Abstract

Abstract. A mesospheric water vapor data set obtained by the middle atmospheric water vapor radiometer (MIAWARA) close to Bern, Switzerland (46.88∘ N, 7.46∘ E) during October 2010 to September 2017 is investigated to study the long-term evolution and variability of quasi 2-day waves (Q2DWs). We present a climatological overview and an insight on the dynamical behavior of these waves with the occurring spectrum of periods as seen from a midlatitude observation site. Such a large and nearly continuous measurement data set as ours is rare and of high scientific value. The core results of our investigation indicate that the activity of the Q2DW manifests in burst-like events and is higher during winter months (November–February) than during summer months (May–August) for the altitude region of the mesosphere (up to 0.02 hPa in winter and up to 0.05 hPa in summer) accessible for the instrument. Single Q2DW events reach at most about 0.8 ppm in the H2O amplitudes. Further, monthly mean Q2DW amplitude spectra are presented and reveal a high-frequency variability between different months. A large fraction of identified Q2DW events (20 %) develop periods between 38 and 40 h. Further, we show the temporal evolution of monthly mean Q2DW oscillations continuously for all months and separated for single months over 7 years. The analysis of autobicoherence spectra gives evidence that Q2DWs are sometimes phase coupled to diurnal oscillations to a high degree and to waves with a period close to 18 h.

Highlights

  • The middle atmosphere is the part of Earth’s atmosphere that extends from about 10 to 110 km of altitude

  • In this study we present quite continuous observations of the quasi 2-day waves (Q2DWs) signature in middle atmospheric water vapor for 7 years (84 months) by the middle atmospheric water vapor radiometer MIAWARA at Bern–Zimmerwald (46.88◦ N, 7.46◦ E)

  • We find no clear trend in the temporal evolution of Q2DW activity within the two pressure layers

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Summary

Introduction

The middle atmosphere is the part of Earth’s atmosphere that extends from about 10 to 110 km of altitude. A high temporal resolution offers the possibility of investigating nonlinear wave–wave interactions between Q2DW and atmospheric waves with even shorter periods, like diurnal or semi-diurnal tides (Pancheva, 2001; Kumar et al, 2008; Guharay et al, 2015). Both observation types, global and local, complement each other and are required to study the Q2DW in all its facets within the Earth’s atmosphere.

Data from ground-based water vapor radiometry
Quasi 2-day wave activity
Monthly climatological overview
30 Winter Summer
Temporal evolution and variability
Autobicoherence analysis
Findings
Conclusions
Full Text
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