Daily variation at three Antarctic geomagnetic observatories within the polar cap
In this work we present a statistical analysis of the diurnal variation as observed at three Antarctic observatories located at different positions within the polar cap during the year 2006. Data used for the analysis are from the Italian geomagnetic observatory at Mario Zucchelli Station (formerly...
Published in: | Journal of Geophysical Research |
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Main Authors: | , , , , |
Other Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
EGU - Copernicus Publications
2008
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Subjects: | |
Online Access: | http://hdl.handle.net/2122/4135 |
id |
ftingv:oai:www.earth-prints.org:2122/4135 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Geomagnetism and paleomagnetism (Time variations diurnal to secular) Magnetospheric physics (Polar cap phenomena Solar wind-magnetosphere interactions) 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous |
spellingShingle |
Geomagnetism and paleomagnetism (Time variations diurnal to secular) Magnetospheric physics (Polar cap phenomena Solar wind-magnetosphere interactions) 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous Pietrolungo, M. Lepidi, S. Cafarella, L. Santarelli, L. Di Mauro, D. Daily variation at three Antarctic geomagnetic observatories within the polar cap |
topic_facet |
Geomagnetism and paleomagnetism (Time variations diurnal to secular) Magnetospheric physics (Polar cap phenomena Solar wind-magnetosphere interactions) 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous |
description |
In this work we present a statistical analysis of the diurnal variation as observed at three Antarctic observatories located at different positions within the polar cap during the year 2006. Data used for the analysis are from the Italian geomagnetic observatory at Mario Zucchelli Station (formerly Terra Nova Bay, geographic latitude 74.7° S, corrected geomagnetic latitude 80.0° S), from the French-Italian observatory at Concordia Station (75.1° S, 88.9° S) and from the French observatory at Dumont D’Urville (66.7° S, 80.4° S), which are located in pairs at the same geographic and corrected geomagnetic latitude; such a position allows to distinguish whether the geographic or the geomagnetic reference system is better suitable to describe the observed phenomena at so high latitudes. The peculiarities of the daily variation as observed during this year and its relation with the observatory location and magnetospheric and interplanetary conditions were analysed. Data were also studied taking into account different Lloyd seasons. The results indicate that the 24-h variation is quite persistent, but its amplitude strongly depends on season and global geomagnetic activity: indeed, it almost vanishes during local winter for quiet geomagnetic conditions; this reduction is more evident at the stations closer to the geographic pole, where the solar radiation reduction during winter is more dramatic. The Interplanetary Magnetic Field orientation has been found to be important in that the north-south and the east-west components control the amplitude and the diurnal pattern of the variation, respectively. Published 2179-2190 1.6. Osservazioni di geomagnetismo 3.4. Geomagnetismo 3.8. Geofisica per l'ambiente JCR Journal reserved |
author2 |
Pietrolungo, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Lepidi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Cafarella, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Santarelli, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Di Mauro, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia |
format |
Article in Journal/Newspaper |
author |
Pietrolungo, M. Lepidi, S. Cafarella, L. Santarelli, L. Di Mauro, D. |
author_facet |
Pietrolungo, M. Lepidi, S. Cafarella, L. Santarelli, L. Di Mauro, D. |
author_sort |
Pietrolungo, M. |
title |
Daily variation at three Antarctic geomagnetic observatories within the polar cap |
title_short |
Daily variation at three Antarctic geomagnetic observatories within the polar cap |
title_full |
Daily variation at three Antarctic geomagnetic observatories within the polar cap |
title_fullStr |
Daily variation at three Antarctic geomagnetic observatories within the polar cap |
title_full_unstemmed |
Daily variation at three Antarctic geomagnetic observatories within the polar cap |
title_sort |
daily variation at three antarctic geomagnetic observatories within the polar cap |
publisher |
EGU - Copernicus Publications |
publishDate |
2008 |
url |
http://hdl.handle.net/2122/4135 |
long_lat |
ENVELOPE(123.333,123.333,-75.100,-75.100) ENVELOPE(140.000,140.000,-66.667,-66.667) ENVELOPE(164.123,164.123,-74.695,-74.695) ENVELOPE(164.117,164.117,-74.700,-74.700) |
geographic |
Antarctic Concordia Station Dumont d’Urville Mario Zucchelli Mario Zucchelli Station Terra Nova Bay |
geographic_facet |
Antarctic Concordia Station Dumont d’Urville Mario Zucchelli Mario Zucchelli Station Terra Nova Bay |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
Annales Geophysicae 8 / 26 (2008) Akasofu, S. I., Ahn, B. H., and Romick, G. J.: A study of the polar current system using the IMS meridian chains of magnetometers, Space Sci. Rev., 36, 337–413, 1983. Brekke, A.: Physics of the upper polar atmosphere, John Wiley & Sons Ltd in association with Praxis Publishing Ltd, p. 491, 1997. Burch, J. L.: Rate of erosion of dayside magnetic flux based on a quantitative study of polar cusp latitude on the interplanetary magnetic field, Radio Sci., 8, 955–961, 1973. Cafarella, L., Di Mauro, D., Lepidi, S., Meloni, A., Pietrolungo, M., Santarelli, L., and Schott, J. J.: Daily variation at Concordia station (Antarctica) and its dependence on IMF conditions, Ann. Geophys., 25, 2045–2051, 2007, http://www.ann-geophys.net/25/2045/2007/. Campbell, W. H.: Introduction to geomagnetic fields, Cambridge University Press, 135–142, 1997. Kivelson, M. G. and Russell, C. T.: Introduction to Space Physics, Cambridge University Press, p. 568, 1996. Iijima, T.: Field-aligned currents in geospace: substance and significance, Magnetospheric Current Systems, edited by: Ohtani, S.-I., Fujii, R., Hesse, M., and Lysak, R. L., Gephysical Monograph, 118, 107–129, 2000. Lepidi, S., Cafarella, L., Francia, P., Meloni, A., Palangio, P., and Schott, J. J.: Low frequency geomagnetic field variations at Dome C (Antartica), Ann. Geophys., 21, 923–932, 2003, http://www.ann-geophys.net/21/923/2003/. Lloyd, H.: On earth-currents, and their connexion with the diurnal changes of the horizontal magnetic needle, Trans. Roy. Irish Acad., 24, 115–141, 1861. Matsushita, S. and Xu, W.: Equivalent ionospheric current system representing solar daily variations of the polar geomagnetic field, J. Geophys. Res., 87, 8241–8254, 1982. McEwen, D. J.: Polar cap phenomena and their relation to boundary layers and the IMF, in: Polar cap Boundary Phenomena, edited by: Moen, J., Egeland, A., and Lockwood, M., 271–280, 1998. Moretto, T., Olsen, N., Ritter, P., and Lu, G.: Investigating the auroral electrojets with low altitude polar orbiting satellites, Ann. Geophys., 20, 1049–1061, 2002, http://www.ann-geophys.net/20/1049/2002/. Nishida, A.: Geomagnetic diagnosis of the magnetosphere, Springer-Verlag, 54–64, 1978. Park, K. S., Ogino, T., and Walker, R. J.: On the importance of antiparallel reconnection when the dipole tilt and IMF By are nonzero, J. Geophys. Res., 111, A05202, doi:10.1029/2004JA010972, 2006. Ratcliffe, J. A.: An introduction to the ionosphere and magnetosphere, Com. Uni Press, Cambridge, p. 256, 1972. Ridley, A. J., Gang, Lu, Clauer, C. R., and Papitashvili, V. O.: A statistical study of the ionospheric convection response to changing interplanetary magnetic field conditions using the assimilative mapping of ionospheric electrodynamics technique, J. Geophys. Res., 103(A3), 4023–4039, 1998. Santarelli, L., Cafarella, L., Lepidi, S., Di Mauro, D., Meloni, A., and Palangio, P.: Fourteen years of geomagnetic daily variation at Mario Zucchelli Station (Antarctica), Annals of Geophysics, Italy, 50, 225–232, 2007. Stasiewicz, K.: Polar cusp topology and position as a function of interplanetary magnetic field and magnetic activity: Comparison of a model with Viking and other observations, J. Geophys. Res., 96, 15 789–15 800, 1991. Stubbs, T. J., Lockwood, M., Cargill, P., Fennell, J., Grande, M., Kellett, B., Perry, C., and Rees, A.: Dawn-dusk asymmetry in particles of solar wind origin within the magnetosphere, Ann. Geophys., 19, 1–9, 2001, http://www.ann-geophys.net/19/1/2001/. Vennerstrom, S., Moretto, T., Olsen, N., Friis-Christensen, E., and Stampe, A. M.: Field aligned currents in the dayside cusp and polar cap region during northward IMF, J. Geophys. Res., 107, A009162, doi:10.1029/2001JA009162, 2002. Vennerstrom, S., Moretto, T., Rastatter, L., and Raeder, J.: Field-aligned currents during northward interplanetary magnetic field: Morphology and causes, J. Geophys. Res., 110, A06205, doi:10.1029/2004JA010802, 2005. Yagova, N. V., Lanzerotti, L. J., Villante, U., Pilipenko, V. A., Lepidi, S., Francia, P., Papitashvili, V. O., and Rodger, A. S.: ULF Pc5-6 magnetic activity in the polar cap as observed along a geomagnetic meridian in Antarctica, J. Geophys. Res., 107, SMP22, doi:10.1029/2001JA900143, 2002. Yagova, N. V., Pilipenko, V. A., Lanzerotti, L. J., Engebretson, M. J., Rodger, A. S., Lepidi S., and Papitashvili, V. O.: Two-dimensional structure of long-period pulsations at polar latitudes in Antarctica, J. Geophys. Res., 109, A03222, doi:10.1029/2003JA010166, 2004. Zhou, X. W., Russell, C. T., Le, G., Fuselier, S. A., and Scudder, J. D.: The polar cusp location and its dependence on dipole tilt, Geophys. Res. Lett., 26, 429–432, 1999. Zhou, X. W., Russell, C. T., and Le, G.: Local time and interplanetary magnetic field By dependence of field-aligned currents at high altitudes, J. Geophys. Res., 105, 2533–2539, 2000a. Zhou, X. W., Russell, C. T., Le, G., Fuselier, S. A., and Scudder, J. D.: Solar wind control of the polar cusp at high altitude, J. Geophys. Res., 105, 245–251, doi:10.1029/1999JA900412, 2000b. http://hdl.handle.net/2122/4135 |
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Journal of Geophysical Research |
container_volume |
111 |
container_issue |
A5 |
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1766255669837561856 |
spelling |
ftingv:oai:www.earth-prints.org:2122/4135 2023-05-15T13:51:40+02:00 Daily variation at three Antarctic geomagnetic observatories within the polar cap Pietrolungo, M. Lepidi, S. Cafarella, L. Santarelli, L. Di Mauro, D. Pietrolungo, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Lepidi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Cafarella, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Santarelli, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Di Mauro, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia 2008-08-04 http://hdl.handle.net/2122/4135 en eng EGU - Copernicus Publications Annales Geophysicae 8 / 26 (2008) Akasofu, S. I., Ahn, B. H., and Romick, G. J.: A study of the polar current system using the IMS meridian chains of magnetometers, Space Sci. Rev., 36, 337–413, 1983. Brekke, A.: Physics of the upper polar atmosphere, John Wiley & Sons Ltd in association with Praxis Publishing Ltd, p. 491, 1997. Burch, J. L.: Rate of erosion of dayside magnetic flux based on a quantitative study of polar cusp latitude on the interplanetary magnetic field, Radio Sci., 8, 955–961, 1973. Cafarella, L., Di Mauro, D., Lepidi, S., Meloni, A., Pietrolungo, M., Santarelli, L., and Schott, J. J.: Daily variation at Concordia station (Antarctica) and its dependence on IMF conditions, Ann. Geophys., 25, 2045–2051, 2007, http://www.ann-geophys.net/25/2045/2007/. Campbell, W. H.: Introduction to geomagnetic fields, Cambridge University Press, 135–142, 1997. Kivelson, M. G. and Russell, C. T.: Introduction to Space Physics, Cambridge University Press, p. 568, 1996. Iijima, T.: Field-aligned currents in geospace: substance and significance, Magnetospheric Current Systems, edited by: Ohtani, S.-I., Fujii, R., Hesse, M., and Lysak, R. L., Gephysical Monograph, 118, 107–129, 2000. Lepidi, S., Cafarella, L., Francia, P., Meloni, A., Palangio, P., and Schott, J. J.: Low frequency geomagnetic field variations at Dome C (Antartica), Ann. Geophys., 21, 923–932, 2003, http://www.ann-geophys.net/21/923/2003/. Lloyd, H.: On earth-currents, and their connexion with the diurnal changes of the horizontal magnetic needle, Trans. Roy. Irish Acad., 24, 115–141, 1861. Matsushita, S. and Xu, W.: Equivalent ionospheric current system representing solar daily variations of the polar geomagnetic field, J. Geophys. Res., 87, 8241–8254, 1982. McEwen, D. J.: Polar cap phenomena and their relation to boundary layers and the IMF, in: Polar cap Boundary Phenomena, edited by: Moen, J., Egeland, A., and Lockwood, M., 271–280, 1998. Moretto, T., Olsen, N., Ritter, P., and Lu, G.: Investigating the auroral electrojets with low altitude polar orbiting satellites, Ann. Geophys., 20, 1049–1061, 2002, http://www.ann-geophys.net/20/1049/2002/. Nishida, A.: Geomagnetic diagnosis of the magnetosphere, Springer-Verlag, 54–64, 1978. Park, K. S., Ogino, T., and Walker, R. J.: On the importance of antiparallel reconnection when the dipole tilt and IMF By are nonzero, J. Geophys. Res., 111, A05202, doi:10.1029/2004JA010972, 2006. Ratcliffe, J. A.: An introduction to the ionosphere and magnetosphere, Com. Uni Press, Cambridge, p. 256, 1972. Ridley, A. J., Gang, Lu, Clauer, C. R., and Papitashvili, V. O.: A statistical study of the ionospheric convection response to changing interplanetary magnetic field conditions using the assimilative mapping of ionospheric electrodynamics technique, J. Geophys. Res., 103(A3), 4023–4039, 1998. Santarelli, L., Cafarella, L., Lepidi, S., Di Mauro, D., Meloni, A., and Palangio, P.: Fourteen years of geomagnetic daily variation at Mario Zucchelli Station (Antarctica), Annals of Geophysics, Italy, 50, 225–232, 2007. Stasiewicz, K.: Polar cusp topology and position as a function of interplanetary magnetic field and magnetic activity: Comparison of a model with Viking and other observations, J. Geophys. Res., 96, 15 789–15 800, 1991. Stubbs, T. J., Lockwood, M., Cargill, P., Fennell, J., Grande, M., Kellett, B., Perry, C., and Rees, A.: Dawn-dusk asymmetry in particles of solar wind origin within the magnetosphere, Ann. Geophys., 19, 1–9, 2001, http://www.ann-geophys.net/19/1/2001/. Vennerstrom, S., Moretto, T., Olsen, N., Friis-Christensen, E., and Stampe, A. M.: Field aligned currents in the dayside cusp and polar cap region during northward IMF, J. Geophys. Res., 107, A009162, doi:10.1029/2001JA009162, 2002. Vennerstrom, S., Moretto, T., Rastatter, L., and Raeder, J.: Field-aligned currents during northward interplanetary magnetic field: Morphology and causes, J. Geophys. Res., 110, A06205, doi:10.1029/2004JA010802, 2005. Yagova, N. V., Lanzerotti, L. J., Villante, U., Pilipenko, V. A., Lepidi, S., Francia, P., Papitashvili, V. O., and Rodger, A. S.: ULF Pc5-6 magnetic activity in the polar cap as observed along a geomagnetic meridian in Antarctica, J. Geophys. Res., 107, SMP22, doi:10.1029/2001JA900143, 2002. Yagova, N. V., Pilipenko, V. A., Lanzerotti, L. J., Engebretson, M. J., Rodger, A. S., Lepidi S., and Papitashvili, V. O.: Two-dimensional structure of long-period pulsations at polar latitudes in Antarctica, J. Geophys. Res., 109, A03222, doi:10.1029/2003JA010166, 2004. Zhou, X. W., Russell, C. T., Le, G., Fuselier, S. A., and Scudder, J. D.: The polar cusp location and its dependence on dipole tilt, Geophys. Res. Lett., 26, 429–432, 1999. Zhou, X. W., Russell, C. T., and Le, G.: Local time and interplanetary magnetic field By dependence of field-aligned currents at high altitudes, J. Geophys. Res., 105, 2533–2539, 2000a. Zhou, X. W., Russell, C. T., Le, G., Fuselier, S. A., and Scudder, J. D.: Solar wind control of the polar cusp at high altitude, J. Geophys. Res., 105, 245–251, doi:10.1029/1999JA900412, 2000b. http://hdl.handle.net/2122/4135 restricted Geomagnetism and paleomagnetism (Time variations diurnal to secular) Magnetospheric physics (Polar cap phenomena Solar wind-magnetosphere interactions) 01. Atmosphere::01.03. Magnetosphere::01.03.99. General or miscellaneous article 2008 ftingv 2022-07-29T06:04:59Z In this work we present a statistical analysis of the diurnal variation as observed at three Antarctic observatories located at different positions within the polar cap during the year 2006. Data used for the analysis are from the Italian geomagnetic observatory at Mario Zucchelli Station (formerly Terra Nova Bay, geographic latitude 74.7° S, corrected geomagnetic latitude 80.0° S), from the French-Italian observatory at Concordia Station (75.1° S, 88.9° S) and from the French observatory at Dumont D’Urville (66.7° S, 80.4° S), which are located in pairs at the same geographic and corrected geomagnetic latitude; such a position allows to distinguish whether the geographic or the geomagnetic reference system is better suitable to describe the observed phenomena at so high latitudes. The peculiarities of the daily variation as observed during this year and its relation with the observatory location and magnetospheric and interplanetary conditions were analysed. Data were also studied taking into account different Lloyd seasons. The results indicate that the 24-h variation is quite persistent, but its amplitude strongly depends on season and global geomagnetic activity: indeed, it almost vanishes during local winter for quiet geomagnetic conditions; this reduction is more evident at the stations closer to the geographic pole, where the solar radiation reduction during winter is more dramatic. The Interplanetary Magnetic Field orientation has been found to be important in that the north-south and the east-west components control the amplitude and the diurnal pattern of the variation, respectively. Published 2179-2190 1.6. Osservazioni di geomagnetismo 3.4. Geomagnetismo 3.8. Geofisica per l'ambiente JCR Journal reserved Article in Journal/Newspaper Antarc* Antarctic Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Antarctic Concordia Station ENVELOPE(123.333,123.333,-75.100,-75.100) Dumont d’Urville ENVELOPE(140.000,140.000,-66.667,-66.667) Mario Zucchelli ENVELOPE(164.123,164.123,-74.695,-74.695) Mario Zucchelli Station ENVELOPE(164.117,164.117,-74.700,-74.700) Terra Nova Bay Journal of Geophysical Research 111 A5 |