TEMPERATURE REGIME OF THE LOWER AND MIDDLE ATMOSPHERE IN CENTRAL YAKUTIA DURING SUDDEN STRATOSPHERIC WARMINGS IN THE PERIOD 2004-2019
https://doi.org/10.25587/SVFU.2021.22.2.012
Abstract
This paper presents the results of the analysis of the dynamics of the temperature regime in the lower and middle atmosphere in Central Yakutia during the maximum development of major sudden stratospheric warmings (SSW, ± 10 days) in the period 2004-2019. The days of the maximum development of major SSWs were determined according to the database of the Chemical Sciences Laboratory (CSL / NOAA). The database of the Global Systems Laboratory (GSL ESRL / NOAA) on radio sounding of the atmosphere (Yakutsk airport station, 62.08 N, 129.75 E, 103 m above sea level, index of the World Meteorological Organization - 24959) was used. When analyzing the dynamics of the temperature regime, we considered the radio sensing data relating to 24:00 h. Additionally, we used temperature profiles at isobaric heights from 1000-1 hPa (37 levels in height) according to the ERA-Interim reanalysis data with a latitudinal-longitudinal resolution of 1 x 1 degree. It was revealed that there was a high correlation (R>0.8) between the temperature profiles according to the data of radio sensing of the atmosphere and the ERA-Interim reanalysis. Spatio-temporal maps of the temperature regime at isobaric heights of 50 and 10 hPa were constructed according to the ERA-Interim reanalysis data. In general, for the period under consideration, the boundaries of the tropopause heights during the maximum SSW development were in the range from 7,301 to 10,200 m, and the average tropospheric temperature was from -42.7 to -29°C. Linear and polynomial trends in the mean tropospheric temperature and temperature at isobaric heights of 50 and 10 hPa were used to determine the growth and decline trends (troughs and ridges). It was revealed that the temperature regime of the stratosphere at the level of 50 hPa before and after the maximum development of major SSWs demostrated, in general, a general growing trend, with the exception of the events of 2006-2008, and at the level of 10 hPa - growth or decline. The dynamics of the temperature regime of the lower and middle atmosphere in Central Yakutia was of a regional (local) nature and depended not on the period (day) of maximum development, but on the location and periphery of the SSW.
About the Authors
M. S. Vasiliev
M.K. Ammosov North-Eastern Federal University
Russian Federation
Russian Federation
R. N. Boroyev
M.K. Ammosov North-Eastern Federal University
Russian Federation
Russian Federation
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Review
For citations:
Vasiliev M.S., Boroyev R.N. TEMPERATURE REGIME OF THE LOWER AND MIDDLE ATMOSPHERE IN CENTRAL YAKUTIA DURING SUDDEN STRATOSPHERIC WARMINGS IN THE PERIOD 2004-2019. Vestnik of North-Eastern Federal University Series "Earth Sciences". 2021;(2):5-16. (In Russ.) https://doi.org/10.25587/SVFU.2021.22.2.012
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