Abstract

Abstract. We present kinetic temperatures at ~87 km and ~94 km altitudes inferred from OH (6,2) and O2 At(0,1) airglow observations, respectively, at South Pole (90° S), Antarctica in the austral winter of 2002. These OH and O2 rotational temperatures measurements show mesosphere and lower thermosphere (MLT) temperature anomalies prior to the 2002 Southern Hemisphere Sudden Stratospheric Warming (SSW) . In this paper we focus on the first of the three minor stratospheric warmings which preceded the major SSW event. Temperature anomalies observed in the MLT region show sudden cooling (ΔT=~30 K) in OH temperatures accompanied by warming (ΔT=~15 K) in O2 temperatures preceding the onset of SSW event by about three to four weeks. This shallow vertical extent of mesospheric cooling is in agreement with the numerical simulation of Coy et al. (2005), however, the model cooling was centered well below the mesopause level. The other observed feature of the South Pole MLT temperature dataset is the intensification of planetary wave activity prior to the onset of SSW event. Fourier analyses of both OH and O2 temperatures show amplification of planetary wave activity in the 5–10 day range prior to the onset of SSW. The timing of wave amplification seen in the wave spectra coincides with the peak in OH and O2 temperature anomalies.

Highlights

  • The winter polar stratosphere is characterized by an extensive vortex region that dynamically interacts with the winter mean flow

  • An unprecedented meteorological event associated with the Stratospheric Warmings (SSW) event was observed in the Southern Hemisphere during the winter of 2002

  • Averaged temperatures and zonal mean zonal winds from National Center for Environment Prediction (NCEP) Reanalysis dataset sampled at 10 hPa are shown in Fig. 3 as a function of latitude and universal time

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Summary

Introduction

The winter polar stratosphere is characterized by an extensive vortex region that dynamically interacts with the winter mean flow. This polar vortex is abruptly disrupted and the mean winds in the high latitude winter stratosphere reverse from westerly to easterly, causing Sudden Stratospheric Warmings (SSW) (Scherhag, 1960; Labitzke, 1965) Such an event can strongly affect the entire middle atmosphere, causing variations in the mesosphere and lower thermosphere (MLT) region circulation (Lysenko et al, 1975; Lauter and Schminder, 1976). We conclude by summarizing the significant findings of this study Both OH Meinel (6,2) and O2 At (0,1) airglow measurements were made by a half meter focal length, modified Czerny-Turner CCD Spectrometer (CCDS) located at South Pole, Antarctica. Kinetic temperatures in the MLT region are inferred from CCDS spectral measurements of OH(6,2) emission (mean altitude of 87 km) and O2 At(0,1) emission (mean altitude of 94 km)

OH temperature data
O2 temperatures
Results
Summary and conclusions
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