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Volumn 278, Issue 5340, 1997, Pages 1104-1106

Observed hemispheric asymmetry in global sea ice changes

Author keywords

[No Author keywords available]

Indexed keywords

SEA WATER;

EID: 0030712376     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.278.5340.1104     Document Type: Article
Times cited : (308)

References (30)
  • 10
    • 1842403742 scopus 로고    scopus 로고
    • note
    • Correction for ice extent and area differences from the various sensors during the overlap periods was critical to obtaining unbiased long-term trends. In Bjørgo et al. (7), a correction for SMMR-SSMI differences was mentioned but none for SSMI F8-F11 differences. Bjørgo et al. used a two-step procedure to match ice concentrations for the SMMR-SSMI correction. Our matching of algorithm coefficients was somewhat comparable to their procedure, but then we additionally matched ice extents and areas during the overlap periods.
  • 11
    • 1842409747 scopus 로고    scopus 로고
    • note
    • Each data set was subjected to careful quality control, including the identification and subsequent correction or removal of bad data. Residual instrumental drift in the SMMR radiances used in the sea ice algorithm was reduced, by means of a procedure used previously (26), to values well below the instrument noise levels (8). The SSMI drifts similarly determined were found to be below or at the instrument noise values (9) for the SSMI radiances used in the sea ice algorithm (19 GHz horizontally and vertically polarized, 22 GHz vertically polarized, and 37 GHz vertically polarized) and so were ignored. Data gaps were filled by performing spatial and temporal interpolations. Additional corrections made to the SMMR and SSMI single-day sea ice concentration grids included the removal of false sea ice signals in the vicinity of the shoreline and over ice-free ocean areas. These were accomplished through the application of a coastline correction algorithm operating on the three image pixels nearest the coast, and also of monthly climatological sea surface temperature thresholds.
  • 12
    • 1842365643 scopus 로고    scopus 로고
    • note
    • The calculation of Arctic and Antarctic sea ice concentrations needed to compute sea ice extents and sea ice areas utilizes methods used previously for the SMMR (26) and SSMI (27) data sets. The details of generating a consistent set of sea ice extents and areas from the SMMR and SSMI sensors are discussed elsewhere (28). Since the publication of this report (28), DMSP F13 SSMI data through 31 December 1996 were added, but we followed the same procedure in preparing the data for analysis.
  • 14
    • 1842366266 scopus 로고    scopus 로고
    • note
    • Other differences giving rise to different ice concentrations include differences in sensor altitudes and view angles; differences in weather filter thresholds and algorithm tie points; and different overpass times, tidal phases, and diurnal effects.
  • 15
    • 1842372858 scopus 로고    scopus 로고
    • note
    • The upper limit of the ice extent and area errors for both the Arctic and Antarctic is obtained by calculating the standard deviations of the ice extent and area differences from the F11 and F13 SSMIs during their 5-month overlap period. The estimates are all about 0.3% of the annual mean value. It is noteworthy that the equatorial crossing times of the two spacecraft differ by 45 min, so that even this estimate includes real fluctuations of the ice covers. Of central importance in this study is not absolute accuracy but the consistency of measurements throughout the data record.
  • 23
    • 0002785989 scopus 로고
    • G. Weller, C. L. Wilson, B. A. B. Severin, Eds. Geophysical Institute and Center for Global Change and Arctic System Research, University of Alaska, Fairbanks, AK
    • T. H. Jacka and W. F. Budd, in International Conference on the Role of the Polar Regions in Global Change, G. Weller, C. L. Wilson, B. A. B. Severin, Eds. (Geophysical Institute and Center for Global Change and Arctic System Research, University of Alaska, Fairbanks, AK, 1991), pp. 63-70.
    • (1991) International Conference on the Role of the Polar Regions in Global Change , pp. 63-70
    • Jacka, T.H.1    Budd, W.F.2
  • 29
    • 1842289382 scopus 로고    scopus 로고
    • note
    • The confidence level was determined with a Student's t test in which the number of degrees of freedom is obtained by subtracting the number of calculated parameters from the number of windows used in the multiple window filtering.
  • 30
    • 1842406765 scopus 로고    scopus 로고
    • note
    • The SSMI data sets were provided by the National Snow and Ice Data Center in Boulder, CO. We thank S. Fiegles, M. Martino, and J. Saleh for their efforts in reprocessing and correcting the SMMR and SSMI data sets and J. A. Maslanik and J. Stroeve for their help in checking the final sea ice concentrations. This work was supported by NASA's polar program.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.