High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography

Elosegui, Pedro . et. al.-- AGU Fall Meeting 3–7 December 2012, San Francisco, California Project “Arctic Ocean sea ice and ocean circulation using satellite methods”ù (SATICE), is the first high-rate, high-precision, continuous GPS positioning experiment on sea ice in the Arctic Ocean. The SATICE s...

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Main Authors: Elosegui, Pedro, Olsson, M., Padman, Laurence
Format: Still Image
Language:unknown
Published: American Geophysical Union 2012
Subjects:
Online Access:http://hdl.handle.net/10261/93199
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spelling ftcsic:oai:digital.csic.es:10261/93199 2024-02-11T10:00:48+01:00 High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography Elosegui, Pedro Olsson, M. Padman, Laurence 2012-12-03 http://hdl.handle.net/10261/93199 unknown American Geophysical Union http://fallmeeting.agu.org/2012/eposters/eposter/c13e-0662/ AGU Fall Meeting: C13E-0662 (2012) http://hdl.handle.net/10261/93199 none póster de congreso http://purl.org/coar/resource_type/c_6670 2012 ftcsic 2024-01-16T09:57:05Z Elosegui, Pedro . et. al.-- AGU Fall Meeting 3–7 December 2012, San Francisco, California Project “Arctic Ocean sea ice and ocean circulation using satellite methods”ù (SATICE), is the first high-rate, high-precision, continuous GPS positioning experiment on sea ice in the Arctic Ocean. The SATICE systems collect continuous, dual-frequency carrier-phase GPS data while drifting on sea ice. Additional geophysical measurements also collected include ocean water pressure, ocean surface salinity, atmospheric pressure, snow-depth, air-ice-ocean temperature profiles, photographic imagery, and others, enabling sea ice drift, freeboard, weather, ice mass balance, and sea-level height determination. Relatively large volumes of data from each buoy are streamed over a satellite link to a central computer on the Internet in near real time, where they are processed to estimate the time-varying buoy positions. SATICE system obtains continuous GPS data at sub-minute intervals with a positioning precision of a few centimetres in all three dimensions. Although monitoring of sea ice motions goes back to the early days of satellite observations, these autonomous platforms bring out a level of spatio-temporal detail that has never been seen before, especially in the vertical axis. These high-resolution data allows us to address new polar science questions and challenge our present understanding of both sea ice dynamics and Arctic oceanography. We will describe the technology behind this new autonomous platform, which could also be adapted to other applications that require high resolution positioning information with sustained operations and observations in the polar marine environment, and present results pertaining to sea ice dynamics and physical oceanography Peer Reviewed Still Image Arctic Arctic Ocean Sea ice Digital.CSIC (Spanish National Research Council) Arctic Arctic Ocean
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description Elosegui, Pedro . et. al.-- AGU Fall Meeting 3–7 December 2012, San Francisco, California Project “Arctic Ocean sea ice and ocean circulation using satellite methods”ù (SATICE), is the first high-rate, high-precision, continuous GPS positioning experiment on sea ice in the Arctic Ocean. The SATICE systems collect continuous, dual-frequency carrier-phase GPS data while drifting on sea ice. Additional geophysical measurements also collected include ocean water pressure, ocean surface salinity, atmospheric pressure, snow-depth, air-ice-ocean temperature profiles, photographic imagery, and others, enabling sea ice drift, freeboard, weather, ice mass balance, and sea-level height determination. Relatively large volumes of data from each buoy are streamed over a satellite link to a central computer on the Internet in near real time, where they are processed to estimate the time-varying buoy positions. SATICE system obtains continuous GPS data at sub-minute intervals with a positioning precision of a few centimetres in all three dimensions. Although monitoring of sea ice motions goes back to the early days of satellite observations, these autonomous platforms bring out a level of spatio-temporal detail that has never been seen before, especially in the vertical axis. These high-resolution data allows us to address new polar science questions and challenge our present understanding of both sea ice dynamics and Arctic oceanography. We will describe the technology behind this new autonomous platform, which could also be adapted to other applications that require high resolution positioning information with sustained operations and observations in the polar marine environment, and present results pertaining to sea ice dynamics and physical oceanography Peer Reviewed
format Still Image
author Elosegui, Pedro
Olsson, M.
Padman, Laurence
spellingShingle Elosegui, Pedro
Olsson, M.
Padman, Laurence
High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
author_facet Elosegui, Pedro
Olsson, M.
Padman, Laurence
author_sort Elosegui, Pedro
title High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
title_short High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
title_full High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
title_fullStr High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
title_full_unstemmed High-precision GPS autonomous platforms for sea ice dynamics and physical oceanography
title_sort high-precision gps autonomous platforms for sea ice dynamics and physical oceanography
publisher American Geophysical Union
publishDate 2012
url http://hdl.handle.net/10261/93199
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_relation http://fallmeeting.agu.org/2012/eposters/eposter/c13e-0662/
AGU Fall Meeting: C13E-0662 (2012)
http://hdl.handle.net/10261/93199
op_rights none
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