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首页> 外文期刊>Geophysical Research Letters >Caribbean Ionosphere Campaign, Year One: Airglow and plasma observations during two intense mid-latitude spread-F events
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Caribbean Ionosphere Campaign, Year One: Airglow and plasma observations during two intense mid-latitude spread-F events

机译:一年级加勒比海电离层运动:两次强烈的中纬度F扩散事件期间的气辉和等离子观测

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摘要

A series of campaigns has been carried out in the Caribbean over a one-year period to study intense midlatitude spread-F events using a cluster of diversified instrumentation. These events are relatively rare but a number of them have now been captured and will be discussed in this and several companion papers. This paper focuses on 630 nm airglow images obtained by the Cornell All-Sky Imager for two of the more spectacular cases that began on February 17, 1998 and February 17, 1999. In the latter case, and for the first time, a poleward surge of depletion/enhancement airglow zones was captured by radar as well as an airglow imager. In the former case structures grew in place overhead and produced strong VHF F-region backscatter as observed by the CUPRI and University of Illinois radars; the other event, exactly one year later, did not result in detectable 3-m backscatter. The two data sets show quantitatively that the low airglow region is elevated in height and depleted in plasma density and Pedersen conductivity. We suggest an enhanced eastward electric field inside the low conductivity zone may be responsible for the surge. The data also suggest small scale turbulence can only be observed in developing structures. [References: 8]
机译:在一年的时间里,加勒比海进行了一系列的运动,以使用一组多样化的仪器研究激烈的中纬度F扩散事件。这些事件相对很少见,但是现在已经捕获了其中的一些事件,并将在本白皮书和其他几篇论文中进行讨论。本文着重于康奈尔全天空成像仪针对1998年2月17日和1999年2月17日开始的两个更为壮观的情况获得的630 nm气辉图像。在后一种情况下,也是第一次出现极地波动雷达和气辉成像仪捕获了耗尽/增强的气辉区域。在前一种情况下,CUPRI和伊利诺伊大学的雷达观察到,结构在头顶增加了位置,并产生了强烈的VHF F区反向散射。另一件事,恰好在一年后,没有导致可检测到的3米反向散射。这两个数据定量地显示出低气辉区域的高度升高,血浆密度和Pedersen电导率降低。我们建议在低电导率区域内向东电场增强可能是电涌的原因。数据还表明,只能在发育的结构中观察到小规模的湍流。 [参考:8]

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