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首页> 外文期刊>Geophysical Research Letters >First daytime thermospheric wind observation from a balloon-borne Fabry-Perot interferometer over Kiruna (68N)
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First daytime thermospheric wind observation from a balloon-borne Fabry-Perot interferometer over Kiruna (68N)

机译:白天在基律纳(68N)上的气球式法布里-珀罗干涉仪进行的第一天热层风观测

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摘要

HIWIND (High altitude Interferometer WIND Observation) is the first balloon Fabry-Perot interferometer (FPI) to achieve successful thermospheric wind measurement for both day and night. By flying at ?40 km altitude, HIWIND avoids the high solar scattering background and enables daytime remote sensing of Doppler shift in airglow for thermospheric wind observation. During its first flight in June 2011 from Kiruna, (68N, 65 MLAT), HIWIND observed persistent equatorward winds, while the NCAR TIEGCM model predicted poleward winds on the dayside. Combined with simultaneous EISCAT incoherent scatter radar observation, HIWIND yielded a daytime Burnside factor value of 0.85. HIWIND data appear to suggest that upward vertical winds near the auroral oval may be the cause for large differences between the FPI measured and radar derived winds near midnight.
机译:HIWIND(高空干涉仪WIND观测)是第一款在白天和晚上都成功完成热圈风测量的法布里-珀罗气球干涉仪(FPI)。 HIWIND通过在约40 km的高度飞行,避免了强烈的太阳散射背景,并能够在白天对气辉中的多普勒频移进行遥感,以进行热层风观测。 HIWIND在2011年6月从基律纳(68N,65 MLAT)进行的首次飞行中,观测到持续的赤道风,而NCAR TIEGCM模型则预测了白天的极风。结合同时进行的EISCAT非相干散射雷达观测,HIWIND的白天Burnside因子值为0.85。 HIWIND数据似乎表明,极光椭圆附近的向上垂直风可能是实测的FPI与午夜附近的雷达衍生风之间存在较大差异的原因。

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