Polar geomagnetism : developing models of high-latitude geomagnetic fields

The availability of high-quality data during the past decade has allowed the development of geomagnetic field models which reproduce well the observed field at low to mid latitudes. However, the complexity of un-modelled processes and interactions in the polar ionosphere and magnetosphere causes sig...

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Main Author: Kelly, Gemma
Other Authors: Holme, Richard; Thomson, Alan W. P.
Published: University of Liverpool 2013
Subjects:
538
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.579383
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spelling ndltd-bl.uk-oai-ethos.bl.uk-5793832017-05-24T03:24:42ZPolar geomagnetism : developing models of high-latitude geomagnetic fieldsKelly, GemmaHolme, Richard; Thomson, Alan W. P.2013The availability of high-quality data during the past decade has allowed the development of geomagnetic field models which reproduce well the observed field at low to mid latitudes. However, the complexity of un-modelled processes and interactions in the polar ionosphere and magnetosphere causes significant residuals between data and models at high latitudes. Signatures of high latitude currents are clearly visible in the residuals for several recent models in both amplitude and direction, and so are not easily interpretable as field-aligned currents. Motivated by this we identify new techniques to allow more, and better quality, data to be selected for use in field modelling at high latitudes. We also look to include more vector data to improve data uniformity and distribution whilst still avoiding the un-modelled sources of the field, in particular within the auroral oval. We investigate both the use of additional indices in the selection process and a method of locating the highly variable external currents to identify the region where vector data are not selected. By introducing additional criteria we extended the local-time window allowing data density to have greater uniformity in time. We also include vector data at higher latitudes, only using scalar data where we believe external field sources are introducing noise to the data. When using our data selection criteria in the generation of a relatively simply parameterised geomagnetic model we get results that are close to more complex models. For example, we are able to reproduce features of the field seen in CHAOS-4, MF7 and EMAG3, despite only using CHAMP data for a single year. This makes us optimistic for future developments using longer time series.538University of Liverpoolhttp://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.579383http://livrepository.liverpool.ac.uk/11053/Electronic Thesis or Dissertation
collection NDLTD
sources NDLTD
topic 538
spellingShingle 538
Kelly, Gemma
Polar geomagnetism : developing models of high-latitude geomagnetic fields
description The availability of high-quality data during the past decade has allowed the development of geomagnetic field models which reproduce well the observed field at low to mid latitudes. However, the complexity of un-modelled processes and interactions in the polar ionosphere and magnetosphere causes significant residuals between data and models at high latitudes. Signatures of high latitude currents are clearly visible in the residuals for several recent models in both amplitude and direction, and so are not easily interpretable as field-aligned currents. Motivated by this we identify new techniques to allow more, and better quality, data to be selected for use in field modelling at high latitudes. We also look to include more vector data to improve data uniformity and distribution whilst still avoiding the un-modelled sources of the field, in particular within the auroral oval. We investigate both the use of additional indices in the selection process and a method of locating the highly variable external currents to identify the region where vector data are not selected. By introducing additional criteria we extended the local-time window allowing data density to have greater uniformity in time. We also include vector data at higher latitudes, only using scalar data where we believe external field sources are introducing noise to the data. When using our data selection criteria in the generation of a relatively simply parameterised geomagnetic model we get results that are close to more complex models. For example, we are able to reproduce features of the field seen in CHAOS-4, MF7 and EMAG3, despite only using CHAMP data for a single year. This makes us optimistic for future developments using longer time series.
author2 Holme, Richard; Thomson, Alan W. P.
author_facet Holme, Richard; Thomson, Alan W. P.
Kelly, Gemma
author Kelly, Gemma
author_sort Kelly, Gemma
title Polar geomagnetism : developing models of high-latitude geomagnetic fields
title_short Polar geomagnetism : developing models of high-latitude geomagnetic fields
title_full Polar geomagnetism : developing models of high-latitude geomagnetic fields
title_fullStr Polar geomagnetism : developing models of high-latitude geomagnetic fields
title_full_unstemmed Polar geomagnetism : developing models of high-latitude geomagnetic fields
title_sort polar geomagnetism : developing models of high-latitude geomagnetic fields
publisher University of Liverpool
publishDate 2013
url http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.579383
work_keys_str_mv AT kellygemma polargeomagnetismdevelopingmodelsofhighlatitudegeomagneticfields
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