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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Source region of 1500 MLT auroral bright spots: Simultaneous Polar UV-images and DMSP particle data
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Source region of 1500 MLT auroral bright spots: Simultaneous Polar UV-images and DMSP particle data

机译:1500 MLT极光亮点的源区域:同时极性的UV图像和DMSP粒子数据

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摘要

We compare auroral images from the Polar ultraviolet imager (UVI) and simultaneous particle observations from the Defense Meteorological Satellite Program (DMSP) in the afternoon (1300 - 1600 MLT) sector along the oval in the northern hemisphere to determine the magnetospheric source region of postnoon auroral bright spots. Auroral bright spots are determined with Polar UVI, while their magnetospheric source regions are determined from DMSP F13 particle data. A total of 65 events of good temporal and spatial coincidence were identified after searching through over 1 year of data, from April 1996 to June 1997. Instances occur of auroral arcs mapping to each of several different regions, including the plasma sheet, the low-latitude boundary layer, and the plasma mantle. However, our results indicate that approx 2/3 of the time the most prominent auroral arcs are associated with plasma sheet electron precipitation and slightly less than 1/3 of the time they are found to occur near (less than 1 deg in magnetic latitudes) the boundary between the plasma sheet and other regions.
机译:我们比较了极地紫外成像仪(UVI)的极光图像和国防气象卫星计划(DMSP)在北半球椭圆形区域下午(1300-1600 MLT)的同步粒子观测,以确定下午的磁层来源区域极光亮点。极光UVI由Polar UVI确定,而其磁层源区域由DMSP F13粒子数据确定。通过搜索从1996年4月至1997年6月的1年多的数据,总共鉴定出65个时间和空间上具有良好事件的事件。纬度边界层和等离子地幔。然而,我们的结果表明,最突出的极光弧约有2/3的时间与等离子片状电子沉淀有关,而略微少于发现它们的时间的1/3(磁纬度小于1度)等离子板和其他区域之间的边界。

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