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Optical Turbulence Measurements and Models for Mount John University Observatory

机译:约翰山大学天文台的光学湍流测量和模型

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摘要

Abstract: Site measurements were collected at Mount John University Observatory in 2005 and 2007 usingna purpose-built scintillation detection and ranging system. CNn2n(h) profiling indicates a weak layer located atn12–14 km above sea level and strong low altitude turbulence extending up to 5 km. During calm weathernconditions, an additional layer was detected at 6–8 kmabove sea level. V(h) profiling suggests that tropopausenlayer velocities are nominally 12–30msn1n, and near-ground velocities range between 2 and 20msn1n,ndependent on weather. Little seasonal variation was detected in either CNn2n(h) and V(h) profiles. The averagencoherence length, r0, was found to be 7 1 cm for the full profile at a wavelength of 589 nm. The averagenisoplanatic angle, y0, was 1.0 0.1 arcsec. The mean turbulence altitude, h0, was found to be 2.0 0.7 kmnabove sea level.No average in theGreenwood frequency, fG, could be established due to the gaps present in thenV(h) profiles obtained. A modified Hufnagel-Valley model was developed to describe the CNn2n(h) profiles atnMount John, which estimates r0 at 6 cmand y0 at 0.9 arcsec. A series of V(h)models were developed, based onnthe Greenwood wind model with an additional peak located at low altitudes. Using the CNn2n(h) model and thensuggested V(h) model for moderate ground wind speeds, fG is estimated at 79Hz.
机译:摘要:站点测量是使用专用的闪烁检测和测距系统在2005年和2007年从约翰山大学天文台收集的。 CNn2n(h)廓线表示位于海拔12-14 km处的薄弱层,并延伸到5 km的强低空湍流。在平静的天气条件下,在海平面以上6–8公里处发现了一个附加层。 V(h)曲线表明,对流层顶面层速度名义上为12–30msn1n,近地面速度在2至20msn1n之间,与天气无关。在CNn2n(h)和V(h)曲线中几乎未检测到季节变化。发现在589 nm波长下的完整轮廓的平均相干长度r0为7 1 cm。平均等平面角y0为1.0 0.1 arcsec。平均湍流高度h0被发现在海平面的2.0 0.7 km处。由于当时的V(h)剖面中存在间隙,因此无法确定格林伍德频率fG的平均值。开发了修改后的Hufnagel-Valley模型来描述JohnMount John的CNn2n(h)轮廓,该轮廓估计r0为6 cm,y0为0.9 arcsec。基于格林伍德风模型开发了一系列的V(h)模型,并在低海拔地区增加了一个峰值。使用CNn2n(h)模型,然后针对中等地面风速使用建议的V(h)模型,估计fG为79Hz。

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