An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere
An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N e), temperature (T e) and effective collision frequency ( ν e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N e distribution...
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Veröffentlicht in: | Advances in space research 1987, Vol.7 (6), p.49-52 |
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creator | Chasovitin, Yu.K. Shirochkov, A.V. Besprozvannaya, A.S. Gulyaeva, T.L. Denisenko, P.F. Armenskaya, O.A. Ivanova, S.E. Kashirin, A.I. Klyueva, N.M. Koryakina, E.A. Mironova, L.S. Sykilinda, T.N. Shushkova, V.B. Vodolazkin, V.I. Sotsky, V.V. Sheidakov, N.E. |
description | An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N
e), temperature (T
e) and effective collision frequency (
ν
e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N
e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N
e and T
e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N
e distributions; (iii) it describes rather correctly the shape of the N
e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T
e.
The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N
e, T
es and
ν
e calculations. |
doi_str_mv | 10.1016/0273-1177(87)90270-5 |
format | Article |
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e), temperature (T
e) and effective collision frequency (
ν
e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N
e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N
e and T
e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N
e distributions; (iii) it describes rather correctly the shape of the N
e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T
e.
The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N
e, T
es and
ν
e calculations.</description><identifier>ISSN: 0273-1177</identifier><identifier>EISSN: 1879-1948</identifier><identifier>DOI: 10.1016/0273-1177(87)90270-5</identifier><identifier>CODEN: ASRSDW</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Ionospheric structure (d, e, f and topside regions) ; Physics of the ionosphere</subject><ispartof>Advances in space research, 1987, Vol.7 (6), p.49-52</ispartof><rights>1987</rights><rights>1988 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c279t-6f879a8266136338c11d998b5a3e487f20f242cc9a832e27713e6da09fe3f2fc3</citedby><cites>FETCH-LOGICAL-c279t-6f879a8266136338c11d998b5a3e487f20f242cc9a832e27713e6da09fe3f2fc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/0273117787902705$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>309,310,314,776,780,785,786,3536,4009,4035,4036,23910,23911,25119,27902,27903,27904,65309</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=7625918$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Chasovitin, Yu.K.</creatorcontrib><creatorcontrib>Shirochkov, A.V.</creatorcontrib><creatorcontrib>Besprozvannaya, A.S.</creatorcontrib><creatorcontrib>Gulyaeva, T.L.</creatorcontrib><creatorcontrib>Denisenko, P.F.</creatorcontrib><creatorcontrib>Armenskaya, O.A.</creatorcontrib><creatorcontrib>Ivanova, S.E.</creatorcontrib><creatorcontrib>Kashirin, A.I.</creatorcontrib><creatorcontrib>Klyueva, N.M.</creatorcontrib><creatorcontrib>Koryakina, E.A.</creatorcontrib><creatorcontrib>Mironova, L.S.</creatorcontrib><creatorcontrib>Sykilinda, T.N.</creatorcontrib><creatorcontrib>Shushkova, V.B.</creatorcontrib><creatorcontrib>Vodolazkin, V.I.</creatorcontrib><creatorcontrib>Sotsky, V.V.</creatorcontrib><creatorcontrib>Sheidakov, N.E.</creatorcontrib><title>An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere</title><title>Advances in space research</title><description>An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N
e), temperature (T
e) and effective collision frequency (
ν
e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N
e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N
e and T
e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N
e distributions; (iii) it describes rather correctly the shape of the N
e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T
e.
The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N
e, T
es and
ν
e calculations.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Ionospheric structure (d, e, f and topside regions)</subject><subject>Physics of the ionosphere</subject><issn>0273-1177</issn><issn>1879-1948</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1987</creationdate><recordtype>article</recordtype><recordid>eNp9kMtKJDEUhsOgMK3OG8wii0EUrDGXqkpqI4h4GRDcOOuQTp2MGdKVNkkL_QY-tqdscekqJPn-c_kI-cnZb854f86Ekg3nSp1odTrgjTXdN7LgWg0NH1q9RxafyHdyUMp_xrhQii3I6-VEYbUOOTgb6SqNEKlPmdYnoP9iWuLjGErNYbmpIU2FJk9HmEqo2zNaMQnZ1k0GaqeRgvfgangB6lKMoWCA-gzPG5jcdk5CxP88lwnTewskUlk_QYYjsu9tLPDj4zwkf2-uH6_umvuH2z9Xl_eNE2qoTe9xKatF33PZS6kd5-Mw6GVnJbRaecG8aIVzyEgBuCOX0I-WDR6kF97JQ3K8q7vOCQcr1axCcRCjnSBtihFt18pO9Qi2O9DlVEoGb9Y5rGzeGs7MrN3MTs3s1Ghl3rWbDmO_Purbgkp9tpML5TOretENXCN2scMAd30JkE1xATXBGDI6MmMKX_d5A0kMmMU</recordid><startdate>1987</startdate><enddate>1987</enddate><creator>Chasovitin, Yu.K.</creator><creator>Shirochkov, A.V.</creator><creator>Besprozvannaya, A.S.</creator><creator>Gulyaeva, T.L.</creator><creator>Denisenko, P.F.</creator><creator>Armenskaya, O.A.</creator><creator>Ivanova, S.E.</creator><creator>Kashirin, A.I.</creator><creator>Klyueva, N.M.</creator><creator>Koryakina, E.A.</creator><creator>Mironova, L.S.</creator><creator>Sykilinda, T.N.</creator><creator>Shushkova, V.B.</creator><creator>Vodolazkin, V.I.</creator><creator>Sotsky, V.V.</creator><creator>Sheidakov, N.E.</creator><general>Elsevier Ltd</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>1987</creationdate><title>An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere</title><author>Chasovitin, Yu.K. ; Shirochkov, A.V. ; Besprozvannaya, A.S. ; Gulyaeva, T.L. ; Denisenko, P.F. ; Armenskaya, O.A. ; Ivanova, S.E. ; Kashirin, A.I. ; Klyueva, N.M. ; Koryakina, E.A. ; Mironova, L.S. ; Sykilinda, T.N. ; Shushkova, V.B. ; Vodolazkin, V.I. ; Sotsky, V.V. ; Sheidakov, N.E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c279t-6f879a8266136338c11d998b5a3e487f20f242cc9a832e27713e6da09fe3f2fc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1987</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Ionospheric structure (d, e, f and topside regions)</topic><topic>Physics of the ionosphere</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chasovitin, Yu.K.</creatorcontrib><creatorcontrib>Shirochkov, A.V.</creatorcontrib><creatorcontrib>Besprozvannaya, A.S.</creatorcontrib><creatorcontrib>Gulyaeva, T.L.</creatorcontrib><creatorcontrib>Denisenko, P.F.</creatorcontrib><creatorcontrib>Armenskaya, O.A.</creatorcontrib><creatorcontrib>Ivanova, S.E.</creatorcontrib><creatorcontrib>Kashirin, A.I.</creatorcontrib><creatorcontrib>Klyueva, N.M.</creatorcontrib><creatorcontrib>Koryakina, E.A.</creatorcontrib><creatorcontrib>Mironova, L.S.</creatorcontrib><creatorcontrib>Sykilinda, T.N.</creatorcontrib><creatorcontrib>Shushkova, V.B.</creatorcontrib><creatorcontrib>Vodolazkin, V.I.</creatorcontrib><creatorcontrib>Sotsky, V.V.</creatorcontrib><creatorcontrib>Sheidakov, N.E.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Advances in space research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chasovitin, Yu.K.</au><au>Shirochkov, A.V.</au><au>Besprozvannaya, A.S.</au><au>Gulyaeva, T.L.</au><au>Denisenko, P.F.</au><au>Armenskaya, O.A.</au><au>Ivanova, S.E.</au><au>Kashirin, A.I.</au><au>Klyueva, N.M.</au><au>Koryakina, E.A.</au><au>Mironova, L.S.</au><au>Sykilinda, T.N.</au><au>Shushkova, V.B.</au><au>Vodolazkin, V.I.</au><au>Sotsky, V.V.</au><au>Sheidakov, N.E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere</atitle><jtitle>Advances in space research</jtitle><date>1987</date><risdate>1987</risdate><volume>7</volume><issue>6</issue><spage>49</spage><epage>52</epage><pages>49-52</pages><issn>0273-1177</issn><eissn>1879-1948</eissn><coden>ASRSDW</coden><abstract>An improved ionospheric global empirical reference model (named RIM-85) is established for the distributions of density (N
e), temperature (T
e) and effective collision frequency (
ν
e) of electrons between 65 and 600 km. For altitudes above 200 km, at low and middle latitudes, the N
e distribution is based on IRI-82, with some necessary corrections. In comparison with IRI-82 and other models the model RIM-85 has a number of important advantages: (i) it describes in detail the height distributions of N
e and T
e below 200 km; (ii) it gives for the first time an adequate description of the high latitude ionosphere, its variations with geomagnetic activity reflecting the occurrence and dynamics of the main large-scale structures of the spatial N
e distributions; (iii) it describes rather correctly the shape of the N
e height profiles at low and high latitudes, in the outer ionosphere and also at high solar activity; (iv) it gives a spatial maximum height distribution of the F-region in the southern hemisphere which is close to the real one and (v) it describes rather correctly the diurnal and seasonal variations of T
e.
The model RIM-85 is established as a computer program, the general structure of which is similar to the corresponding programs for the IRI-79 and IRI-82 models; it includes some subroutines taken from this model software. Therefore the newly developed model can easily be included into a new version of IRI as a subprogram for N
e, T
es and
ν
e calculations.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/0273-1177(87)90270-5</doi><tpages>4</tpages></addata></record> |
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language | eng |
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source | Elsevier ScienceDirect Journals |
subjects | Earth, ocean, space Exact sciences and technology External geophysics Ionospheric structure (d, e, f and topside regions) Physics of the ionosphere |
title | An empirical model for the global distributions of density, temperature and effective collision frequency of electrons in the ionosphere |
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