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SCANDI – an all-sky Doppler imager for studies of thermospheric spatial structure

机译:SCANDI –用于研究热层空间结构的全天空多普勒成像仪

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摘要

A new all-sky Fabry-Perot Interferometer called the Scanning Doppler Imager(SCANDI) was built and installed at Longyearbyen in December 2006.Observations have been made of the Doppler shifts and Doppler broadening ofthe 630 nm airglow and aurora, from which upper thermospheric winds andtemperatures are calculated. SCANDI allows measurements over a field-of-view(FOV) with a horizontal radius of nearly 600 km for observations at analtitude of 250 km using a time resolution of 8 min. The instrumentprovides the ability to observe thermospheric spatial structure within a FOVwhich overlaps that of the EISCAT Svalbard radar and CUTLASS SuperDARNradars. Coordinating with these instruments provides an importantopportunity for studying ion-neutral coupling. The all-sky image is dividedinto several sectors to provide a horizontal spatial resolution ofbetween 100–300 km. This is a powerful extension in observational capabilitybut requires careful calibration and data analysis, as described here. Twoobservation modes were used: a fixed and a scanning etalon gap. SCANDIresults are corroborated using the Longyearbyen single look direction FPI,and ESR measurements of the ion temperatures. The data show thermospherictemperature gradients of a few Kelvins per kilometre, and a great deal ofmeso-scale variability on spatial scales of several tens of kilometres.
机译:2006年12月,在朗伊尔城(Longyearbyen)建造并安装了一种新型的全天法布里-珀罗干涉仪,称为扫描多普勒成像仪(SCANDI)。对630 nm的气辉和极光的多普勒频移和多普勒展宽进行了观测,由此产生了上层热圈计算温度。 SCANDI允许使用8分钟的时间分辨率在水平半径近600 km的视场(FOV)上进行测量,以在250 km的海拔高度进行观测。该仪器提供了在FOV内观测热球空间结构的能力,该结构与EISCAT斯瓦尔巴德雷达和CUTLASS SuperDARNradars的重叠。与这些仪器配合使用为研究离子中性耦合提供了重要的机会。全天候图像分为几个扇区,以提供100-300 km之间的水平空间分辨率。这是观察能力的强大扩展,但需要仔细校准和数据分析,如此处所述。使用了两种观察模式:固定的和扫描的标准具间隙。使用Longyearbyen单视方向FPI和离子温度的ESR测量,可以确认SCANDI结果。数据显示每公里几开尔文的热球温度梯度,以及几十公里的空间尺度上的中尺度变化。

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