The change of surface wind in the north Western Siberia since 1966

Бібліографічні деталі
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012046, 5 p.]
Автор: Reshetko M. V. Margarita Viktorovna
Співавтор: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Інші автори: Chernikova A. V., Vasina E. V.
Резюме:Title screen
The statistical analysis of near-surface wind characteristics has been performed in the territory of the North of Western Siberia. The conclusion on wind speed decrease of different intensity for different directions and increase of calmness frequency is made. The maximum changes in wind speed are observed in winter and summer seasons, in transitional seasons these values are lower. The most intensive changes in wind direction frequency occur in summer; the less intensive ones are typical for winter.
Опубліковано: 2016
Серія:Geoecology and Environmental Protection
Предмети:
Онлайн доступ:http://dx.doi.org/10.1088/1755-1315/43/1/012046
http://earchive.tpu.ru/handle/11683/35155
Формат: Електронний ресурс Частина з книги
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650858
Опис
Резюме:Title screen
The statistical analysis of near-surface wind characteristics has been performed in the territory of the North of Western Siberia. The conclusion on wind speed decrease of different intensity for different directions and increase of calmness frequency is made. The maximum changes in wind speed are observed in winter and summer seasons, in transitional seasons these values are lower. The most intensive changes in wind direction frequency occur in summer; the less intensive ones are typical for winter.
DOI:10.1088/1755-1315/43/1/012046