IceBridge Sea Ice Freeboard, Snow Depth, and Thickness

This data set contains derived geophysical data products including sea ice freeboard, snow depth, and sea ice thickness measurements in Greenland and the Arctic retrieved from IceBridge Snow Radar, Digital Mapping System (DMS), Continuous Airborne Mapping By Optical Translator (CAMBOT), and Airborne Topographic Mapper (ATM) sensors. The data were collected as part of Operation IceBridge funded campaigns, and are stored in ASCII text files.

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.

Kurtz, N., M. S. Studinger, J. Harbeck, V. Onana, and S. Farrell. 2012, updated 2014. IceBridge Sea Ice Freeboard, Snow Depth, and Thickness. Boulder, Colorado USA: NASA DAAC at the National Snow and Ice Data Center. http://nsidc.org/data/idcsi2.html.

Overview

Platform

NASA DC-8
NASA P-3B

Sensor

ATM, Snow Radar, DMS, CAMBOT

Spatial Coverage

Greenland and the Arctic

Spatial Resolution

Freeboard: 40 m length scale

Snow Depth: based on synthetic aperture dictated footprint size and averaged to a 40 m length scale in the along-track direction

Thickness: 40 m length scale

Temporal Coverage

31 March 2009 to present

Temporal Resolution

Seasonal

Parameters

Freeboard
Ice Depth/Thickness
Snow Depth

Data Format

ASCII text

Metadata Access

View Metadata Record

Get Data

FTP

1. Contacts and Acknowledgments

Investigator(s) Name and Title

Nathan Kurtz, Michael Studinger, Jeremy Harbeck, Vincent-De-Paul Onana
Cryospheric Sciences Laboratory
NASA Goddard Space Flight Center
Greenbelt, Maryland USA

Sinead Farrell
Earth System Science Interdisciplinary Center (ESSIC)
University of Maryland
College Park, Maryland USA

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 production of a sea ice and snow thickness product would not have been possible without the help of many people. We would like to thank the IceBridge Sea Ice Science team and members of the community for support and guidance. We would also like to thank the instrument teams and air crews for long hours in the field and at home collecting and processing the data and the National Snow and Ice Data Center for archiving and publishing the data. This work is funded by NASA's Airborne Science and Cryospheric Sciences Programs.

2. Detailed Data Description

Format

The data files are in comma delimited ASCII text format. Each data file is paired with an associated XML file. The XML files contain point latitude and point longitude, along with instrument, sensor, and campaign metadata.

File and Directory Structure

Data files are on the FTP site, ftp://n5eil01u.ecs.nsidc.org/SAN2/ICEBRIDGE/IDCSI2.001/ in folders organized by date, for example /2009.03.31/ to /2012.04.10/.

File Naming Convention

Data files are named according to the following convention and as described in Table 1:

IDCSI2_20110316.txt

IDCSI2_YYYYMMDD.txt

Where:

Table 1. File Naming Convention
Variable Description
IDCSI2 Short name for IceBridge Sea Ice Freeboard, Snow Depth, and Thickness
YYYY Four-digit year of data collection
MM Two-digit month of data collection
DD Two-digit day of data collection
.txt Indicates ASCII text file

File Size

Data files range from approximately 8 MB to 60 MB.

Volume

The entire data set is approximately 1.3 GB.

Spatial Coverage

Spatial coverage for the IceBridge Sea Ice Freeboard, Snow Depth, and Thickness parameters currently includes Greenland and the Arctic.

Greenland / Arctic:
Southernmost Latitude: 60° N
Northernmost Latitude: 90° N
Westernmost Longitude: 180° W
Easternmost Longitude: 180° E

Spatial Resolution

Freeboard: adjusted 40 m length scale.

Snow depth: at the 460 m nominal flight altitude the snow radar has a footprint size of 11 m across track dictated by the pulse-limited footprint size, and 14.5 m along-track dictated by the synthetic aperture formed. The data are averaged in the along-track direction to a 40 m length scale.

Thickness: estimates sea ice thickness over a 40 m length scale to provide the highest resolution available from the data.

Projection and Grid Description

ATM Data

Referenced to the ITRF-2005 reference frame and projected onto the WGS-84 ellipsoid.

Snow Radar Data

Referenced as a relative distance from the aircraft with latitude and longitude coordinates provided by the GPS system on the aircraft.

CAMBOT Images

Georeferenced as a series of camera locations: latitude, longitude, elevation and altitude above ground (WGS-84) and aircraft orientation roll, pitch, and heading.

DMS Images

Arctic. Polar Stereographic Standard Parallel 70° N, Longitude of the origin (central meridian): 45° W, WGS-84 ellipsoid.
Antarctic. Polar Stereographic Standard Parallel 71° S, Longitude of the origin (central meridian): 0°, WGS-84 ellipsoid.

Temporal Coverage

31 March 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

Parameter Description

The Sea Ice Freeboard, Snow Depth, and Thickness data files contain parameters as described in Table 2.

Table 2. File Parameters and Units
Parameter Description Units
lat Latitude Degrees
lon Longitude Degrees
thickness Sea ice thickness Meters
thickness_unc Sea ice thickness uncertainty Meters
mean_fb Mean freeboard from the combined ATM and DMS data set Meters
ATM_fb Mean freeboard from the ATM data set only (may be biased due to the loss of data over thin ice and water) Meters
fb_unc Freeboard uncertainty Meters
snow_depth Snow depth Meters
snow_depth_unc Snow depth uncertainty Meters
n_atm Number of ATM measurements used n/a
pcnt_ow Percentage of open water detected in the DMS imagery over the 40 m area n/a
pcnt_thin_ice Percentage of grease ice and/or nilas detected in the DMS imagery over the 40 m area n/a
pcnt_grey_ice Percentage of non-snow-covered grey ice detected in the DMS imagery over the 40 m area n/a
corr_elev Surface elevation after the removal of geoid, atmospheric pressure, and tidal corrections Meters
elev Mean ATM elevation Meters
date Date of measurement in YYYYMMDD format n/a
elapsed Elapsed time from the start of the day in UTC Seconds
atmos_corr Atmospheric pressure loading term Meters
geoid_corr Geoid value Meters
ellip_corr Conversion factor between the WGS-84 and Topex/Poseidon ellipsoids Meters
tidal_corr Sum of the ocean, load, and earth tides Meters
ocean_tide_corr_part Ocean tide for the sea surface height Meters
load_tide_corr_part Load tide for the sea surface height Meters
earth_tide_corr_part Solid earth tide for the sea surface height Meters
ssh Local interpolated sea surface height Meters
n_ssh Number of ATM measurements used to determine the nearest sea surface height estimate n/a
ssh_sd Standard deviation of ATM elevations used to determine the nearest sea surface height estimate Meters
ssh_diff Difference between the centroids of the final and initial Gaussian fits to the nearest sea surface height Meters
ssh_elapsed Elapsed time since the last sea surface height data point was encountered Seconds
ssh_tp_dist Distance to the nearest sea surface height tie point Meters
surface_roughness Standard deviation of the ATM elevation points in the 40 m grid Meters
ATM_file_name Name of the ATM file which the surface elevation measurements were from n/a
Tx Mean transmit signal strength (40 m resolution) of the ATM data Relative
Rx Mean received signal strength (40 m resolution) of the ATM data Relative
KT19_surf Surface temperature from the KT-19 instrument Celsius
KT19_int Internal temperature of the KT-19 instrument Celsius
low_en_corr Correction added to the ATM elevation data for low signal strength Meters
sa_int_elev Height of radar derived snow-air interface relative to the WGS-84 ellipsoid Meters
si_int_elev Height of radar derived snow-ice interface relative to the WGS-84 ellipsoid Meters
my_ice_flag Flag for ice type, 0: first year ice, 1: multi-year ice, from 12.5 km resolution AMSR-E data n/a
empty1...empty10 Empty columns which may be used in future versions n/a

Sample Data Record

The sample record shows the header and three records from the 2011 Greenland data file: OIB_20110316_IDCSI2.txt.

3. Data Access and Tools

Get Data

Data are available via FTP.

Software and Tools

The data files may be opened by any text editor or word processing program that reads ASCII text files.

A MATLAB program is available for reading the ASCII data files and displaying graphical representations of the data.

Quality Assessment

For details on data quality, see Sea Ice Thickness, Freeboard, and Snow Depth Products from Operation IceBridge Airborne Data (Kurtz et al. 2013).

4. Data Acquisition and Processing

This data set contains the geophysical data products sea ice thickness, freeboard, and snow depth retrieved from Operation IceBridge Level-1B ATM, Snow Radar, DMS, and CAMBOT data.

For instrument details related to specific campaigns, see Mission, Campaign, and Flight Specific Notes.

Data Acquisition Methods

IceBridge Sea Ice Freeboard, Snow Depth, and Thickness products are derived from four Operation IceBridge data sets:

Surface temperature data are provided by the KT-19 infrared pyrometer:

Figure 2 describes the retrieval of sea ice thickness, snow depth, and freeboard (Kurtz et al. 2013). In addition to the ATM and Snow Radar instruments, Operation IceBridge DMS and CAMBOT were used to identify features and surface types on the sea ice.

processing steps flow chart

Figure 2. Product Retrieval from Instrument Data

For details on specific seasonal campaigns, see the Appendix in the Operation IceBridge sea ice freeboard, snow depth, and thickness data products manual.

Derivation Techniques and Algorithms

IceBridge Sea Ice Freeboard, Snow Depth, and Thickness is a retrieval of three products obtained from IceBridge data.

Technical summaries are provided below. For further details on derivation techniques, algorithms, processing steps, and error sources, see Sea Ice Thickness, Freeboard, and Snow Depth Products from Operation IceBridge Airborne Data (Kurtz et al. 2013).

Sea Ice Freeboard

Freeboard is retrieved using geolocated aerial photography and a lead discrimination algorithm to maximize the quality and number of laser altimeter data points used to determine the sea surface height. This method is used to deal with loss of data due to specular reflection of the laser pulse away from the receiver when insufficient surface roughness elements are present to cause diffuse scattering. The combination of photography and laser altimetry allows for more accurate retrieval of sea ice freeboard. The primary ATM laser altimeter product is surface elevation referenced to the WGS-84 ellipsoid. The conversion of ATM elevation data into sea ice freeboard is accomplished by subtracting out the instantaneous sea surface height from each elevation measurement (Kurtz et al. 2013).

Sea Ice Snow Depth

Retrieval methods for the IceBridge snow radar have been described by Kurtz and Farrell (2011), Kurtz et al. (2013), and Farrell et al. (2012). The Kurtz and Farrell (2011) method is used to retrieve snow depth for the 2009 IceBridge campaign for this product and the Kurtz et al. (2013) method is used for all subsequent campaigns. The retrieval algorithms for the snow radar system detect the snow-air and snow-ice interfaces within the radar waveform and determine the snow depth by multiplying the time separation between the interfaces by the speed of light within the snow pack (Kurtz et al. 2013).

Sea Ice Thickness

Sea ice thickness, hi, is calculated using the corresponding 40 m scale freeboard and snow depth data as input for the hydrostatic balance equation:

Equation 1 (Equation 1)

Where:

Table 3. Hydrostatic Balance Equation
Variable Description
fbadj freeboard
hs snow depth
ρw density of sea water
ρi density of sea ice
ρs density of snow

ρw and ρi are taken to be 1024 kg m–3 and 915 kg m–3 which are derived from the result of numerous field measurements summarized by Wadhams et al. (1992).

ρs is taken to be 320 kg m–3 following the climatological values compiled by Warren et al. (1999).

Error Sources

Time tags in the 'elapsed' data field in some samples are identical yet have different latitude and longitude, and there are jumps in lat/lon at those points where the time stamps do not change. This timestamp issue appears to be present in each of the files for the 2011 Arctic campaign, apparently arising from the initial 2011 snow radar data set. This should only be an issue with the timestamp, not the location information, so the latitude and longitude fields should be correct. Reprocessed and corrected 2011 snow radar data have been received, and a fully corrected version will be released in the near future with Version 2 of the IDCSI2 data set. Version 2 will cover all data released to date and will include fixes for errors such as this as well as multiple upgrades.

During the processing of this data all averaging was based on the locations of the snow radar footprints. Each lat/lon ˜40 m spot was processed individually. During this process, if ATM data was available for this footprint, the timestamp was recorded from the ATM data within the footprint. If there were no ATM data available for the location, the timestamp from the snow radar was used. The code was initially designed for calculating ATM freeboard and the snow radar / thickness portion was added afterwards. This idiosyncrasy has since been removed and all timestamps are assigned at the beginning, similar to the lat/lon fields and are not dependent upon other data fields.

In the assignment of the timestamp from the snow radar data source, a coding error was made that failed to regularly update the timestamp being assigned to the correct one for the current location being processed. Due to this error, when the final script ran and rearranged every point to ensure that the elapsed time field was monotonically increasing, it also rearranged every other field, including the lat/lon fields. So even though the lat/lon fields appear to have "bad spots," they are actually just out of order in the file.

The lat/lon fields in the original ˜40 m footprint snow radar data set were ingested for the lat/lon positions. Other than being out of order, the values are identical. This means that the user has two options:

  1. To use the data spatially, use the lat/lon fields to plot everything; keeping in mind that the file may spatially jump around a bit, but all the data, other than the small repeating areas only in the ELAPSED field should be good.
  2. For the data to be monotonically increasing in time/along-track, filter the data by eliminating the entries that are missing ATM data, as the problem occurs only where the snow radar locations do not contain ATM data. For example, use a filter that treats all entries where the ELEV field is greater than -99999.0 as good. If fields filtered in this manner are plotted, the problem areas are erased.

Sensor or Instrument Description

ATM

The NASA ATM instrument is a scanning airborne laser that measures surface elevation of the ice by timing laser pulses transmitted from the aircraft, reflected from the ground and returning to the aircraft. This laser pulse time-of-flight information is used to derive surface elevation measurements by combining measurement of the scan pointing angle, precise GPS trajectories, and aircraft attitude information.

Snow Radar

The University of Kansas CReSIS ultra-wideband snow radar operates over the frequency range from 2 to 8 GHz to map near-surface internal layers in polar firn with fine vertical resolution. The radar also has been used to measure thickness of snow over sea ice. Information about snow thickness is essential to estimate sea ice thickness from ice freeboard measurements performed with satellite radar and laser altimeters.

DMS

The NASA Digital Mapping System is an airborne digital camera that acquires high resolution natural color and panchromatic imagery from low and medium altitude research aircraft.

CAMBOT

The CAMBOT system is comprised of a Canon Rebel XTi (or alternatively the XSi model) camera and a Mac Mini running custom data acquisition software. The camera is powered with an AC power adapter and connected to the Mac mini via USB. The camera is outfitted with a Canon Zoom Lens EF-S 18-55 mm lens.

5. References and Related Publications

Farrell, S. L., N. T. Kurtz, L. Connor, B. Elder, C. Leuschen, T. Markus, D. C. McAdoo, B. Panzer, J. Richter-Menge, and J. Sonntag. 2012. A First Assessment of IceBridge Snow and Ice Thickness Data over Arctic Sea Ice. IEEE Transactions on Geoscience and Remote Sensing, 50(6):2098-2111, doi:10.1109/TGRS.2011.2170843.

Kurtz, N. T. and S. L. Farrell. 2011. Large-scale Surveys of Snow Depth on Arctic Sea Ice from Operation IceBridge. Geophysical Research Letters, 38:L20505, doi:10.1029/2011GL049216.

Kurtz, N. T., Farrell, S. L., Studinger, M., Galin, N., Harbeck, J. P., Lindsay, R., Onana, V. D., Panzer, B., and Sonntag, J. G. 2013. Sea Ice Thickness, Freeboard, and Snow Depth Products from Operation IceBridge Airborne Data. The Cryosphere, 7:1035-1056, doi:10.5194/tc-7-1035-2013.

Wadhams, P., W. B. Tucker III, W. B. Krabill, R. N. Swift, J. C. Comiso, and N. R. Davis. 1992. Relationship Between Sea Ice Freeboard and Draft in the Arctic Basin, and Implications for Ice Thickness Monitoring. Journal of Geophysical Research, 97(C12):20325-20334.

Warren, S. G., I. G. Rigor, N. Untersteiner, V. F. Radionov, N. N. Bryazgin, Y. I. Aleksandrov, and R. Colony. 1999. Snow Depth on Arctic Sea Ice. Journal of Climate, 12:1814-1829.

Related Data Collections

Related Web Sites

  • Airborne Topographic Mapper Web site at NASA Wallops Flight Facility (http://atm.wff.nasa.gov/).
  • CReSIS Sensors Development Radar Web site (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).
  • NASA Digital Mapping System Web page (http://asapdata.arc.nasa.gov/dms/).

6. Document Information

Acronyms and Abbreviations

The acronyms used in this document are listed in Table 3.

Table 3. Acronyms and Abbreviations
Acronym Description
ASCII American Standard Code for Information Interchange
ATM Airborne Topographic Mapper
CAMBOT Continuous Airborne Mapping By Optical Translator
CIRES Cooperative Institute for Research in Environmental Science
DMS Digital Mapping System
FTP File Transfer Protocol
GPS Global Positioning System
ITRF International Terrestrial Reference Frame
NASA National Aeronautics and Space Administration
NSIDC National Snow and Ice Data Center
WGS-84 World Geodetic System 1984

Document Creation Date

14 January 2013

Document Revision Date

01 August 2013

28 October 2013

17 April 2014

17 June 2014

Document URL

http://nsidc.org/data/docs/daac/icebridge/idcsi2/index.html