Vertical Helicity Flux as an Index of General Atmospheric Circulation
- Авторы: Kurgansky M.1,2, Maksimenkov L.1, Khapaev A.1, Chkhetiani O.1,3
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Учреждения:
- Obukhov Institute of Atmospheric Physics
- Faculty of Physics
- Space Research Institute
- Выпуск: Том 479, № 2 (2018)
- Страницы: 477-481
- Раздел: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/192801
- DOI: https://doi.org/10.1134/S1028334X18040037
- ID: 192801
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Аннотация
As an index of the general atmospheric circulation over the hemisphere, it is proposed to calculate the hemisphere-area-averaged (poleward of the latitude 20°) product of the Coriolis parameter by the wind velocity squared at the upper boundary of the planetary boundary layer. In practical calculations, data on the wind velocity at an isobaric level of 850 hPa were used. Control calculations for the 900 hPa level gave similar results. It is shown that the index introduced adequately characterizes the seasonal and interannual variability of the general atmospheric circulation over both hemispheres.
Об авторах
M. Kurgansky
Obukhov Institute of Atmospheric Physics; Faculty of Physics
Автор, ответственный за переписку.
Email: kurgansk@ifaran.ru
Россия, Moscow, 119017; Moscow, 119991
L. Maksimenkov
Obukhov Institute of Atmospheric Physics
Email: kurgansk@ifaran.ru
Россия, Moscow, 119017
A. Khapaev
Obukhov Institute of Atmospheric Physics
Email: kurgansk@ifaran.ru
Россия, Moscow, 119017
O. Chkhetiani
Obukhov Institute of Atmospheric Physics; Space Research Institute
Email: kurgansk@ifaran.ru
Россия, Moscow, 119017; Moscow, 117997