Modeling of the lower ionosphere climate

Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemic...
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Gespeichert in:

Autor*in:	Kulyamin, D. V. [verfasserIn] Dymnikov, V. P.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2015

Schlagwörter:	mathematical modeling atmospheric general circulation middle atmosphere ionosphere region

Anmerkung:	© Pleiades Publishing, Ltd. 2015

Übergeordnetes Werk:	Enthalten in: Izvestiya - Moscow : MAIK Nauka/Interperiodica Publ., 2006, 51(2015), 3 vom: Mai, Seite 272-291
Übergeordnetes Werk:	volume:51 ; year:2015 ; number:3 ; month:05 ; pages:272-291

Links:	Volltext

DOI / URN:	10.1134/S0001433815030068

Katalog-ID:	SPR020053630

Internformat


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520			\|a Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer.
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650		4	\|a atmospheric general circulation \|7 (dpeaa)DE-He213
650		4	\|a middle atmosphere \|7 (dpeaa)DE-He213
650		4	\|a ionosphere \|7 (dpeaa)DE-He213
650		4	\|a region \|7 (dpeaa)DE-He213
700	1		\|a Dymnikov, V. P. \|4 aut
773	0	8	\|i Enthalten in \|t Izvestiya \|d Moscow : MAIK Nauka/Interperiodica Publ., 2006 \|g 51(2015), 3 vom: Mai, Seite 272-291 \|w (DE-627)34232098X \|w (DE-600)2071674-6 \|x 1555-628X \|7 nnns
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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_65
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_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_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
912			\|a GBV_ILN_281
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
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_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_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
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_2070
912			\|a GBV_ILN_2086
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_2188
912			\|a GBV_ILN_2190
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_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_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
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912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
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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
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Indexfelder

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publishDate	2015
allfields	10.1134/S0001433815030068 doi (DE-627)SPR020053630 (SPR)S0001433815030068-e DE-627 ger DE-627 rakwb eng Kulyamin, D. V. verfasserin aut Modeling of the lower ionosphere climate 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213 Dymnikov, V. P. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 3 vom: Mai, Seite 272-291 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:3 month:05 pages:272-291 https://dx.doi.org/10.1134/S0001433815030068 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 3 05 272-291
spelling	10.1134/S0001433815030068 doi (DE-627)SPR020053630 (SPR)S0001433815030068-e DE-627 ger DE-627 rakwb eng Kulyamin, D. V. verfasserin aut Modeling of the lower ionosphere climate 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213 Dymnikov, V. P. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 3 vom: Mai, Seite 272-291 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:3 month:05 pages:272-291 https://dx.doi.org/10.1134/S0001433815030068 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 3 05 272-291
allfields_unstemmed	10.1134/S0001433815030068 doi (DE-627)SPR020053630 (SPR)S0001433815030068-e DE-627 ger DE-627 rakwb eng Kulyamin, D. V. verfasserin aut Modeling of the lower ionosphere climate 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213 Dymnikov, V. P. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 3 vom: Mai, Seite 272-291 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:3 month:05 pages:272-291 https://dx.doi.org/10.1134/S0001433815030068 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 3 05 272-291
allfieldsGer	10.1134/S0001433815030068 doi (DE-627)SPR020053630 (SPR)S0001433815030068-e DE-627 ger DE-627 rakwb eng Kulyamin, D. V. verfasserin aut Modeling of the lower ionosphere climate 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213 Dymnikov, V. P. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 3 vom: Mai, Seite 272-291 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:3 month:05 pages:272-291 https://dx.doi.org/10.1134/S0001433815030068 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 3 05 272-291
allfieldsSound	10.1134/S0001433815030068 doi (DE-627)SPR020053630 (SPR)S0001433815030068-e DE-627 ger DE-627 rakwb eng Kulyamin, D. V. verfasserin aut Modeling of the lower ionosphere climate 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2015 Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213 Dymnikov, V. P. aut Enthalten in Izvestiya Moscow : MAIK Nauka/Interperiodica Publ., 2006 51(2015), 3 vom: Mai, Seite 272-291 (DE-627)34232098X (DE-600)2071674-6 1555-628X nnns volume:51 year:2015 number:3 month:05 pages:272-291 https://dx.doi.org/10.1134/S0001433815030068 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_65 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_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_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_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2188 GBV_ILN_2190 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_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 51 2015 3 05 272-291
language	English
source	Enthalten in Izvestiya 51(2015), 3 vom: Mai, Seite 272-291 volume:51 year:2015 number:3 month:05 pages:272-291
sourceStr	Enthalten in Izvestiya 51(2015), 3 vom: Mai, Seite 272-291 volume:51 year:2015 number:3 month:05 pages:272-291
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	mathematical modeling atmospheric general circulation middle atmosphere ionosphere region
isfreeaccess_bool	false
container_title	Izvestiya
authorswithroles_txt_mv	Kulyamin, D. V. @@aut@@ Dymnikov, V. P. @@aut@@
publishDateDaySort_date	2015-05-01T00:00:00Z
hierarchy_top_id	34232098X
id	SPR020053630
language_de	englisch
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author	Kulyamin, D. V.
spellingShingle	Kulyamin, D. V. misc mathematical modeling misc atmospheric general circulation misc middle atmosphere misc ionosphere misc region Modeling of the lower ionosphere climate
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topic_title	Modeling of the lower ionosphere climate mathematical modeling (dpeaa)DE-He213 atmospheric general circulation (dpeaa)DE-He213 middle atmosphere (dpeaa)DE-He213 ionosphere (dpeaa)DE-He213 region (dpeaa)DE-He213
topic	misc mathematical modeling misc atmospheric general circulation misc middle atmosphere misc ionosphere misc region
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title	Modeling of the lower ionosphere climate
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title_full	Modeling of the lower ionosphere climate
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author_browse	Kulyamin, D. V. Dymnikov, V. P.
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doi_str_mv	10.1134/S0001433815030068
title_sort	modeling of the lower ionosphere climate
title_auth	Modeling of the lower ionosphere climate
abstract	Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. © Pleiades Publishing, Ltd. 2015
abstractGer	Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. © Pleiades Publishing, Ltd. 2015
abstract_unstemmed	Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. Based on a preliminary model identification using direct measurements, and radiowave absorption and propagation, it has been indicated that the model satisfactorily reproduces climatic characteristics of the ionospheric D layer. © Pleiades Publishing, Ltd. 2015
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title_short	Modeling of the lower ionosphere climate
url	https://dx.doi.org/10.1134/S0001433815030068
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up_date	2024-07-03T13:39:12.197Z
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V.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Modeling of the lower ionosphere climate</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2015</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract A coupled model of the troposphere-stratosphere-mesosphere and the ionospheric D region (for 0–90 km altitudes) is presented. The model is based on a three-dimensional general atmospheric circulation model in a hybrid coordinate system. A five-component model has been taken as a photochemical model for the lower ionosphere. The role of the neutral atmosphere thermodynamic characteristics in the formation of the D layer mean state has been investigated by the model results. 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Modeling of the lower ionosphere climate

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