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THE POTENTIAL ENERGY DENSITY OF GRAVITY WAVES IN THE WINTER STRATOSPHERE AND LOWER MESOSPHERE FROM LIDAR MEASUREMENTS OVER YAKUTSK The potential energy density of gravity waves in the winter stratosphere and lower mesosphere from lidar measurements over Yakutsk

Опубликовано в Solar-Terrestrial Physics · Том 12, Номер 3 · Страницы 95–101 · Рубрика: Results of current research
DOI: https://doi.org/10.12737/stp-123202611 · EDN: JRSVAH
Получено: 21.10.2025 Одобрено: 02.03.2026 Опубликовано: 19.09.2026 Язык публикаций: ENG
This paper analyzes the characteristics of atmospheric gravity wave activity in the stratosphere and lower mesosphere during the winters from 2010 to 2017 by calculating their potential energy per unit mass from variations in the temperature profile obtained from lidar measurements near Yakutsk, Russia (62° N, 129° E). The most common vertical wavelengths identified through wavelet analysis are 4–6 km and 8–12 km. We examine temporal and altitude variability of waves with vertical wavelengths from 2 km to 20 km and a temporal resolution 10–20 min. The minimum and maximum values of the gravity wave potential energy density (GWPED) per unit mass vary from 5–10 J/kg at an altitude of 30 km to 100–250 J/kg at an altitude of 60 km. Moreover, the most significant variations in the potential energy of gravity waves are observed during sudden winter stratospheric warmings.
lidar, internal gravity waves, wavelet analysis, Brunt—Väisälä frequency, IGW potential energy density (GWPED)
Финансирование
The work was financially supported by the Russian Science Foundation (Grant No. 25-27-20119) https://rscf.ru/project/25-27-20119/. Experimental data was obtained within the framework of Government Assignment No. 125102712109-5
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