Abstract
Abstract. Analyses of 32 yr (1979–2010) of Arctic sea ice extents and areas derived from satellite passive microwave radiometers are presented for the Northern Hemisphere as a whole and for nine Arctic regions. There is an overall negative yearly trend of −51.5 ± 4.1 × 103 km2 yr−1 (−4.1 ± 0.3% decade−1) in sea ice extent for the hemisphere. The yearly sea ice extent trends for the individual Arctic regions are all negative except for the Bering Sea: −3.9 ± 1.1 × 103 km2 yr−1 (−8.7 ± 2.5% decade−1) for the Seas of Okhotsk and Japan, +0.3 ± 0.8 × 103 km2 yr−1 (+1.2 ± 2.7% decade−1) for the Bering Sea, −4.4 ± 0.7 × 103 km2 yr−1 (−5.1 ± 0.9% decade−1) for Hudson Bay, −7.6 ± 1.6 × 103 km2 yr−1 (−8.5 ± 1.8% decade−1) for Baffin Bay/Labrador Sea, −0.5 ± 0.3 × 103 km2 yr−1 (−5.9 ± 3.5% decade−1) for the Gulf of St. Lawrence, −6.5 ± 1.1 × 103 km2 yr−1 (−8.6 ± 1.5% decade−1) for the Greenland Sea, −13.5 ± 2.3 × 103 km2 yr−1 (−9.2 ± 1.6% decade−1) for the Kara and Barents Seas, −14.6 ± 2.3 × 103 km2 yr−1 (−2.1 ± 0.3% decade−1) for the Arctic Ocean, and −0.9 ± 0.4 × 103 km2 yr−1 (−1.3 ± 0.5% decade−1) for the Canadian Archipelago. Similarly, the yearly trends for sea ice areas are all negative except for the Bering Sea. On a seasonal basis for both sea ice extents and areas, the largest negative trend is observed for summer with the next largest negative trend being for autumn. Both the sea ice extent and area trends vary widely by month depending on region and season. For the Northern Hemisphere as a whole, all 12 months show negative sea ice extent trends with a minimum magnitude in May and a maximum magnitude in September, whereas the corresponding sea ice area trends are smaller in magnitude and reach minimum and maximum values in March and September.
Highlights
Satellite passive microwave observations of the Earth’s polar sea ice cover over the last three decades have provided the basis for studying its regional, seasonal, and interannual variabilities
The data set from which the sea ice extents and areas are calculated consists of sea ice concentration maps derived from the radiances obtained from the following satellite microwave radiometers: the Nimbus 7 Scanning Multichannel Microwave Radiometer (SMMR), which operated from 26 October 1978 through 20 August 1987, the Defense Meteorological Satellite Program (DMSP) series of F8, F11, and F13 Special Sensor Microwave Imagers (SSMI), and the F17 Special Sensor Microwave Imager Sounder (SSMIS)
Sea ice extents and areas are presented for the Northern Hemisphere as monthly averaged values, monthly deviations, and yearly and seasonally averaged values for the years 1979–2010 (Fig. 2)
Summary
Satellite passive microwave observations of the Earth’s polar sea ice cover over the last three decades have provided the basis for studying its regional, seasonal, and interannual variabilities. Analyses of the Antarctic sea ice cover for this period are presented in a companion paper (Parkinson and Cavalieri, 2012). In this study we extend the 28-yr (1979–2006) time series presented by Parkinson and Cavalieri (2008) and discuss the differences in the Arctic sea ice variabilities and trends observed principally between the 28-yr and 32-yr periods. L. Parkinson: Arctic sea ice variability and trends, 1979–2010 of the use of different satellite sensors, each of which may differ in their measurement wavelengths, fields-of-view, angles of incidence, ascending node times, and calibrations. Details of the approach, including filling data gaps, reducing land-to-ocean spillover effects, reducing weather effects over ice-free ocean, and matching sea ice extents and areas for each pair of overlapping sensors, are discussed by Cavalieri et al (1999).
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