Keyhole Markup Language
L2 Processing Level 2
MCoRDS Multichannel Coherent Radar Depth Sounder
MVDR MVDR Minimum Variance Distortionless Response
NASA National Aeronautics and Space Administration
NSF National Science Foundation
NSIDC National Snow and Ice Data Center
P-3 Lockheed P-3B Orion aircraft
SAR Synthetic Aperture Radar
TR Transmit Receive
URL Uniform Resource Locator
UTC Universal Time Coordinated
WGS-84 World Geodetic System 1984

Document Creation Date

02 November 2011

Document Revision Date

17 April 2012

29 October 2012

13 November 2012

17 May 2013

17 February 2014

Document URL

http://nsidc.org/data/docs/daac/icebridge/irmcr2/index.html