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Version Summary
Updated metadata field values for PGEVERSION (collection level remains
Version 4)Removed 15% sea ice concentration threshold that assigned pixels
with a sea ice concentration of <15% as ocean (data value of 255)Reprocessed NISE Version
4 to include sea ice concentration values of 1-14%
This revision is an update to NISE Version 4. All
Version 4 data (17 August 2009 - present) have been reprocessed
with this system.
Overview
- 1 day
- 25 km
- 25 km
Strengths
- Near-real-time combined sea ice and snow product (Armstrong and Brodzik, 2001; Maslanik and Stroeve, 1999)
- Useful for large-scale monitoring of sea ice and snow conditions (Armstrong and Brodzik, 2001; Maslanik and Stroeve, 1999)
- Uses data from up to 5 days previous to fill in all spatial gaps (particularly important for lower latitude snow cover) (Armstrong and Brodzik, 2001)
- Microwave observations provide surface snow and ice coverage during cloudy and night-time (including polar night) conditions (Cavalieri et al., 1999)
- Good source as input to products/models requiring a spatially complete snow and sea ice cover field at moderate/low resolution (Armstrong and Brodzik, 2001)
Limitations
- Low spatial resolution (25 km gridded) limits detail on concentration and precision of sea ice edge; is unsuitable for operational/navigational support (Cavalieri et al., 1999) and/or for detailed mapping of snow extent (Armstrong and Brodzik, 2002)
- Underestimates sea ice concentration during melt season (Kern et al., 2020) and/or when the ice is thin (Ivanova et al., 2015)
- Underestimates thin snow (Armstrong and Brodzik, 2002)
- Snow in dense forest and mountainous regions may be missed or underestimated (Armstrong and Brodzik, 2002)
- Wet snow is not accurately retrieved (Armstrong and Brodzik, 2002)
- There is a gap in coverage near the coast due to low spatial resolution and mixed land-ocean footprints (Armstrong and Brodzik, 2002)
- Near-real-time product with no planned reprocessing for long-term consistency; should not be used to derive long-term trends in sea ice or snow (Cavalieri et al., 1999)