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Characterization of summer Arctic sea ice morphology in the 135°-175°W sector using multi-scale methods
Lei RB(雷瑞波); Tian-Kunze, Xiangshan; Li BR(李丙瑞); Heil, Petra; Wang, Jia; Zeng JB(曾俊宝); Tian ZX(田忠翔)
Department水下机器人研究室
Source PublicationCold Regions Science and Technology
ISSN0165-232X
2017
Volume133Pages:108-120
Indexed BySCI ; EI
EI Accession number20164703033360
WOS IDWOS:000388113000012
Contribution Rank6
Funding OrganizationNational Natural Science Foundation of China (No. 41476170) and Chinese Polar Environment Comprehensive Investigation and Assessment Programs (Nos. CHINARE2015-03-01/04-03/04-04). JW was supported by the NOAA CPO Office of Arctic Research through RUSALCA project, which was GLERL Contribution (No. 1837). PH was supported by the Antarctic Climate and Ecosystems CRC program. This work contributes to Australian Antarctic Science project (No. 4301).
KeywordSea Ice Concentration Thickness Melt Pond Morphology Arctic
AbstractIn summer 2014, sea ice morphological characteristics were investigated in the 135°-175°W sector of the Arctic Ocean using in situ, shipborne, and remote sensing measurements. Sea ice in this sector was deformed and compact compared to previous observations. The average ice area in the region (70°-82.5°N, 135°-175°W) was 7.6 × 105km2for 29 July through 6 September 2014, the fourth largest record between 2003 and 2014. This can be attributed to the enhanced multiyear sea ice inflow from north of the Canadian Arctic Archipelago from September 2013 to August 2014. Multiyear ice coverage in the study region on 30 April 2014 was 55%, which was larger than the values in 2005-2013. During the melt season of 2014, the Arctic Dipole had a positive anomaly, associated with enhanced southerly wind. In summer 2014 the marginal ice zone exhibited a distinct ice retreat, whereas the pack ice zone (PIZ) showed strong persistence due to the large coverage of multiyear ice. The northward retreat of the PIZ boundary was < 100 km from late July through early September 2014. In the PIZ of 76-80.5°N, average ice thickness weighted by ice concentration, obtained by shipborne measurements in August 2014 was 0.54 m thicker than that obtained in August 2010 due to enhanced ice deformation and less open waters in 2014. At 81°N, sea ice with modal thickness of 1.48 m reached thermodynamic balance by late August 2014, which was much earlier than that in 2010.
Language英语
WOS HeadingsScience & Technology ; Technology ; Physical Sciences
WOS SubjectEngineering, Environmental ; Engineering, Civil ; Geosciences, Multidisciplinary
WOS KeywordPHYSICAL-CHARACTERISTICS ; PACIFIC SECTOR ; OCEAN ; THICKNESS ; COVER
WOS Research AreaEngineering ; Geology
Citation statistics
Cited Times:3[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.sia.cn/handle/173321/19412
Collection水下机器人研究室
Corresponding AuthorLei RB(雷瑞波)
Affiliation1.Key Laboratory for Polar Science of the State Oceanic Administration, Polar Research Institute of China, Shanghai, 200136, China
2.Institute of Oceanography, University of Hamburg, Hamburg, 20146, Germany
3.Australian Antarctic Division, Kingston, Tasmania, 7050, Australia
4.Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania, 7001, Australia
5.NOAA Great Lakes Environmental Research Laboratory, Ann Arbor, MI, 48108, United States
6.Shenyang Institute of Automation, Chinese Academy of Sciences, Shenyang, Liaoning, 110016, China
7.National Marine Environmental Forecasting Center, Beijing, 100081, China
Recommended Citation
GB/T 7714
Lei RB,Tian-Kunze, Xiangshan,Li BR,et al. Characterization of summer Arctic sea ice morphology in the 135°-175°W sector using multi-scale methods[J]. Cold Regions Science and Technology,2017,133:108-120.
APA Lei RB.,Tian-Kunze, Xiangshan.,Li BR.,Heil, Petra.,Wang, Jia.,...&Tian ZX.(2017).Characterization of summer Arctic sea ice morphology in the 135°-175°W sector using multi-scale methods.Cold Regions Science and Technology,133,108-120.
MLA Lei RB,et al."Characterization of summer Arctic sea ice morphology in the 135°-175°W sector using multi-scale methods".Cold Regions Science and Technology 133(2017):108-120.
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