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Sea Ice Concentration data from AMSR-E, AMSR2 & SSMIS, U Bremen and U Hamburg ASI algorithm

The sea ice data derived from AMSR-E using the ARTIST sea ice (ASI) algorithm offer a factor of 4 finer spatial resolution than most sea ice data sets from passive microwave satellite instruments. ASI is based on the difference of vertically and horizontally polarized brightness temperatures at 89 GHz; this difference is independent of temperature but depends on emissivity; ice differences are small while water exhibits a large polarization difference. ASI obtains intermediate concentrations by interpolation between these end-member signatures (tie-points). A drawback of ASI is that higher frequencies are sensitive to weather. Nonetheless, the ASI includes adjustments intended to correct for weather using the lower-frequency channels. The AMSR-E satellite died in October, 2011. The AMSR-2 was launched in early 2012, and data are available as of 2013. U Bremen also offers daily sea ice estimates based on the 91 GHz channel of the SSMIS. There are no uncertainty estimates with the data sets, and it is not yet known how merging the AMSR-E, SSMIS and AMSR-2 data impacts apparent climate trends. Version 5.6i is the most recent processing.

Key Strengths:

  • At 6.25 km, finer spatial resolution than many passive microwave sea ice products
  • May be more useful for flux estimates that the lower-resolution data sets
  • High-frequency channels (89GHz)-mainly measuring surface emission-make the retrievals potentially less influenced by snow layering than algorithms using lower frequencies

Key Limitations:

  • Short record length for climate studies (AMSR-E satellite died in Oct 2011)
  • The high-frequency (89 GHz) channel is more sensitive to weather effects (atmospheric water vapor and cloud liquid water) than the low-frequency channels employed by other sea ice products.
  • The fixed tie points for ice and open water could lead to biases over seasonal and longer timescales due to changing atmospheric and surface conditions and/or degrading satellite instrumentation

Technical Notes

The data from the Integrated Climate Data Center at Hamburg are a more recent processing (L. Kaleschke, personal communication, 2012). Description.

Bremen HDF files: v5

ICDC netCDF files: v5.6i.

Figure 1 on this page is from the ICDC v5.6i

Years of Record

2002/06 to 2011/10
temporal metadataID:

Formats

Timestep

Daily

Data Time Period Extended?

no, data set not being extended

Domain

NH - Northern Hemisphere | SH - Southern Hemisphere | Antarctic | Arctic

Spatial Resolution

6.25 x 6.25 km

Ocean or Land

Ocean Only

Missing Data Flag

missing data present

Vertical Levels

Surface Data Set

Input Data

AMSR-E 89 GHz channel; separate data from SSMIS; planned AMSR-2

Earth system components and main variables

Cryosphere, Sea Ice Concentration, Ocean

Suggested Data Citation

Spreen, G., L. Kaleschke, and G.Heygster(2008), Sea ice remote sensing using AMSR-E 89 GHz channels J. Geophys. Res.,vol. 113, C02S03, doi:10.1029/2005JC003384.
the data from Hamburg: Spreen, G., and L. Kaleschke (2008), "AMSR-E ASI 6.25 km Sea Ice Concentration Data, V5.5", Institute of Oceanography, University of Hamburg, Germany, digital media (ftp-projects.zmaw.de/seaice/).

Data Access: Please Cite data sources, following the data providers' instructions.

  1. netCDF and OPeNDAP format, v5.6i: Hamburg Integrated Climate Data Center
  2. U Bremen: AMSR-E Daily maps and data archive (HDF v5, geoTIFF)
  3. U Bremen: SSMI/S Daily maps and data archive (HDF, geoTIFF)

Usage Restrictions

none

Key Figures

Click the thumbnails to view larger sizes

Thumbnails

Captions
Arctic sea ice: ASI v5.6i Average ice concentration in the Arctic in March for 2003-2007 based on the AMSR-E data and ASI algorithm. Figure by D. Schneider.

Cite this page

National Center for Atmospheric Research Staff (Eds). Last modified 20 Aug 2013. "The Climate Data Guide: Sea Ice Concentration data from AMSR-E, AMSR2 & SSMIS, U Bremen and U Hamburg ASI algorithm." Retrieved from https://climatedataguide.ucar.edu/climate-data/sea-ice-concentration-data-amsr-e-amsr2-ssmis-u-bremen-and-u-hamburg-asi-algorithm.

Acknowledgement of any material taken from this page is appreciated. On behalf of experts who have contributed data, advice, and/or figures, please cite their work as well.

Sea Ice Concentration data from AMSR-E, AMSR2 & SSMIS, U Bremen and U Hamburg ASI algorithm

The sea ice data derived from AMSR-E using the ARTIST sea ice (ASI) algorithm offer a factor of 4 finer spatial resolution than most sea ice data sets from passive microwave satellite instruments. ASI is based on the difference of vertically and horizontally polarized brightness temperatures at 89 GHz; this difference is independent of temperature but depends on emissivity; ice differences are small while water exhibits a large polarization difference. ASI obtains intermediate concentrations by interpolation between these end-member signatures (tie-points). A drawback of ASI is that higher frequencies are sensitive to weather. Nonetheless, the ASI includes adjustments intended to correct for weather using the lower-frequency channels. The AMSR-E satellite died in October, 2011. The AMSR-2 was launched in early 2012, and data are available as of 2013. U Bremen also offers daily sea ice estimates based on the 91 GHz channel of the SSMIS. There are no uncertainty estimates with the data sets, and it is not yet known how merging the AMSR-E, SSMIS and AMSR-2 data impacts apparent climate trends. Version 5.6i is the most recent processing.

2002-06/2011-10