TheTe-Tn difference in the lowerE region and radio-wave absorption

Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements).

Gespeichert in:

Autor*in:	Laštovička, Jan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	1981

Schlagwörter:	Atmosphere Atmosphere Temperature Structural Geology Electron Temperature lowerE Region

Anmerkung:	© ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981

Übergeordnetes Werk:	Enthalten in: Studia geophysica et geodaetica - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957, 25(1981), 3 vom: 01. Sept., Seite 294-296
Übergeordnetes Werk:	volume:25 ; year:1981 ; number:3 ; day:01 ; month:09 ; pages:294-296

Links:	Volltext

DOI / URN:	10.1007/BF01591942

Katalog-ID:	SPR051361841

Internformat


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035			\|a (DE-627)SPR051361841
035			\|a (SPR)BF01591942-e
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041			\|a eng
100	1		\|a Laštovička, Jan \|e verfasserin \|4 aut
245	1	0	\|a TheTe-Tn difference in the lowerE region and radio-wave absorption
264		1	\|c 1981
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337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
500			\|a © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981
520			\|a Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements).
650		4	\|a Atmosphere \|7 (dpeaa)DE-He213
650		4	\|a Atmosphere Temperature \|7 (dpeaa)DE-He213
650		4	\|a Structural Geology \|7 (dpeaa)DE-He213
650		4	\|a Electron Temperature \|7 (dpeaa)DE-He213
650		4	\|a lowerE Region \|7 (dpeaa)DE-He213
773	0	8	\|i Enthalten in \|t Studia geophysica et geodaetica \|d Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 \|g 25(1981), 3 vom: 01. Sept., Seite 294-296 \|w (DE-627)332167518 \|w (DE-600)2053073-0 \|x 1573-1626 \|7 nnns
773	1	8	\|g volume:25 \|g year:1981 \|g number:3 \|g day:01 \|g month:09 \|g pages:294-296
856	4	0	\|u https://dx.doi.org/10.1007/BF01591942 \|z lizenzpflichtig \|3 Volltext
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912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_121
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_206
912			\|a GBV_ILN_224
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_374
912			\|a GBV_ILN_602
912			\|a GBV_ILN_647
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2018
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2043
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2158
912			\|a GBV_ILN_2188
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2193
912			\|a GBV_ILN_2232
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2446
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2472
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_2808
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4277
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4328
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4346
912			\|a GBV_ILN_4367
912			\|a GBV_ILN_4393
912			\|a GBV_ILN_4700
912			\|a GBV_ILN_4753
951			\|a AR
952			\|d 25 \|j 1981 \|e 3 \|b 01 \|c 09 \|h 294-296

Indexfelder

author_variant	j l jl
matchkey_str	article:15731626:1981----::httdfeeciteoeeeinnrdo
hierarchy_sort_str	1981
publishDate	1981
allfields	10.1007/BF01591942 doi (DE-627)SPR051361841 (SPR)BF01591942-e DE-627 ger DE-627 rakwb eng Laštovička, Jan verfasserin aut TheTe-Tn difference in the lowerE region and radio-wave absorption 1981 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981 Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213 Enthalten in Studia geophysica et geodaetica Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 25(1981), 3 vom: 01. Sept., Seite 294-296 (DE-627)332167518 (DE-600)2053073-0 1573-1626 nnns volume:25 year:1981 number:3 day:01 month:09 pages:294-296 https://dx.doi.org/10.1007/BF01591942 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_224 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 25 1981 3 01 09 294-296
spelling	10.1007/BF01591942 doi (DE-627)SPR051361841 (SPR)BF01591942-e DE-627 ger DE-627 rakwb eng Laštovička, Jan verfasserin aut TheTe-Tn difference in the lowerE region and radio-wave absorption 1981 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981 Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213 Enthalten in Studia geophysica et geodaetica Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 25(1981), 3 vom: 01. Sept., Seite 294-296 (DE-627)332167518 (DE-600)2053073-0 1573-1626 nnns volume:25 year:1981 number:3 day:01 month:09 pages:294-296 https://dx.doi.org/10.1007/BF01591942 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_224 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 25 1981 3 01 09 294-296
allfields_unstemmed	10.1007/BF01591942 doi (DE-627)SPR051361841 (SPR)BF01591942-e DE-627 ger DE-627 rakwb eng Laštovička, Jan verfasserin aut TheTe-Tn difference in the lowerE region and radio-wave absorption 1981 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981 Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213 Enthalten in Studia geophysica et geodaetica Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 25(1981), 3 vom: 01. Sept., Seite 294-296 (DE-627)332167518 (DE-600)2053073-0 1573-1626 nnns volume:25 year:1981 number:3 day:01 month:09 pages:294-296 https://dx.doi.org/10.1007/BF01591942 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_224 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 25 1981 3 01 09 294-296
allfieldsGer	10.1007/BF01591942 doi (DE-627)SPR051361841 (SPR)BF01591942-e DE-627 ger DE-627 rakwb eng Laštovička, Jan verfasserin aut TheTe-Tn difference in the lowerE region and radio-wave absorption 1981 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981 Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213 Enthalten in Studia geophysica et geodaetica Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 25(1981), 3 vom: 01. Sept., Seite 294-296 (DE-627)332167518 (DE-600)2053073-0 1573-1626 nnns volume:25 year:1981 number:3 day:01 month:09 pages:294-296 https://dx.doi.org/10.1007/BF01591942 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_224 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 25 1981 3 01 09 294-296
allfieldsSound	10.1007/BF01591942 doi (DE-627)SPR051361841 (SPR)BF01591942-e DE-627 ger DE-627 rakwb eng Laštovička, Jan verfasserin aut TheTe-Tn difference in the lowerE region and radio-wave absorption 1981 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981 Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213 Enthalten in Studia geophysica et geodaetica Dordrecht [u.a.] : Springer Science + Business Media B.V, 1957 25(1981), 3 vom: 01. Sept., Seite 294-296 (DE-627)332167518 (DE-600)2053073-0 1573-1626 nnns volume:25 year:1981 number:3 day:01 month:09 pages:294-296 https://dx.doi.org/10.1007/BF01591942 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_121 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_224 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2043 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2158 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2193 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2808 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 25 1981 3 01 09 294-296
language	English
source	Enthalten in Studia geophysica et geodaetica 25(1981), 3 vom: 01. Sept., Seite 294-296 volume:25 year:1981 number:3 day:01 month:09 pages:294-296
sourceStr	Enthalten in Studia geophysica et geodaetica 25(1981), 3 vom: 01. Sept., Seite 294-296 volume:25 year:1981 number:3 day:01 month:09 pages:294-296
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Atmosphere Atmosphere Temperature Structural Geology Electron Temperature lowerE Region
isfreeaccess_bool	false
container_title	Studia geophysica et geodaetica
authorswithroles_txt_mv	Laštovička, Jan @@aut@@
publishDateDaySort_date	1981-09-01T00:00:00Z
hierarchy_top_id	332167518
id	SPR051361841
language_de	englisch
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author	Laštovička, Jan
spellingShingle	Laštovička, Jan misc Atmosphere misc Atmosphere Temperature misc Structural Geology misc Electron Temperature misc lowerE Region TheTe-Tn difference in the lowerE region and radio-wave absorption
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topic_title	TheTe-Tn difference in the lowerE region and radio-wave absorption Atmosphere (dpeaa)DE-He213 Atmosphere Temperature (dpeaa)DE-He213 Structural Geology (dpeaa)DE-He213 Electron Temperature (dpeaa)DE-He213 lowerE Region (dpeaa)DE-He213
topic	misc Atmosphere misc Atmosphere Temperature misc Structural Geology misc Electron Temperature misc lowerE Region
topic_unstemmed	misc Atmosphere misc Atmosphere Temperature misc Structural Geology misc Electron Temperature misc lowerE Region
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format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
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title	TheTe-Tn difference in the lowerE region and radio-wave absorption
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title_full	TheTe-Tn difference in the lowerE region and radio-wave absorption
author_sort	Laštovička, Jan
journal	Studia geophysica et geodaetica
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author_browse	Laštovička, Jan
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doi_str_mv	10.1007/BF01591942
title_sort	thete-tn difference in the lowere region and radio-wave absorption
title_auth	TheTe-Tn difference in the lowerE region and radio-wave absorption
abstract	Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981
abstractGer	Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981
abstract_unstemmed	Summary The difference observed between the electron temperature, $ T_{e} $, and the neutral atmosphere temperature, $ T_{n} $, is shown to be able to contribute significantly to the observed variability of ionospheric radio-wave absorption (A1 andHF-A3 measurements). © ACADEMIA Publishing House of the Czechoslovak Academy of Sciences 1981
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title_short	TheTe-Tn difference in the lowerE region and radio-wave absorption
url	https://dx.doi.org/10.1007/BF01591942
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up_date	2024-07-03T21:21:29.728Z
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TheTe-Tn difference in the lowerE region and radio-wave absorption

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