Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks
The Earth is immersed in a planetary magnetic field. The field is generated in the Earth’s core and can be measured at its surface. It shows mainly a typical dipolar profile with the dipole axis roughly parallel to the Earth’s rotation axis (tilting about 12°). At low latitudes the field reaches its...
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2008
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ftingv:oai:www.earth-prints.org:2122/4402 2023-05-15T13:51:40+02:00 Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks An Overview in the IPY Perspective Cafarella, L. Di Mauro, D. Lepidi, S. Meloni, A. Cafarella, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Di Mauro, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Lepidi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Meloni, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Capra, A.; Dipartimento di Ingegneria Meccanica e Civile, Università degli Studi di Modena e Reggio Emilia, Italy Dietrich, R.; Institut für Planetare Geodasie, TU Dresden, 01062 Dresden, Germany Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Capra, A. Dietrich, R. Dipartimento di Ingegneria Meccanica e Civile, Università degli Studi di Modena e Reggio Emilia, Italy Institut für Planetare Geodasie, TU Dresden, 01062 Dresden, Germany 2008-11 http://hdl.handle.net/2122/4402 en eng Springer-Verlag Geodetic and Geophysical Observations in Antarctica 9783540748816 http://hdl.handle.net/2122/4402 restricted Geomagnetic observatories Antarctica Magnetosphere Secular variation 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous 04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversals 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques book chapter 2008 ftingv 2022-07-29T06:05:06Z The Earth is immersed in a planetary magnetic field. The field is generated in the Earth’s core and can be measured at its surface. It shows mainly a typical dipolar profile with the dipole axis roughly parallel to the Earth’s rotation axis (tilting about 12°). At low latitudes the field reaches its minimum, while its maximum intensity is observable in polar regions, reaching there almost three times its equatorial value. The region around the Earth where the geomagnetic field extends is known as the Earth’s magnetosphere. This region contains a very low density gas of electrically charged particles and is the space around the Earth where many electric and magnetic phenomena happen. Published 299-317 1.6. Osservazioni di geomagnetismo 3.4. Geomagnetismo 3.9. Fisica della magnetosfera, ionosfera e meteorologia spaziale reserved Book Part Antarc* Antarctica IPY Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Tilting ENVELOPE(-54.065,-54.065,49.700,49.700) |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Geomagnetic observatories Antarctica Magnetosphere Secular variation 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous 04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversals 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques |
spellingShingle |
Geomagnetic observatories Antarctica Magnetosphere Secular variation 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous 04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversals 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques Cafarella, L. Di Mauro, D. Lepidi, S. Meloni, A. Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
topic_facet |
Geomagnetic observatories Antarctica Magnetosphere Secular variation 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous 04. Solid Earth::04.05. Geomagnetism::04.05.02. Geomagnetic field variations and reversals 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques |
description |
The Earth is immersed in a planetary magnetic field. The field is generated in the Earth’s core and can be measured at its surface. It shows mainly a typical dipolar profile with the dipole axis roughly parallel to the Earth’s rotation axis (tilting about 12°). At low latitudes the field reaches its minimum, while its maximum intensity is observable in polar regions, reaching there almost three times its equatorial value. The region around the Earth where the geomagnetic field extends is known as the Earth’s magnetosphere. This region contains a very low density gas of electrically charged particles and is the space around the Earth where many electric and magnetic phenomena happen. Published 299-317 1.6. Osservazioni di geomagnetismo 3.4. Geomagnetismo 3.9. Fisica della magnetosfera, ionosfera e meteorologia spaziale reserved |
author2 |
Cafarella, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Di Mauro, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Lepidi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Meloni, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Capra, A.; Dipartimento di Ingegneria Meccanica e Civile, Università degli Studi di Modena e Reggio Emilia, Italy Dietrich, R.; Institut für Planetare Geodasie, TU Dresden, 01062 Dresden, Germany Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Capra, A. Dietrich, R. Dipartimento di Ingegneria Meccanica e Civile, Università degli Studi di Modena e Reggio Emilia, Italy Institut für Planetare Geodasie, TU Dresden, 01062 Dresden, Germany |
format |
Book Part |
author |
Cafarella, L. Di Mauro, D. Lepidi, S. Meloni, A. |
author_facet |
Cafarella, L. Di Mauro, D. Lepidi, S. Meloni, A. |
author_sort |
Cafarella, L. |
title |
Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
title_short |
Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
title_full |
Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
title_fullStr |
Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
title_full_unstemmed |
Geomagnetic Observatories in Antarctica; State of the Art and a Perspective View in the Global and Regional Frameworks |
title_sort |
geomagnetic observatories in antarctica; state of the art and a perspective view in the global and regional frameworks |
publisher |
Springer-Verlag |
publishDate |
2008 |
url |
http://hdl.handle.net/2122/4402 |
long_lat |
ENVELOPE(-54.065,-54.065,49.700,49.700) |
geographic |
Tilting |
geographic_facet |
Tilting |
genre |
Antarc* Antarctica IPY |
genre_facet |
Antarc* Antarctica IPY |
op_relation |
Geodetic and Geophysical Observations in Antarctica 9783540748816 http://hdl.handle.net/2122/4402 |
op_rights |
restricted |
_version_ |
1766255673072418816 |