Vladimir I. Kaftan

Dr. Vladimir I. Kaftan

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Research Focus & Metrics

Academic Career Length

39Years (1988-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2019 in Izvestiya, Physics of the Solid Earth
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Alexei GvishianiAlexei Gvishiani
Alexei Gvishiani
VKVladimir I. Kaftan
Vladimir I. Kaftan
RKRoman Krasnoperov
Roman Krasnoperov
VTViktor Tatarinov
Viktor Tatarinov
EVE. V. Vavilin
E. V. Vavilin
The application of geoinformatics and systems analysis methods for processing and interpreting geospatial data in geophysics and geodynamics is considered. The modern capabilities of...

1 May 2013 in Journal of Advanced Research
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BKBoris Komitov
Boris Komitov
VKVladimir I. Kaftan
Vladimir I. Kaftan
The solar minimum between solar cycles 23 and 24 during the period 2007-2009 has been the longest and deepest one at least since for the last 100 years. We suggest that the Sun is going to his next supercenturial minimum. The main aim of this paper is to tell about arguments concerning this statement. They are based on series of studies, which have been provided during the period since 1997 up to 2010. The progress of solar cycle 24 since its minimum at the end of 2008 up to the end of October 2011 in the light of long term solar activity dynamics is analyzed.

1 January 2017 in Atomic Energy
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VTViktor Tatarinov
Viktor Tatarinov
VKVladimir I. Kaftan
Vladimir I. Kaftan
ISI. N. Seelev
I. N. Seelev

21 December 2017 in IOP Conference Series: Earth and Environmental Science
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VKVladimir I. Kaftan
Vladimir I. Kaftan
AMAndrey Melnikov
Andrey Melnikov
Research on deformation precursors of earthquakes was of immediate interest from the middle to the end of the previous century. The repeated conventional geodetic measurements, such as precise levelling and linear-angular networks, were used for the study. Many examples of studies referenced to strong seismic events using conventional geodetic techniques are presented in [T. Rikitake, 1976]. One of the first case studies of geodetic earthquake precursors was done by Yu.A. Meshcheryakov [1968]. Rare repetitions, insufficient densities and locations of control geodetic networks made difficult predicting future places and times of earthquakes occurrences. Intensive development of Global Navigation Satellite Systems (GNSS) during the recent decades makes research more effective. The results of GNSS observations in areas of three large earthquakes (Napa M6.1, USA, 2014; El Mayor Cucapah M7.2, USA, 2010; and Parkfield M6.0, USA, 2004) are treated and presented in the paper. The characteristics of land surface deformation before, during, and after earthquakes have been obtained. The results prove the presence of anomalous deformations near their epicentres. The temporal character of dilatation and shear strain changes show existence of spatial heterogeneity of deformation of the Earth's surface from months to years before the main shock close to it and at some distance from it. The revealed heterogeneities can be considered as deformation precursors of strong earthquakes. According to historical data and proper research values of critical deformations which are offered to be used for seismic danger scale creation based on continuous GNSS observations are received in a reference to the mentioned large earthquakes. It is shown that the approach has restrictions owing to uncertainty of the moment in the beginning of deformation accumulation and the place of expectation of another seismic event. Verification and clarification of the derived conclusions are proposed.


1 January 2015 in Geomagnetism and Aeronomy
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VKVladimir I. Kaftan
Vladimir I. Kaftan
RKRoman Krasnoperov
Roman Krasnoperov
Geodetic observations at geomagnetic observatories are used to orient reference directions in relation to a common coordinate grid. This problem is solved with the use of the measuring tools of global navigation satellite systems (GNSS). The results of experimental GNSS determinations at the St. Petersburg Geomagnetic Observatory, Russia, are presented. Combination of magnetic and GNSS observations is proposed in order to reveal the cause-effect relationships between magnetic field variations and global geodynamic processes.