Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval

The purpose of this thesis was to mount Airborne Electromagnetic (AEM) sensors for sea-ice thickness retrieval under the wings of long range airplanes and to quantify existing noise sources. Another aim was to determine and to characterise thickness distribution functions of several regions in the c...

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Bibliographic Details
Main Author: Rabenstein, Lasse
Other Authors: Miller, Heinrich, Lemke, Peter
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2010
Subjects:
620
Online Access:https://media.suub.uni-bremen.de/handle/elib/22
https://nbn-resolving.org/urn:nbn:de:gbv:46-00101669-14
id ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/22
record_format openpolar
spelling ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/22 2023-05-15T14:49:24+02:00 Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval Luftgestütze elektromagnetische Verfahren zur arktisweiten Bestimmung von Meereisdicken Rabenstein, Lasse Miller, Heinrich Lemke, Peter 2010-05-28 application/pdf https://media.suub.uni-bremen.de/handle/elib/22 https://nbn-resolving.org/urn:nbn:de:gbv:46-00101669-14 eng eng Universität Bremen FB5 Geowissenschaften https://media.suub.uni-bremen.de/handle/elib/22 urn:nbn:de:gbv:46-00101669-14 info:eu-repo/semantics/openAccess Bitte wählen Sie eine Lizenz aus: (Unsere Empfehlung: CC-BY) CC-BY Airborne Electromagnetics Sea Ice Thickness 620 620 Engineering ddc:620 Dissertation doctoralThesis 2010 ftsubbremen 2022-11-09T07:09:17Z The purpose of this thesis was to mount Airborne Electromagnetic (AEM) sensors for sea-ice thickness retrieval under the wings of long range airplanes and to quantify existing noise sources. Another aim was to determine and to characterise thickness distribution functions of several regions in the central Arctic. The accuracy of a prototype aeroplane EM system was found to be /- 0.5 m. The accuracy was reduced due to wing flexure, which produces noise of equal amplitude as the wanted ocean signal. Other noise sources are inductive ocean-aeroplane coupling and pitch which may disturb the measurements by another 10 percent of the signal. It is suggested to take the 90° out of phase response signal, since wing flexure noise mainly is 180° out of phase. On transects in the central Arctic mean thickness standard errors as low as 0.2 m could be obtained for 10 km long profiles in less deformed ice independently of the age of the ice regime. In a deformed multi year ice (MYI) regime standard errors of 0.2 m were obtained on transects as long as 100 km. These results show that a reduction of central Arctic mean sea-ice thickness by 1.8 between 1991 and 2007 was higher than typical spatial variability. Doctoral or Postdoctoral Thesis Arctic Arktis* Sea ice Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) Arctic
institution Open Polar
collection Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen)
op_collection_id ftsubbremen
language English
topic Airborne Electromagnetics
Sea Ice Thickness
620
620 Engineering
ddc:620
spellingShingle Airborne Electromagnetics
Sea Ice Thickness
620
620 Engineering
ddc:620
Rabenstein, Lasse
Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
topic_facet Airborne Electromagnetics
Sea Ice Thickness
620
620 Engineering
ddc:620
description The purpose of this thesis was to mount Airborne Electromagnetic (AEM) sensors for sea-ice thickness retrieval under the wings of long range airplanes and to quantify existing noise sources. Another aim was to determine and to characterise thickness distribution functions of several regions in the central Arctic. The accuracy of a prototype aeroplane EM system was found to be /- 0.5 m. The accuracy was reduced due to wing flexure, which produces noise of equal amplitude as the wanted ocean signal. Other noise sources are inductive ocean-aeroplane coupling and pitch which may disturb the measurements by another 10 percent of the signal. It is suggested to take the 90° out of phase response signal, since wing flexure noise mainly is 180° out of phase. On transects in the central Arctic mean thickness standard errors as low as 0.2 m could be obtained for 10 km long profiles in less deformed ice independently of the age of the ice regime. In a deformed multi year ice (MYI) regime standard errors of 0.2 m were obtained on transects as long as 100 km. These results show that a reduction of central Arctic mean sea-ice thickness by 1.8 between 1991 and 2007 was higher than typical spatial variability.
author2 Miller, Heinrich
Lemke, Peter
format Doctoral or Postdoctoral Thesis
author Rabenstein, Lasse
author_facet Rabenstein, Lasse
author_sort Rabenstein, Lasse
title Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
title_short Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
title_full Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
title_fullStr Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
title_full_unstemmed Airborne Electromagnetics as a Method for Arctic Wide Sea Ice Thickness Retrieval
title_sort airborne electromagnetics as a method for arctic wide sea ice thickness retrieval
publisher Universität Bremen
publishDate 2010
url https://media.suub.uni-bremen.de/handle/elib/22
https://nbn-resolving.org/urn:nbn:de:gbv:46-00101669-14
geographic Arctic
geographic_facet Arctic
genre Arctic
Arktis*
Sea ice
genre_facet Arctic
Arktis*
Sea ice
op_relation https://media.suub.uni-bremen.de/handle/elib/22
urn:nbn:de:gbv:46-00101669-14
op_rights info:eu-repo/semantics/openAccess
Bitte wählen Sie eine Lizenz aus: (Unsere Empfehlung: CC-BY)
op_rightsnorm CC-BY
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