SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1

The Sea Ice Experiment - Dynamic Nature of the Arctic (SEDNA) is an international collaborative effort to improve the understanding of the interaction between sea ice dynamics and Arctic climate. It was also the first International Polar Year 2007-2008field project. The SEDNA data portal provides ac...

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Main Authors: IARC: International Arctic Research Center, UAF, National Snow and Ice Data Center
Format: Dataset
Language:unknown
Published: National Snow and Ice Data Center (NSIDC)
Subjects:
Online Access:https://search.dataone.org/view/sha256:c22cb00610f3c9a2ef8b5ba25eb1e81a43df73ff25a88091ebe1f088d9f3b375
id dataone:sha256:c22cb00610f3c9a2ef8b5ba25eb1e81a43df73ff25a88091ebe1f088d9f3b375
record_format openpolar
institution Open Polar
collection National Snow and Ice Data Center (NSIDC) (via DataONE)
op_collection_id dataone:urn:node:NSIDC
language unknown
description The Sea Ice Experiment - Dynamic Nature of the Arctic (SEDNA) is an international collaborative effort to improve the understanding of the interaction between sea ice dynamics and Arctic climate. It was also the first International Polar Year 2007-2008field project. The SEDNA data portal provides access to many and varied data sets from the diverse set of campaign participants.The data portal holds 37 entries from remote sensing to in situ measurements collected during the ice camp in March and April 2007. This data collection is distributed by the International Arctic Research Center (IARC) at the University of Alaska Fairbanks (UAF). NSIDC maintains the metadata for this data collection, so the data are easier to find through the NSIDC data catalog and those catalogs with which NSIDC shares metadata. This summary and metadata are accurate as of June 2011.The UAF archive site may have more recent data updates and publications, please visit their site for the most up-to-date information. The mass balance of sea ice and the evolution of sea ice thickness distribution is a key component of the Arctic system. It is controlled by thermodynamic ice growth and melt, mechanical redistribution through ridging and rafting, and transport. The SEDNA experiment was designed in a regional Lagrangian frame of reference and tracked the evolution of a region of ice surrounding the Applied Physics Laboratory Ice Station (APLIS) 2007 ice camp in an effort to evaluate the role of mechanical redistribution on ice thickness distribution. The SEDNA data collection is unique in that several ice thickness data sets were inter-calibrated and coordinated with monitoring of the ice pack strain-rate (horizontal deformation) and measurements of internal ice stress. This experiment was designed to improve our understanding of the relationship between sea ice thickness and dynamics and to investigate the stress and strain-rate relationships with a comprehensive suite of spatio-temporal coincident observations. Measurements were made with the aim of resolving the time evolving ice thickness distribution in the vicinity of the ice camp, to map ice pack deformation (strain-rate), and track strain-rate and internal ice stress in time. This has required a detailed inter-comparison of ice thickness measurements from a number of sources including submarine upward looking sonar (ULS) (Peter Wadhams), AUV multi-beam ULS (Peter Wadhams and Martin Doble), airborne LIDAR (Rene Forsberg), Helicopter borne electromagnetic induction (EMI) (Christian Haas), and in situ snow and ice measurements with drill and EM-31 soil surveyor (Cathy Geiger and Jackie Richter-Menge). Sea ice deformation was mapped in near-real time from analysis of RADARSat-1 ScanSAR-B by the Map of Moving Topography method (Mani Thomas, Chandra Kambhattmettu, and Cathy Geiger), and high temporal sampling was achieved with an array of GPS drifting buoys (Jenny Hutchings). Matt Pruis used GPS buoys to measure deformation of single leads. Ice stress and mass balance were measured with CRREL stress buoys (Jackie Richter-Menge). Additional measurements include a 3-m weather station (Andrew Roberts), CTD profiles every six hours (Jeremy Wilkinson), downward looking Acoustic Doppler Current Profiler (ADCP), and met-buoys (Ignatius Rigor). Data are generally available in three formats: the original format, netCDF, and ASCII. The original version is not always well documented. The netCDF version includes carefully collected documentation placed in the header fields of the netCDF file. Often, data are also available in a separate ASCII file as columns of data concatenated behind the netCDF header information in plain text form. SEDNA is supported by the NSF Grant \"Collaborative Research: Detailed Investigation of the Dynamic Component of Sea Ice Mass Balance\" (OPP ARC 0612527 (UAF), 0611991 (CRREL), and 0612105 (University of Delaware)).
format Dataset
author IARC: International Arctic Research Center, UAF
National Snow and Ice Data Center
spellingShingle IARC: International Arctic Research Center, UAF
National Snow and Ice Data Center
SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
author_facet IARC: International Arctic Research Center, UAF
National Snow and Ice Data Center
author_sort IARC: International Arctic Research Center, UAF
title SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
title_short SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
title_full SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
title_fullStr SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
title_full_unstemmed SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1
title_sort sedna: sea ice experiment - dynamic nature of the arctic, version 1
publisher National Snow and Ice Data Center (NSIDC)
publishDate
url https://search.dataone.org/view/sha256:c22cb00610f3c9a2ef8b5ba25eb1e81a43df73ff25a88091ebe1f088d9f3b375
op_coverage BEGINDATE: 2007-02-01T00:00:00Z ENDDATE: 2007-06-30T00:00:00Z
long_lat ENVELOPE(-62.550,-62.550,-64.667,-64.667)
ENVELOPE(-62.900,-62.900,-64.300,-64.300)
ENVELOPE(-68.417,-68.417,-67.733,-67.733)
ENVELOPE(-68.838,-68.838,-69.402,-69.402)
ENVELOPE(-178.833,-178.833,65.967,65.967)
ENVELOPE(-66.200,-66.200,-66.817,-66.817)
geographic Arctic
Doble
Fairbanks
Geiger
Jenny
Jeremy
Rene
Wilkinson
geographic_facet Arctic
Doble
Fairbanks
Geiger
Jenny
Jeremy
Rene
Wilkinson
genre Arctic
Collaborative Research: Detailed Investigation of the Dynamic Component of Sea Ice Mass Balance
ice pack
International Arctic Research Center
International Arctic Research Center (IARC)
International Polar Year
Sea ice
Alaska
genre_facet Arctic
Collaborative Research: Detailed Investigation of the Dynamic Component of Sea Ice Mass Balance
ice pack
International Arctic Research Center
International Arctic Research Center (IARC)
International Polar Year
Sea ice
Alaska
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spelling dataone:sha256:c22cb00610f3c9a2ef8b5ba25eb1e81a43df73ff25a88091ebe1f088d9f3b375 2024-11-03T19:44:59+00:00 SEDNA: Sea ice Experiment - Dynamic Nature of the Arctic, Version 1 IARC: International Arctic Research Center, UAF National Snow and Ice Data Center BEGINDATE: 2007-02-01T00:00:00Z ENDDATE: 2007-06-30T00:00:00Z 2023-11-29T00:07:07Z https://search.dataone.org/view/sha256:c22cb00610f3c9a2ef8b5ba25eb1e81a43df73ff25a88091ebe1f088d9f3b375 unknown National Snow and Ice Data Center (NSIDC) Dataset dataone:urn:node:NSIDC 2024-11-03T19:19:44Z The Sea Ice Experiment - Dynamic Nature of the Arctic (SEDNA) is an international collaborative effort to improve the understanding of the interaction between sea ice dynamics and Arctic climate. It was also the first International Polar Year 2007-2008field project. The SEDNA data portal provides access to many and varied data sets from the diverse set of campaign participants.The data portal holds 37 entries from remote sensing to in situ measurements collected during the ice camp in March and April 2007. This data collection is distributed by the International Arctic Research Center (IARC) at the University of Alaska Fairbanks (UAF). NSIDC maintains the metadata for this data collection, so the data are easier to find through the NSIDC data catalog and those catalogs with which NSIDC shares metadata. This summary and metadata are accurate as of June 2011.The UAF archive site may have more recent data updates and publications, please visit their site for the most up-to-date information. The mass balance of sea ice and the evolution of sea ice thickness distribution is a key component of the Arctic system. It is controlled by thermodynamic ice growth and melt, mechanical redistribution through ridging and rafting, and transport. The SEDNA experiment was designed in a regional Lagrangian frame of reference and tracked the evolution of a region of ice surrounding the Applied Physics Laboratory Ice Station (APLIS) 2007 ice camp in an effort to evaluate the role of mechanical redistribution on ice thickness distribution. The SEDNA data collection is unique in that several ice thickness data sets were inter-calibrated and coordinated with monitoring of the ice pack strain-rate (horizontal deformation) and measurements of internal ice stress. This experiment was designed to improve our understanding of the relationship between sea ice thickness and dynamics and to investigate the stress and strain-rate relationships with a comprehensive suite of spatio-temporal coincident observations. Measurements were made with the aim of resolving the time evolving ice thickness distribution in the vicinity of the ice camp, to map ice pack deformation (strain-rate), and track strain-rate and internal ice stress in time. This has required a detailed inter-comparison of ice thickness measurements from a number of sources including submarine upward looking sonar (ULS) (Peter Wadhams), AUV multi-beam ULS (Peter Wadhams and Martin Doble), airborne LIDAR (Rene Forsberg), Helicopter borne electromagnetic induction (EMI) (Christian Haas), and in situ snow and ice measurements with drill and EM-31 soil surveyor (Cathy Geiger and Jackie Richter-Menge). Sea ice deformation was mapped in near-real time from analysis of RADARSat-1 ScanSAR-B by the Map of Moving Topography method (Mani Thomas, Chandra Kambhattmettu, and Cathy Geiger), and high temporal sampling was achieved with an array of GPS drifting buoys (Jenny Hutchings). Matt Pruis used GPS buoys to measure deformation of single leads. Ice stress and mass balance were measured with CRREL stress buoys (Jackie Richter-Menge). Additional measurements include a 3-m weather station (Andrew Roberts), CTD profiles every six hours (Jeremy Wilkinson), downward looking Acoustic Doppler Current Profiler (ADCP), and met-buoys (Ignatius Rigor). Data are generally available in three formats: the original format, netCDF, and ASCII. The original version is not always well documented. The netCDF version includes carefully collected documentation placed in the header fields of the netCDF file. Often, data are also available in a separate ASCII file as columns of data concatenated behind the netCDF header information in plain text form. SEDNA is supported by the NSF Grant \"Collaborative Research: Detailed Investigation of the Dynamic Component of Sea Ice Mass Balance\" (OPP ARC 0612527 (UAF), 0611991 (CRREL), and 0612105 (University of Delaware)). Dataset Arctic Collaborative Research: Detailed Investigation of the Dynamic Component of Sea Ice Mass Balance ice pack International Arctic Research Center International Arctic Research Center (IARC) International Polar Year Sea ice Alaska National Snow and Ice Data Center (NSIDC) (via DataONE) Arctic Doble ENVELOPE(-62.550,-62.550,-64.667,-64.667) Fairbanks Geiger ENVELOPE(-62.900,-62.900,-64.300,-64.300) Jenny ENVELOPE(-68.417,-68.417,-67.733,-67.733) Jeremy ENVELOPE(-68.838,-68.838,-69.402,-69.402) Rene ENVELOPE(-178.833,-178.833,65.967,65.967) Wilkinson ENVELOPE(-66.200,-66.200,-66.817,-66.817)