1999
DOI: 10.1029/1999jc900081
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Deriving long‐term time series of sea ice cover from satellite passive‐microwave multisensor data sets

Abstract: Abstract. We have generated consistent sea ice extent and area data records spanning 18.2 years from passive-microwave radiances obtained with the Nimbus 7 scanning multichannel microwave radiometer and with the Defense Meteorological Satellite Program F8, Fll, and F13 special sensor microwave/imagers. The goal in the creation of these data was to produce a long-term, consistent set of sea ice extents and areas that provides the means for reliably determining sea ice variability over the 18.2-year period and a… Show more

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Cited by 402 publications
(396 citation statements)
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“…This means that in the coastal zone, if there is open water or intermediate concentrations, the sea ice concentration will be overestimated. The statistical method which is described by Cavalieri et al (1999) is used for filtering the ice concentration near the coast.…”
Section: Statistical Filtering Of Ice Concentration Near the Coastlinementioning
confidence: 99%
“…This means that in the coastal zone, if there is open water or intermediate concentrations, the sea ice concentration will be overestimated. The statistical method which is described by Cavalieri et al (1999) is used for filtering the ice concentration near the coast.…”
Section: Statistical Filtering Of Ice Concentration Near the Coastlinementioning
confidence: 99%
“…We used two indices of of sea ice extent anomalies, based on the methods of Cavalieri et al (1999), as an index of physical conditions that are likely to affect ice-obligate Adélie penguins. The first provides a index of ice conditions in the WAP region, as described by Hewitt (1997), where sea ice extent and duration have decreased markedly in recent years (Stammerjohn et al 2008a).…”
Section: Environmental Correlates Of Survival and Recapture Probabilitymentioning
confidence: 99%
“…Corrections proposed by Cavalieri et al (1999) are applied to SMMR data to mediate the discontinuity in SIC observations between SMMR and SSM/I data, and to data from both satellites to remove measurement errors. Corrections are not applied for summer SIC measurement errors (such as noise) and 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 Time series of the annual number (unit 10 6 ) of all reports (thick solid), SLP (dash), total cloud cover (dotted), wind (long and short-dashes), SST (thin solid), AT (dash-dotted), and DPT (dash-two-dotted) available for the objective analyses negative biases attributable to surface conditions (such as meltwater ponding and the submersion of the ice interface).…”
Section: Sea Icementioning
confidence: 99%