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The regular nocturnal course of temperature in the midlatitude mesopause region according to hydroxyl airglow measurements

机译:根据羟基气辉测量,中纬度中经期区域的夜间温度规律

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Using ground-based spectral measurements in the near-infrared range at the Zvenigorod scientific station of the Institute of Atmospheric Physics (56A degrees N, 37A degrees E) for 2000-2013, we obtained average nighttime changes in rotational and vibrational temperatures of hydroxyl with its emission layer localized at mesopause heights. The rotational temperature reflects the kinetic temperature of the emission layer of the atmosphere. The analysis made it possible to determine the characteristics of the first three harmonics of diurnal temperature dynamics in the mesopause region both with and without altitudinal oscillations of the OH emission layer. In both cases, the second and third harmonics are statistically significant: their amplitudes are similar to 1 K and the phases of their first maxima are near 0300 and 0130 local solar time.
机译:使用2000-2013年大气物理研究所Zvenigorod科学站(北纬56A,东经37A)近红外范围内的地面光谱测量,我们得出了羟基的旋转和振动温度在夜间的平均变化它的发射层位于中绝经高度。旋转温度反映了大气排放层的动力学温度。该分析使得可以确定在具有和不具有OH发射层的垂直振荡的情况下,在更年期区域中昼夜温度动态的前三个谐波的特性。在这两种情况下,二次谐波和三次谐波在统计上都是有意义的:它们的振幅类似于1 K,并且它们的第一次最大值的相位接近当地太阳时间0300和0130。

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