Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations

In the present work the wind dynamics in the atmospheric boundary layer is studied; it is shown that wind slope angle at the ground surface with respect to isobars depends on the horizontal pressure gradients along parallel and meridian and not always equal to 45°.

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Main Authors: Yuliya Aleksandrovna Semenova, Kristina Stanislavovna Avakyan, Robert Gurgenovich Zakinyan
Format: Article
Language:Russian
Published: North-Caucasus Federal University 2022-09-01
Series:Наука. Инновации. Технологии
Subjects:
Online Access:https://scienceit.elpub.ru/jour/article/view/558
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author Yuliya Aleksandrovna Semenova
Kristina Stanislavovna Avakyan
Robert Gurgenovich Zakinyan
author_facet Yuliya Aleksandrovna Semenova
Kristina Stanislavovna Avakyan
Robert Gurgenovich Zakinyan
author_sort Yuliya Aleksandrovna Semenova
collection DOAJ
description In the present work the wind dynamics in the atmospheric boundary layer is studied; it is shown that wind slope angle at the ground surface with respect to isobars depends on the horizontal pressure gradients along parallel and meridian and not always equal to 45°.
format Article
id doaj-art-43ce154ecd7b4bb79974d2a9f5053e21
institution DOAJ
issn 2308-4758
language Russian
publishDate 2022-09-01
publisher North-Caucasus Federal University
record_format Article
series Наука. Инновации. Технологии
spelling doaj-art-43ce154ecd7b4bb79974d2a9f5053e212025-08-20T02:49:12ZrusNorth-Caucasus Federal UniversityНаука. Инновации. Технологии2308-47582022-09-01012629557Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientationsYuliya Aleksandrovna Semenova0Kristina Stanislavovna Avakyan1Robert Gurgenovich Zakinyan2Северо-Кавказский федеральный университетСеверо-Кавказский федеральный университетСеверо-Кавказский федеральный университетIn the present work the wind dynamics in the atmospheric boundary layer is studied; it is shown that wind slope angle at the ground surface with respect to isobars depends on the horizontal pressure gradients along parallel and meridian and not always equal to 45°.https://scienceit.elpub.ru/jour/article/view/558спираль экманапограничный слой атмосферыгеострофический ветерсила кориолисасила вязкого тренияekman's spiralatmospheric boundary layergeostrophic windcoriolis forceviscous force
spellingShingle Yuliya Aleksandrovna Semenova
Kristina Stanislavovna Avakyan
Robert Gurgenovich Zakinyan
Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
Наука. Инновации. Технологии
спираль экмана
пограничный слой атмосферы
геострофический ветер
сила кориолиса
сила вязкого трения
ekman's spiral
atmospheric boundary layer
geostrophic wind
coriolis force
viscous force
title Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
title_full Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
title_fullStr Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
title_full_unstemmed Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
title_short Development of the Ekman's theory of the atmospheric boundary layer at different isobars orientations
title_sort development of the ekman s theory of the atmospheric boundary layer at different isobars orientations
topic спираль экмана
пограничный слой атмосферы
геострофический ветер
сила кориолиса
сила вязкого трения
ekman's spiral
atmospheric boundary layer
geostrophic wind
coriolis force
viscous force
url https://scienceit.elpub.ru/jour/article/view/558
work_keys_str_mv AT yuliyaaleksandrovnasemenova developmentoftheekmanstheoryoftheatmosphericboundarylayeratdifferentisobarsorientations
AT kristinastanislavovnaavakyan developmentoftheekmanstheoryoftheatmosphericboundarylayeratdifferentisobarsorientations
AT robertgurgenovichzakinyan developmentoftheekmanstheoryoftheatmosphericboundarylayeratdifferentisobarsorientations