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Volume 16, issue 12
Atmos. Chem. Phys., 16, 7853–7866, 2016
https://doi.org/10.5194/acp-16-7853-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 7853–7866, 2016
https://doi.org/10.5194/acp-16-7853-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Jun 2016

Research article | 27 Jun 2016

Neutral atmosphere temperature trends and variability at 90 km, 70 °N, 19 °E, 2003–2014

Silje Eriksen Holmen1,2,3, Chris M. Hall2, and Masaki Tsutsumi4,5 Silje Eriksen Holmen et al.
  • 1The University Centre in Svalbard, Longyearbyen, Norway
  • 2Tromsø Geophysical Observatory, UiT – The Arctic University of Norway, Tromsø, Norway
  • 3Birkeland Centre for Space Science, Bergen, Norway
  • 4National Institute of Polar Research, Tokyo, Japan
  • 5The Graduate University for Advanced Studies (SOKENDAI), Department of Polar Science, Hayama, Japan

Abstract. Neutral temperatures at 90 km height above Tromsø, Norway, have been determined using ambipolar diffusion coefficients calculated from meteor echo fading times using the Nippon/Norway Tromsø Meteor Radar (NTMR). Daily temperature averages have been calculated from November 2003 to October 2014 and calibrated against temperature measurements from the Microwave Limb Sounder (MLS) on board Aura. Large-scale periodic oscillations ranging from ∼ 9 days to a year were found in the data using Lomb–Scargle periodogram analysis, and these components were used to seasonally detrend the daily temperature values before assessing trends. Harmonic oscillations found are associated with the large-scale circulation in the middle atmosphere together with planetary and gravity wave activity. The overall temperature change from 2003 to 2014 is −2.2 K ± 1.0 K decade−1, while in summer (May–June–July) and winter (November–December–January) the change is −0.3 K ± 3.1 K decade−1 and −11.6 K ± 4.1 K decade−1, respectively. The temperature record is at this point too short for incorporating a response to solar variability in the trend. How well suited a meteor radar is for estimating neutral temperatures at 90 km using meteor trail echoes is discussed, and physical explanations behind a cooling trend are proposed.

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Atmospheric temperatures at 90 km height above Tromsø, Norway, from 2003 to 2014 have been determined using meteor radar. Periodic oscillations ranging from ~ 9 days to a year were found in the dataset, which were related to the large-scale circulation in the middle atmosphere and with wave activity. A trend analysis was performed, revealing an overall weak cooling trend from 2003 to 2014, which is in line with other recent studies on mesopause region (~ 90 km) temperature trends.
Atmospheric temperatures at 90 km height above Tromsø, Norway, from 2003 to 2014 have been...
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