Data-derived spatial-resolution errors of Antarctic sea-ice thickness

Uncertainties due to spatial resolution (E R ) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely sensed and in situ observations of the Southern Ocean (south of −60°) to determine appropriate data sources based on length scales for conti...

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Published inPolar geography (1995) Vol. 36; no. 3; pp. 202 - 220
Main Authors Stampone, Mary D., Geiger, Cathleen A., DeLiberty, Tracy L., Bernstein, E. Rachel
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LanguageEnglish
Published Abingdon Taylor & Francis Group 01.09.2013
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Abstract Uncertainties due to spatial resolution (E R ) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely sensed and in situ observations of the Southern Ocean (south of −60°) to determine appropriate data sources based on length scales for continental-scale sea-ice studies. Sea-ice thickness is not normally distributed such that the mean, median, and mode are distinct from each other. Averaging only retains the mean value, reducing bias and natural variability as z is aggregated to coarse resolutions. The rate of smoothing as a function of resolution influences the sea-ice thickness distribution represented by each product. Analysis of E R for 1° through 5° resolutions shows absolute E R increasing with grid-cell size and sea-ice extent in both datasets. The absolute E R for gridded thickness distribution ranges from 0.02 to 0.40 m at 1° and from 0.03 to 0.78 m at 5°. The E R value and slope (m) is lower (E R ≤0.20 m, m<0.05) for ice charts than the ship dataset (0.10 m<E R <0.80 m, m<0.17) with relative E R between datasets remaining consistent. From these results, recommendations for dataset use and future sea-ice observation frequency and distribution schemes are discussed.
AbstractList Uncertainties due to spatial resolution (E R ) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely sensed and in situ observations of the Southern Ocean (south of −60°) to determine appropriate data sources based on length scales for continental-scale sea-ice studies. Sea-ice thickness is not normally distributed such that the mean, median, and mode are distinct from each other. Averaging only retains the mean value, reducing bias and natural variability as z is aggregated to coarse resolutions. The rate of smoothing as a function of resolution influences the sea-ice thickness distribution represented by each product. Analysis of E R for 1° through 5° resolutions shows absolute E R increasing with grid-cell size and sea-ice extent in both datasets. The absolute E R for gridded thickness distribution ranges from 0.02 to 0.40 m at 1° and from 0.03 to 0.78 m at 5°. The E R value and slope (m) is lower (E R ≤0.20 m, m<0.05) for ice charts than the ship dataset (0.10 m<E R <0.80 m, m<0.17) with relative E R between datasets remaining consistent. From these results, recommendations for dataset use and future sea-ice observation frequency and distribution schemes are discussed.
Uncertainties due to spatial resolution (E R) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely sensed and in situ observations of the Southern Ocean (south of -60°) to determine appropriate data sources based on length scales for continental-scale sea-ice studies. Sea-ice thickness is not normally distributed such that the mean, median, and mode are distinct from each other. Averaging only retains the mean value, reducing bias and natural variability as z is aggregated to coarse resolutions. The rate of smoothing as a function of resolution influences the sea-ice thickness distribution represented by each product. Analysis of E R for 1° through 5° resolutions shows absolute E R increasing with grid-cell size and sea-ice extent in both datasets. The absolute E R for gridded thickness distribution ranges from 0.02 to 0.40 m at 1° and from 0.03 to 0.78 m at 5°. The E R value and slope (m) is lower (E R[less-than or equal to]0.20 m, m<0.05) for ice charts than the ship dataset (0.10 m<E R<0.80 m, m<0.17) with relative E R between datasets remaining consistent. From these results, recommendations for dataset use and future sea-ice observation frequency and distribution schemes are discussed. [PUBLICATION ABSTRACT]
Uncertainties due to spatial resolution (E sub(R)) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely sensed and in situ observations of the Southern Ocean (south of -60 degree ) to determine appropriate data sources based on length scales for continental-scale sea-ice studies. Sea-ice thickness is not normally distributed such that the mean, median, and mode are distinct from each other. Averaging only retains the mean value, reducing bias and natural variability as z is aggregated to coarse resolutions. The rate of smoothing as a function of resolution influences the sea-ice thickness distribution represented by each product. Analysis of E sub(R) for 1 degree through 5 degree resolutions shows absolute E sub(R) increasing with grid-cell size and sea-ice extent in both datasets. The absolute E sub(R) for gridded thickness distribution ranges from 0.02 to 0.40 m at 1 degree and from 0.03 to 0.78 m at 5 degree . The E sub(R) value and slope (m) is lower (E sub(R) less than or equal to 0.20 m, m<0.05) for ice charts than the ship dataset (0.10 m<E sub(R)<0.80 m, m<0.17) with relative E sub(R) between datasets remaining consistent. From these results, recommendations for dataset use and future sea-ice observation frequency and distribution schemes are discussed.
Author Stampone, Mary D.
DeLiberty, Tracy L.
Geiger, Cathleen A.
Bernstein, E. Rachel
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Snippet Uncertainties due to spatial resolution (E R ) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely...
Uncertainties due to spatial resolution (E R) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using remotely...
Uncertainties due to spatial resolution (E sub(R)) of gridded sea-ice thickness (z) distributions remain largely unquantified. We address this issue using...
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Title Data-derived spatial-resolution errors of Antarctic sea-ice thickness
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