Recent results of the cedar storm study

被引:8
作者
Buonsanto, MJ [1 ]
Bust, G
Clark, R
Codrescu, M
Crowley, G
Emery, BA
Fuller-Rowell, TJ
Hoogeveen, G
Jacobson, A
Knipp, D
Maurits, S
Richards, PG
Taylor, JR
Watkins, BJ
机构
[1] MIT, Haystack Observ, Westford, MA 01886 USA
[2] Univ Texas, Appl Res Labs, Austin, TX 78713 USA
[3] Univ New Hampshire, Dept Elect & Comp Engn, Kingsbury ECE, Durham, NH 03824 USA
[4] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80303 USA
[5] NOAA, Space Environm Ctr, Boulder, CO 80303 USA
[6] SW Res Inst, San Antonio, TX 78228 USA
[7] Natl Ctr Atmospher Res, High Altitude Observ, Boulder, CO 80307 USA
[8] Univ Calif Los Alamos Natl Lab, Space & Atmospher Sci Grp, Los Alamos, NM 87545 USA
[9] USAF Acad, Dept Phys, Colorado Springs, CO 80840 USA
[10] Univ Alaska, Inst Geophys, Fairbanks, AK 99775 USA
[11] Univ Alabama, Dept Comp Sci, Huntsville, AL 35899 USA
[12] Univ Leicester, Dept Phys & Astron, Leicester LE1 7RH, Leics, England
来源
QUANTITATIVE DESCRIPTION OF IONOSPHERIC STORM EFFECTS AND IRREGULARITIES | 1997年 / 20卷 / 09期
关键词
D O I
10.1016/S0273-1177(97)00569-3
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
The CEDAR storm study is a cooperative effort to study specific storm-intervals with particularly good data coverage. The aim is to involve interested scientists with F-region/thermosphere data or modelling capabilities in coordinated efforts to understand the coupled upper atmosphere regions at different heights and on a global scale. The major storms studied to date occurred in March 1990, June 1991,November 1993, and May 1995. In this paper the objectives and organization of the CEDAR Storm Study are described, and results from several recent projects are reported. These include attempts at a global description of high latitude ion convection related to magnetosphere changes; Joule and particle heating, neutral winds, temperatures, and composition; plasmaspheric irregularity imaging; ionospheric model validation; the relationship between SAR arcs, subauroral ion drift (SAID) events, and the ionospheric trough; high latitude patches and blobs; ionospheric storm effects observed by radio and optical tomographic techniques; upper thermosphere neutral winds at high and middle latitudes; and effects of energy transfer into the lower thermosphere and mesosphere on neutral winds. (C) 1997 COSPAR. Published by Elsevier Science Ltd.
引用
收藏
页码:1655 / 1664
页数:10
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