On the low latitude topside models .2. Electron temperature

被引：11

作者：

Triskova, L ^{[1
]}

Smilauer, J ^{[1
]}

Truhlik, V ^{[1
]}

Afonin, VV ^{[1
]}

机构：

[1] RUSSIAN ACAD SCI, SPACE RES INST, MOSCOW 117810, RUSSIA

来源：

LOW AND EQUATORIAL LATITUDES IN THE INTERNATIONAL REFERENCE IONOSPHERE (IRI) | 1996年 / 18卷 / 06期

关键词：

D O I：

10.1016/0273-1177(95)00926-4

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Electron temperature measured within the scope of the ACTIVE Project was analyzed for range of +/-30 invariant latitude. Apogee (2500 km) and perigee (500 km) electron temperature data of December 1989 and March 1990 are in general agreement with the IRI. In morning hours there appears in high altitudes a longitude effect that is due to the variable illumination of the zone of main electron production. Geomagnetic activity causes an increase of electron temperature near 500 km, a decrease near 2500 km.

引用

页码：213 / 216

页数：4

共 4 条

[1]

Afonin V. V., 1994, KOSM ISSLED, V32, P82

[2] INTERNATIONAL REFERENCE IONOSPHERE - PAST, PRESENT, AND FUTURE .2. PLASMA TEMPERATURES, ION COMPOSITION AND ION DRIFT [J].

BILITZA, D ;

RAWER, K ;

BOSSY, L ;

GULYAEVA, T .

ADVANCES IN SPACE RESEARCH, 1993, 13 (03) :15-23

[3]

BILITZA D, 1990, NSSDC9022 NAT SPAC S

[4] On the low latitude topside models .1. Electron density [J].

Triskova, L ;

Smilauer, J ;

Truhlik, V ;

Afonin, VV .

LOW AND EQUATORIAL LATITUDES IN THE INTERNATIONAL REFERENCE IONOSPHERE (IRI), 1996, 18 (06) :209-212

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