首页> 外文会议>ESA Symposium on European Rocket and Balloon Programmes and Related Research >ROCKET OBSERVATIONS OF POSITIVE IONS DURING POLAR MESOSPHERE WINTER ECHO CONDITIONS AT ANDENES IN JANUARY 2005; FIRST ANALYSIS AND INTERPRETATIONS
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ROCKET OBSERVATIONS OF POSITIVE IONS DURING POLAR MESOSPHERE WINTER ECHO CONDITIONS AT ANDENES IN JANUARY 2005; FIRST ANALYSIS AND INTERPRETATIONS

机译:2005年1月Andenes极地肌间冬季回声条件下阳性离子的火箭探测;第一次分析和解释

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On January 18, 2005, two instrumented miniaturised rocket payloads, each with a Positive Ion Probe (PIP) and a Faraday rotation/differential absorption experiment, were launched from Andoya Rocket Range (69°N). The instrumented payloads were launched into conditions with Polar Mesosphere Winter Echoes (PMWE) as part of a salvo of meteorological rockets measuring temperature and wind using falling spheres and chaff. Layers of PMWE were detected in the altitude range 55-77 km by the 53.5 MHz ALWIN radar. Fluctuations in the ion density, as measured in situ by the instrumented payloads, show that there was turbulence inside the PMWE layers, but not above/below and between. Data from the PIPs are analysed and related to the geophysical conditions, as observed with the ALWIN radar and meteorological rockets.
机译:2005年1月18日,由Andoya Rocket(69°N)发射两种仪表化的小型火箭有效载荷,每种具有正离子探针(PIP)和法拉第旋转/微分吸收实验。仪表的有效载荷被推动到具有极地冬季冬季回声(PMWE)的条件下,作为气象火箭队的丹琴赛的一部分使用落球和谷壳测量温度和风。在53.5 MHz Alwin雷达中,在高度范围内检测到PMWE层。离子密度的波动,如仪表有效载荷原位测量,表明PMWE层内部存在湍流,但在下方和下方之间存在湍流。分析来自点的数据并与地球物理条件相关,与阿尔文雷达和气象火箭队观察到。

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