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Long term variations in the frequency of polar mesospheric clouds in the Northern Hemisphere from SBUV

机译:SBUV对北半球极地中层云的频率进行长期变化

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Earlier studies have indicated that there is a secular increase in the occurrence frequency of polar mesospheric clouds (PMC), along with an anti-correlation with the solar activity. The combined data records from the Solar Backscatter Ultraviolet (SBUV and SBUV/2) instruments provide the longest satellite record (28 years) of the PMC frequency of occurrence. This record has been analyzed to determine the long-term variation in the PMC occurrence frequency in each of three latitude bands (54 degrees-64 degrees N, 64 degrees-74 degrees N, 74 degrees-82 degrees N). This analysis includes an adjustment for changes in the local time of measurement due to the satellite orbital drift, to take into account diurnal variations in the PMC frequency. Multiple linear regression fits using solar activity and time show that the occurrence frequency nearly doubles from solar maximum to solar minimum in all latitude bands. There is a long-term increase in the occurrence frequency ranging from 7% per decade at 64 degrees-74 degrees N to 20% per decade at 74 degrees-82 degrees N. These secular increases are significant at the 95% level for the 74 degrees-82 degrees N and all latitudes combined. We find a time lag of half a year (with an uncertainty of one year) between the minimum solar activity and the maximum PMC activity, consistent with our previous findings for PMC albedo. Citation: Shettle, E. P., M. T. DeLand, G. E. Thomas, and J.J. Olivero (2009), Long term variations in the frequency of polar mesospheric clouds in the Northern Hemisphere from SBUV, Geophys. Res. Lett., 36, L02803, doi:10.1029/2008GL036048.
机译:早期的研究表明,极地中层云(PMC)的发生频率会长期增加,并且与太阳活动呈反相关。来自太阳反向散射紫外线(SBUV和SBUV / 2)仪器的组合数据记录提供了PMC发生频率的最长卫星记录(28年)。已对该记录进行分析,以确定三个纬度带(54度至64度N,64度至74度N,74度至82度N)中每个纬度中PMC发生频率的长期变化。该分析包括对由于卫星轨道漂移而引起的本地测量时间变化的调整,以考虑PMC频率的日变化。使用太阳活动和时间的多元线性回归拟合表明,在所有纬度带中,发生频率从最大太阳到最小太阳几乎翻了一番。长期发生的频率从64度-74度N时每十年的7%增加到74度-82度N时每十年的20%。这些长期增长在74度到95%的水平上是显着的北纬82度和所有纬度的总和。我们发现最小太阳活动和最大PMC活动之间存在半年的时间间隔(不确定性为一年),这与我们之前对PMC反照率的发现一致。引用:Shettle,E. P.,M. T. DeLand,G. E. Thomas和J.J. Olivero(2009),来自SBUV的北半球极性中层云的频率长期变化,Geophys。 Res。 Lett。,36,L02803,doi:10.1029 / 2008GL036048。

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