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Optical turbulence measurements at a mountain ridge

机译:在山脊的光学湍流测量

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The optical turbulence conditions at a mountain ridge (North Oscuro Peak, White Sands Missile Range, NM) were determined from observations of fine wire sensors and a sodar (sonic detection and ranging). both instruments provided the temperature structure parameter (C_T~2) from which the refractive index structure parameter (C_n~2) was calculated using local measurements of temperature and pressure. The fine wire measurements were used to calibratethe sodar. Atmospheric measurements shown include wind speed and direction, temperature, and solar radiation snesed horizontally as well as parallel to the west-facing slope. Of particular emphasis isthe relationship of the sodar observations to solar radiation and wind speed and direction. The results are explained in terms of the geometry of the site and the mountain-valley wind regime. Results are shown as average range profiles of C_n~2 sensed at various zenith angles at different times of the day and as contours of C_n~2 in a vetical plane oriented normal to the west-facing slope.
机译:根据细线传感器和声雷达(声波探测和测距)的观测确定了山脊(北奥斯库罗峰,白沙导弹靶场,NM)的光学湍流条件。两种仪器都提供了温度结构参数(C_T〜2),通过使用温度和压力的局部测量值可以计算出折射率结构参数(C_n〜2)。细线测量用于校准声压。显示的大气测量包括风速和风向,温度以及水平和平行于西向倾斜的太阳辐射。特别强调的是声is观测与太阳辐射以及风速和风向的关系。根据场地的几何形状和山谷风态来解释结果。结果显示为在一天的不同时间在不同天顶角处感测到的C_n〜2的平均范围轮廓,并显示为垂直于西向倾斜的垂直平面中C_n〜2的轮廓。

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