{"title":"A Complete Map of Greenland Ice Velocity Derived from Satellite Data Collected over 20 Years.","authors":"Ian Joughin, Ben E Smith, Ian M Howat","doi":"10.1017/jog.2017.73","DOIUrl":null,"url":null,"abstract":"<p><p>While numerous maps of Greenland ice flow velocity exist, most have gaps in coverage and/or accuracy is limited. We processed a large volume of synthetic aperture radar (SAR) and Landsat 8 imagery collected between 1995 and 2015 to produce a nearly complete map of ice flow velocity for Greenland at a far greater accuracy than most prior products. We evaluated the accuracy of this map by comparing it with a variety of measured and estimated velocities. For the slow-moving interior of the ice sheet, where estimates are determined from interferometric phase, the errors are ~2 m a<sup>-1</sup> or better. For coastal areas, where estimates are determined entirely from speckle- or feature-tracking methods, errors are 2-3 m a<sup>-1</sup>, which is in good agreement with the estimated formal errors. Especially for the slow-moving majority of the ice sheet, this map provides an important source of data for numerous types of glaciological studies.</p>","PeriodicalId":92731,"journal":{"name":"The journal of glaciology","volume":"64 243","pages":"1-11"},"PeriodicalIF":2.6000,"publicationDate":"2018-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582972/pdf/nihms-1022227.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"The journal of glaciology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1017/jog.2017.73","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2017/11/21 0:00:00","PubModel":"Epub","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
While numerous maps of Greenland ice flow velocity exist, most have gaps in coverage and/or accuracy is limited. We processed a large volume of synthetic aperture radar (SAR) and Landsat 8 imagery collected between 1995 and 2015 to produce a nearly complete map of ice flow velocity for Greenland at a far greater accuracy than most prior products. We evaluated the accuracy of this map by comparing it with a variety of measured and estimated velocities. For the slow-moving interior of the ice sheet, where estimates are determined from interferometric phase, the errors are ~2 m a-1 or better. For coastal areas, where estimates are determined entirely from speckle- or feature-tracking methods, errors are 2-3 m a-1, which is in good agreement with the estimated formal errors. Especially for the slow-moving majority of the ice sheet, this map provides an important source of data for numerous types of glaciological studies.