Long-term trends of midlatitude horizontal mesosphere/lower thermosphere winds over four decades

IF 0.6 Q4 ENGINEERING, ELECTRICAL & ELECTRONIC
Christoph Jacobi, Aleš Kuchař, T. Renkwitz, J. Jaen
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引用次数: 0

Abstract

Abstract. We analyse 43 years of mesosphere/lower thermosphere (MLT) horizontal winds obtained from a joint analysis of low frequency (LF) spaced receiver lower ionospheric drift measurements from late 1978 through 2008 and VHF meteor radar wind observations since summer 2004 at Collm (51.3∘ N, 13.0∘ E). Due to limitations of the earlier LF measurements, we restrict ourselves to the analysis of monthly mean winds near 90 km, which represents the meteor peak height as well as mean LF reflection heights in the MLT. We observe mainly positive trends of the zonal prevailing wind throughout the year, while the meridional winds tend to decrease in magnitude in both summer and winter. Furthermore, there is a change in long-term trends around the late 1990s, which is most clearly visible in summer MLT winds. We compare these measurements with long-term partial reflection radar observations of winds at 81–85 km over Juliusruh (54.6∘ N, 13.4∘ E) since 1990, and find general qualitative agreement of trends except for summer. The latter can be explained by the different altitudes considered, and by the latitude dependence of the summer mesospheric jet.
四十年来中纬度水平中间层/低温层风的长期趋势
摘要。我们分析了43年的中间层/低层热层(MLT)水平风,这些风是通过联合分析1978年末至2008年低频(LF)间隔接收机下部电离层漂移测量和2004年夏季以来在科尔姆(51.3°N, 13.0°E)的甚高频流星雷达风观测得来的。由于早期低低频测量的局限性,我们只分析了90公里附近的月平均风,这代表了MLT中流星峰值高度和低低频反射平均高度。纬向盛行风全年主要呈正趋势,而经向风在夏季和冬季均有减小的趋势。此外,20世纪90年代末前后的长期趋势发生了变化,这在夏季MLT风中最为明显。我们将这些测量结果与1990年以来julusruh(54.6°N, 13.4°E)上空81-85公里风的长期部分反射雷达观测结果进行比较,发现除了夏季外,其他趋势在质量上大体一致。后者可以用考虑的不同高度和夏季中间层急流的纬度依赖性来解释。
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来源期刊
Advances in Radio Science
Advances in Radio Science ENGINEERING, ELECTRICAL & ELECTRONIC-
CiteScore
0.90
自引率
0.00%
发文量
3
审稿时长
45 weeks
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