Wintertime Antarctic coastal polynya area: 1992-2008

被引:60
作者
Kern, S. [1 ]
机构
[1] Univ Hamburg, Inst Oceanog, Ctr Marine & Atmospher Sci, D-20146 Hamburg, Germany
关键词
NOVA BAY POLYNYA; SEA-ICE; ROSS SEA; DYNAMICS;
D O I
10.1029/2009GL038062
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An iterative classification technique based on Special Sensor Microwave/Imager data is used to estimate the total daily circum-Antarctic coastal polynya area for 1992-2008. The average wintertime (June to September) area is estimated at 245,000 +/- 10,000 km(2), and varies between 210,000 km(2) (1997) and 281,000 km(2) (2007). The polynyas along East-Antarctica (60 to 160 degrees E) contribute about 40% to this area. The most persistent polynyas are located along East Antarctica: Lars-Christensen Coast (LCC), Prydz Bay, Western Davis Sea, Mertz Glacier, and in the Ross Sea: Ross Ice Shelf and Terra Nova Bay. The polynya at the LCC is observed on 110 +/- 5 days during winter for 1992-2008. It is the most persistent of the observed polynyas, covering an average area of 2400 km(2) on more than 90 days. Trends in the average wintertime area of the major coastal polynyas during 1992-2008 are small and not significant. Citation: Kern, S. (2009), Wintertime Antarctic coastal polynya area: 1992-2008, Geophys. Res. Lett., 36, L14501, doi:10.1029/2009GL038062.
引用
收藏
页数:5
相关论文
共 20 条
[1]   Phytoplankton dynamics within 37 Antarctic coastal polynya systems [J].
Arrigo, KR ;
van Dijken, GL .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2003, 108 (C8)
[2]   Antarctic sea ice variability and trends, 1979-2006 [J].
Cavalieri, D. J. ;
Parkinson, C. L. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2008, 113 (C7)
[3]   Passive microwave algorithms for sea ice concentration: A comparison of two techniques [J].
Comiso, JC ;
Cavalieri, DJ ;
Parkinson, CL ;
Gloersen, P .
REMOTE SENSING OF ENVIRONMENT, 1997, 60 (03) :357-384
[4]   Improved determination of the sea ice edge with SSM/I data for small-scale analyses [J].
Hunewinkel, T ;
Markus, T ;
Heygster, GC .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1998, 36 (05) :1795-1808
[5]   A comprehensive view of Kara Sea polynya dynamics, sea-ice compactness and export from model and remote sensing data [J].
Kern, S ;
Harms, I ;
Bakan, S ;
Chen, Y .
GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (15) :1-4
[6]   Polynya signature simulation method polynya area in comparison to AMSR-E 89 GHz sea-ice concentrations in the Ross Sea and off the Adeflie Coast, Antarctica, for 2002-05: first results [J].
Kern, Stefan ;
Spreen, Gunnar ;
Kaleschke, Lars ;
De la Rosa, Sara ;
Heygster, Georg .
ANNALS OF GLACIOLOGY, VOL 46, 2007, 2007, 46 :409-+
[7]   Ross Sea polynyas: Response of ice concentration retrievals to large areas of thin ice [J].
Kwok, R. ;
Comiso, J. C. ;
Martin, S. ;
Drucker, R. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2007, 112 (C12)
[8]   Polynya dynamics: A review of observations and modeling [J].
Maqueda, MAM ;
Willmott, AJ ;
Biggs, NRT .
REVIEWS OF GEOPHYSICS, 2004, 42 (01) :RG10041-37
[9]   A METHOD TO ESTIMATE SUBPIXEL-SCALE COASTAL POLYNYAS WITH SATELLITE PASSIVE MICROWAVE DATA [J].
MARKUS, T ;
BURNS, BA .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1995, 100 (C3) :4473-4487
[10]   Modeling water mass formation in the Mertz Glacier Polynya and Adelie Depression, East Antarctica [J].
Marsland, SJ ;
Bindoff, NL ;
Williams, GD ;
Budd, WF .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2004, 109 (C11) :C110031-18