Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances

Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern is...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Shiokawa, K. [verfasserIn] Otsuka, Y. [verfasserIn] Ejiri, M. K. [verfasserIn] Sahai, Y. [verfasserIn] Kadota, T. [verfasserIn] Ihara, C. [verfasserIn] Ogawa, T. [verfasserIn] Igarashi, K. [verfasserIn] Miyazaki, S. [verfasserIn] Saito, A. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2002

Schlagwörter:	Total Electron Content Ionospheric Disturbance Total Electron Content Variation Total Electron Content Data Virtual Height

Anmerkung:	© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002

Übergeordnetes Werk:	Enthalten in: Earth, planets and space - Springer Berlin Heidelberg, 1998, 54(2002), 1 vom: Jan., Seite 57-62
Übergeordnetes Werk:	volume:54 ; year:2002 ; number:1 ; month:01 ; pages:57-62

Links:	Volltext

DOI / URN:	10.1186/BF03352421

Katalog-ID:	SPR036899917

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allfields	10.1186/BF03352421 doi (DE-627)SPR036899917 (SPR)BF03352421-e DE-627 ger DE-627 rakwb eng 550 VZ 38.70 bkl 39.22 bkl Shiokawa, K. verfasserin aut Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002 Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213 Otsuka, Y. verfasserin aut Ejiri, M. K. verfasserin aut Sahai, Y. verfasserin aut Kadota, T. verfasserin aut Ihara, C. verfasserin aut Ogawa, T. verfasserin aut Igarashi, K. verfasserin aut Miyazaki, S. verfasserin aut Saito, A. verfasserin aut Enthalten in Earth, planets and space Springer Berlin Heidelberg, 1998 54(2002), 1 vom: Jan., Seite 57-62 (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:54 year:2002 number:1 month:01 pages:57-62 https://dx.doi.org/10.1186/BF03352421 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 38.70 VZ 39.22 VZ AR 54 2002 1 01 57-62
spelling	10.1186/BF03352421 doi (DE-627)SPR036899917 (SPR)BF03352421-e DE-627 ger DE-627 rakwb eng 550 VZ 38.70 bkl 39.22 bkl Shiokawa, K. verfasserin aut Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002 Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213 Otsuka, Y. verfasserin aut Ejiri, M. K. verfasserin aut Sahai, Y. verfasserin aut Kadota, T. verfasserin aut Ihara, C. verfasserin aut Ogawa, T. verfasserin aut Igarashi, K. verfasserin aut Miyazaki, S. verfasserin aut Saito, A. verfasserin aut Enthalten in Earth, planets and space Springer Berlin Heidelberg, 1998 54(2002), 1 vom: Jan., Seite 57-62 (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:54 year:2002 number:1 month:01 pages:57-62 https://dx.doi.org/10.1186/BF03352421 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 38.70 VZ 39.22 VZ AR 54 2002 1 01 57-62
allfields_unstemmed	10.1186/BF03352421 doi (DE-627)SPR036899917 (SPR)BF03352421-e DE-627 ger DE-627 rakwb eng 550 VZ 38.70 bkl 39.22 bkl Shiokawa, K. verfasserin aut Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002 Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213 Otsuka, Y. verfasserin aut Ejiri, M. K. verfasserin aut Sahai, Y. verfasserin aut Kadota, T. verfasserin aut Ihara, C. verfasserin aut Ogawa, T. verfasserin aut Igarashi, K. verfasserin aut Miyazaki, S. verfasserin aut Saito, A. verfasserin aut Enthalten in Earth, planets and space Springer Berlin Heidelberg, 1998 54(2002), 1 vom: Jan., Seite 57-62 (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:54 year:2002 number:1 month:01 pages:57-62 https://dx.doi.org/10.1186/BF03352421 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 38.70 VZ 39.22 VZ AR 54 2002 1 01 57-62
allfieldsGer	10.1186/BF03352421 doi (DE-627)SPR036899917 (SPR)BF03352421-e DE-627 ger DE-627 rakwb eng 550 VZ 38.70 bkl 39.22 bkl Shiokawa, K. verfasserin aut Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002 Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213 Otsuka, Y. verfasserin aut Ejiri, M. K. verfasserin aut Sahai, Y. verfasserin aut Kadota, T. verfasserin aut Ihara, C. verfasserin aut Ogawa, T. verfasserin aut Igarashi, K. verfasserin aut Miyazaki, S. verfasserin aut Saito, A. verfasserin aut Enthalten in Earth, planets and space Springer Berlin Heidelberg, 1998 54(2002), 1 vom: Jan., Seite 57-62 (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:54 year:2002 number:1 month:01 pages:57-62 https://dx.doi.org/10.1186/BF03352421 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 38.70 VZ 39.22 VZ AR 54 2002 1 01 57-62
allfieldsSound	10.1186/BF03352421 doi (DE-627)SPR036899917 (SPR)BF03352421-e DE-627 ger DE-627 rakwb eng 550 VZ 38.70 bkl 39.22 bkl Shiokawa, K. verfasserin aut Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances 2002 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002 Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213 Otsuka, Y. verfasserin aut Ejiri, M. K. verfasserin aut Sahai, Y. verfasserin aut Kadota, T. verfasserin aut Ihara, C. verfasserin aut Ogawa, T. verfasserin aut Igarashi, K. verfasserin aut Miyazaki, S. verfasserin aut Saito, A. verfasserin aut Enthalten in Earth, planets and space Springer Berlin Heidelberg, 1998 54(2002), 1 vom: Jan., Seite 57-62 (DE-627)353898597 (DE-600)2087663-4 1880-5981 nnns volume:54 year:2002 number:1 month:01 pages:57-62 https://dx.doi.org/10.1186/BF03352421 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 38.70 VZ 39.22 VZ AR 54 2002 1 01 57-62
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author	Shiokawa, K.
spellingShingle	Shiokawa, K. ddc 550 bkl 38.70 bkl 39.22 misc Total Electron Content misc Ionospheric Disturbance misc Total Electron Content Variation misc Total Electron Content Data misc Virtual Height Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
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topic_title	550 VZ 38.70 bkl 39.22 bkl Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances Total Electron Content (dpeaa)DE-He213 Ionospheric Disturbance (dpeaa)DE-He213 Total Electron Content Variation (dpeaa)DE-He213 Total Electron Content Data (dpeaa)DE-He213 Virtual Height (dpeaa)DE-He213
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title	Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
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title_full	Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
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title_sort	imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
title_auth	Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
abstract	Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002
abstractGer	Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002
abstract_unstemmed	Abstract This paper reports the first attempt to observe the equatorward limit of medium-scale traveling ionospheric disturbances (TIDs) in the middle latitudes. The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT. © The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences. 2002
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title_short	Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances
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The TIDs usually propagate southwestward in the northern hemisphere. An all-sky cooled-CCD imager measured 630-nm airglow at a southern island of Japan, Okinawa (26.9°N, 128.3°E, geomagnetic latitude (MLAT) = 17.0°), during the FRONT-2 campaign of August 4–15, 1999. The TIDs were detected at the mainland of Japan (∼21°–36° MLAT) by the total electron content (TEC) observations of more than 1000 GPS receivers. In the August 4 event, the TIDs moving southwestward was seen only in the northern sky of Okinawa as a depletion band in the 630-nm airglow images. In the August 6 event, the TIDs were not seen in the 630-nm images at Okinawa, although weak TID activity was observed by the GPS network at the mainland of Japan. The TEC data also showed weakening of the TID activity below 18° MLAT. Based on these observations, we suggest that there is a possible limit of medium-scale TID propagation around ∼18° MLAT.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Total Electron Content</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ionospheric Disturbance</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Total Electron Content Variation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Total Electron Content Data</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Virtual Height</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Otsuka, Y.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ejiri, M. 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Imaging observations of the equatorward limit of midlatitude traveling ionospheric disturbances

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