K. Duncan, S. Farrell, J. Hutchings, J. Richter-Menge
{"title":"Late Winter Observations of Sea Ice Pressure Ridge Sail Height","authors":"K. Duncan, S. Farrell, J. Hutchings, J. Richter-Menge","doi":"10.1002/essoar.10500429.1","DOIUrl":null,"url":null,"abstract":"Analysis of high-resolution imagery acquired by the Digital Mapping System during annual, late-winter NASA Operation IceBridge surveys of Arctic sea ice between 2010 and 2018 reveals that pressure ridge sail heights (<inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula>) vary regionally and interannually. We find distinct differences in <inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula> distributions between the central Arctic (CA) and the Beaufort/Chukchi Seas region. Our results show that differences with respect to ice type occur within the tails of the <inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula> distributions and that the 95th and 99th percentiles of <inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula> are strong indicators of the predominant ice type in which the pressure ridge formed. During the first part of the study period <inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula> increased, with the largest sails observed in the winters of 2015 and 2016, after which <inline-formula> <tex-math notation=\"LaTeX\">${H} _{\\mathbf {S}}$ </tex-math></inline-formula> declined, suggesting that the most heavily deformed sea ice may have drifted beyond the area surveyed and exited the CA. Our analysis of the interannual and regional variability in sea ice deformation in the western Arctic during the last decade provides an improved understanding of sail height that will help advance ridge parameterizations in sea ice models.","PeriodicalId":13046,"journal":{"name":"IEEE Geoscience and Remote Sensing Letters","volume":"18 1","pages":"1525-1529"},"PeriodicalIF":4.0000,"publicationDate":"2019-01-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/essoar.10500429.1","citationCount":"7","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"IEEE Geoscience and Remote Sensing Letters","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1002/essoar.10500429.1","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENGINEERING, ELECTRICAL & ELECTRONIC","Score":null,"Total":0}
引用次数: 7
Abstract
Analysis of high-resolution imagery acquired by the Digital Mapping System during annual, late-winter NASA Operation IceBridge surveys of Arctic sea ice between 2010 and 2018 reveals that pressure ridge sail heights (${H} _{\mathbf {S}}$ ) vary regionally and interannually. We find distinct differences in ${H} _{\mathbf {S}}$ distributions between the central Arctic (CA) and the Beaufort/Chukchi Seas region. Our results show that differences with respect to ice type occur within the tails of the ${H} _{\mathbf {S}}$ distributions and that the 95th and 99th percentiles of ${H} _{\mathbf {S}}$ are strong indicators of the predominant ice type in which the pressure ridge formed. During the first part of the study period ${H} _{\mathbf {S}}$ increased, with the largest sails observed in the winters of 2015 and 2016, after which ${H} _{\mathbf {S}}$ declined, suggesting that the most heavily deformed sea ice may have drifted beyond the area surveyed and exited the CA. Our analysis of the interannual and regional variability in sea ice deformation in the western Arctic during the last decade provides an improved understanding of sail height that will help advance ridge parameterizations in sea ice models.
期刊介绍:
IEEE Geoscience and Remote Sensing Letters (GRSL) is a monthly publication for short papers (maximum length 5 pages) addressing new ideas and formative concepts in remote sensing as well as important new and timely results and concepts. Papers should relate to the theory, concepts and techniques of science and engineering as applied to sensing the earth, oceans, atmosphere, and space, and the processing, interpretation, and dissemination of this information. The technical content of papers must be both new and significant. Experimental data must be complete and include sufficient description of experimental apparatus, methods, and relevant experimental conditions. GRSL encourages the incorporation of "extended objects" or "multimedia" such as animations to enhance the shorter papers.