Magnetic declination of the territory of Ukraine: the results of observations and calculations

Оrlyuk, М.І.; Romenets, А.; Марченко, А. В.; Orlyuk, I.M.; Ivashchenko, I. N.

doi:10.24028/gzh.0203-3100.v37i2.2015.111307

Cited by 10 publications

(6 citation statements)

References 6 publications

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“…Since the dome of the geomagnetic field extends to an altitude of about 90 km, into the ionosphere layer, where the variation (rapidly Figure 1: An example of the data table of the geomagnetic observatory "Odesa" variable) component of the geomagnetic field is formed, regional magnetic anomalies can affect the manifestation of the variability of the geomagnetic field. When processing long-term, long-term observational data, the influence of the magnetic anomaly on the geomagnetic activity of the Earth was revealed (Maksymchuk & Orlyuk, 2018;Ryabov et al, 2019;Sukharev et al, 2018;Orlyuk et al, 2015).…”

Section: Magnetic Anomaly Zonementioning

confidence: 99%

Comparative Analysis of Magnetic Storms in the Odessa Magnetic Anomaly Region With Planetary and Ionospheric Storms During the Monitoring Program at Rt "Uran-4" (1987 – 2010)

Sobitnyak,

Ryabov,

Orlyuk

et al. 2023

OAP

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This work is a continuation of the study of the response of the Odesa geomagnetic anomaly to the manifestations of solar and planetary geomagnetic activity. Not far from the territory of this magnetic anomaly there is the geomagnetic observatory "Odesa" and the decameter radio telescope "URAN-4" of the RI NASU. A catalogue of magnetic storms for the period 1987-1994 and 2000-2009 was compiled for the monitoring program of high-power space radio sources at RT "URAN-4" using the database of the geomagnetic observatory "Odesa". In this paper, a comparative analysis of the features of the manifestations of geomagnetic storms in the zone of the Odesa magnetic anomaly, planetary storms and ionospheric storms in the 22nd and 23rd cycles of solar activity is carried out. The main results are as follows. The magnetic anomaly amplifies the effects of regional manifestations of planetary magnetic storms. The number of different types of magnetic storms and the dynamics of their changes in the Odesa anomaly differ significantly in the 22nd and 23rd cycles of solar activity. Comparisons have shown that the duration of magnetic storms in the Odessa anomaly is longer than the duration of planetary magnetic and ionospheric storms. According to the data of the «URAN-4» radio telescope, geomagnetic storms form various manifestations of the effects of ionospheric flickers and flux changes for space radio sources depending on the time of their observations. For the region of the Odesa geomagnetic anomaly, such comprehensive studies have not been carried out before. The conducted studies will become an important basis for understanding the influence of magnetic anomalies on the dynamics of the ionosphere during periods of solar and geomagnetic activity.

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Section: Magnetic Anomaly Zonementioning

confidence: 99%

Comparative Analysis of Magnetic Storms in the Odessa Magnetic Anomaly Region With Planetary and Ionospheric Storms During the Monitoring Program at Rt "Uran-4" (1987 – 2010)

Sobitnyak,

Ryabov,

Orlyuk

et al. 2023

OAP

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“…Analysis of recent research and publications. Traditional services include credit, operating, investment [7,52]. Credit is a service related to providing the borrowers with the money in terms of their repayment, payment and timeliness.…”

Section: ніколаєва людмила севастьяненко олена корольков олексій пmentioning

confidence: 99%

Law Problems in Banking (Protection of Consumer Rights in Banking Services)

2019

Conference Proceedings

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Each person throughout his life uses certain services to meet his needs. The service is a result of work, whether or not there is or there isn't a material form in it. In the process of building a democratic rule of law and becoming a market economy, it is important to provide, develop, improve and implement banking services, which in turn requires an improvement of the banking system in the state and the proper legal regulation of banking activities. Recently, it has undergone significant changes: the two-level banking system has been created, the activities of commercial banks and specialized lending and financial institutions are becoming more and more developed, the non-traditional areas of application of bank capital are expanding, and the nature of the relationship between banks and clients is changing.

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“…The upper edge of deep sources in most cases refers to the roof of the diorite layer of the Earth's crust. For the territory of the craton, the depth to this boundary is (8)(9)(10)(11)(12)(13)(14)(15) km. Exceptions are the Dnieper-Donetsk avlakogen and the Caspian depression, where the depth of immersion of the crystalline basement reaches 20 km.…”

mentioning

confidence: 99%

“…Naturally, ignoring this can lead to errors both in estimating the magnetization of the sources of the Earth's crust and in their spatial position. The possibility of taking this feature into account is realized in software and algorithmic support of the solution of the direct magnetoprospecting problem for a spherical Earth [4,6].…”

mentioning

confidence: 99%

See 1 more Smart Citation

3d Magnetic Model of the Earth Crust of the Eastern European Craton With the Account of the Earth Sphericity and Its Tectonic Interpretation

Оrlyuk¹,

Марченко²,

Bakarjieva³

2017

VKNUGEOL

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Magnetic declination of the territory of Ukraine: the results of observations and calculations

Cited by 10 publications

References 6 publications

Comparative Analysis of Magnetic Storms in the Odessa Magnetic Anomaly Region With Planetary and Ionospheric Storms During the Monitoring Program at Rt "Uran-4" (1987 – 2010)

Comparative Analysis of Magnetic Storms in the Odessa Magnetic Anomaly Region With Planetary and Ionospheric Storms During the Monitoring Program at Rt "Uran-4" (1987 – 2010)

Law Problems in Banking (Protection of Consumer Rights in Banking Services)

3d Magnetic Model of the Earth Crust of the Eastern European Craton With the Account of the Earth Sphericity and Its Tectonic Interpretation

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