Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations

Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations

Dynamics of cloudiness above geologically active regions of Ukraine is studied on an example of the Crimean peninsula based on satellite pictures, data of surface meteorological observation stations and diagnostic and prognostic numerical simulation. The event on September 20, 2002 has been chosen a...

Повний опис

Збережено в:
Бібліографічні деталі
Дата:2012
Автори: Beliy, T. A., Pirnach, A. M.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116592
Теги: Додати тег
Немає тегів, Будьте першим, хто поставить тег для цього запису!
Назва журналу:Geofizicheskiy Zhurnal

Репозитарії

Geofizicheskiy Zhurnal
id journalsuranua-geofizicheskiy-article-116592
record_format ojs
spelling journalsuranua-geofizicheskiy-article-1165922020-10-07T12:02:45Z Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations Beliy, T. A. Pirnach, A. M. Dynamics of cloudiness above geologically active regions of Ukraine is studied on an example of the Crimean peninsula based on satellite pictures, data of surface meteorological observation stations and diagnostic and prognostic numerical simulation. The event on September 20, 2002 has been chosen as an example. An earthquake of class K = 8,8 with epicenter coordinates 44,77° n. l., 37,12 ° e. l., which happened during that period at 20 h 42 in the Crimea. Morphological changes were registered on the satellite pictures of cloudiness as linear cloudy anomalies (LCA) eight hours before the earthquake. LCA was located above geological fault, which separated the Scythian plate and the Crimean meganticlinorium. Numerical analysis of cloudiness evolution demonstrated that one of the possible factors of LCA appearance above geological faults of the Earth is inhomogeneous distribution of positive and negative anomalies of gravity force. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116592 10.24028/gzh.0203-3100.v34i1.2012.116592 Geofizicheskiy Zhurnal; Vol. 34 No. 1 (2012); 115-129 Геофизический журнал; Том 34 № 1 (2012); 115-129 Геофізичний журнал; Том 34 № 1 (2012); 115-129 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116592/110618 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Beliy, T. A.
Pirnach, A. M.
spellingShingle Beliy, T. A.
Pirnach, A. M.
Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
author_facet Beliy, T. A.
Pirnach, A. M.
author_sort Beliy, T. A.
title Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
title_short Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
title_full Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
title_fullStr Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
title_full_unstemmed Cloud dynamics over the geologically active zones of Ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
title_sort cloud dynamics over the geologically active zones of ukraine: diagnostic and predictive numerical modeling, surface and satellite observations
description Dynamics of cloudiness above geologically active regions of Ukraine is studied on an example of the Crimean peninsula based on satellite pictures, data of surface meteorological observation stations and diagnostic and prognostic numerical simulation. The event on September 20, 2002 has been chosen as an example. An earthquake of class K = 8,8 with epicenter coordinates 44,77° n. l., 37,12 ° e. l., which happened during that period at 20 h 42 in the Crimea. Morphological changes were registered on the satellite pictures of cloudiness as linear cloudy anomalies (LCA) eight hours before the earthquake. LCA was located above geological fault, which separated the Scythian plate and the Crimean meganticlinorium. Numerical analysis of cloudiness evolution demonstrated that one of the possible factors of LCA appearance above geological faults of the Earth is inhomogeneous distribution of positive and negative anomalies of gravity force.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2012
url https://journals.uran.ua/geofizicheskiy/article/view/116592
work_keys_str_mv AT beliyta clouddynamicsoverthegeologicallyactivezonesofukrainediagnosticandpredictivenumericalmodelingsurfaceandsatelliteobservations
AT pirnacham clouddynamicsoverthegeologicallyactivezonesofukrainediagnosticandpredictivenumericalmodelingsurfaceandsatelliteobservations
first_indexed 2024-04-21T19:40:57Z
last_indexed 2024-04-21T19:40:57Z
_version_ 1796974530992799744

Схожі ресурси