Standard

Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects). / Semakov, Nikolay; Kovalev, Aleksandr; Pavlov, Anatoliy и др.

в: E3S Web of Conferences, Том 196, 02020, 16.10.2020.

Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование

Harvard

Semakov, N, Kovalev, A, Pavlov, A & Fedotova, O 2020, 'Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects)', E3S Web of Conferences, Том. 196, 02020. https://doi.org/10.1051/e3sconf/202019602020

APA

Semakov, N., Kovalev, A., Pavlov, A., & Fedotova, O. (2020). Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects). E3S Web of Conferences, 196, [02020]. https://doi.org/10.1051/e3sconf/202019602020

Vancouver

Semakov N, Kovalev A, Pavlov A, Fedotova O. Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects). E3S Web of Conferences. 2020 окт. 16;196:02020. doi: 10.1051/e3sconf/202019602020

Author

Semakov, Nikolay ; Kovalev, Aleksandr ; Pavlov, Anatoliy и др. / Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects). в: E3S Web of Conferences. 2020 ; Том 196.

BibTeX

@article{0a5e3e70bc1c4b648b64598ce83bc9a2,
title = "Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects)",
abstract = "The parameters of the equivalent central dipole calculated using hourly values of the magnetic field elements during 2011: the angular elements transformed to the hourly values of the geographic coordinates of the North magnetic pole and the intensity values transformed to local magnetic constant. Next step is the calculation of the daily mean values at every hour. This method applied to both current digital data and historical data presented as monthly tables of hourly values. The advantage of method is its ability to show the changes of the magnetic field independently from daily variation. Using of the {"}integrate{"}parameters (the magnetic pole coordinates and local magneto constant) allows detect the regional features of its variations. The features in the daily values compared with anomalous geological and geophysical events observed in the past and predicted in the near future. ",
author = "Nikolay Semakov and Aleksandr Kovalev and Anatoliy Pavlov and Olga Fedotova",
note = "Publisher Copyright: {\textcopyright} 2020 The Authors, published by EDP Sciences. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.; 11th International Conference �Solar-Terrestrial Relations and Physics of Earthquake Precursors�, STRPEP 2020 ; Conference date: 22-09-2020 Through 25-09-2020",
year = "2020",
month = oct,
day = "16",
doi = "10.1051/e3sconf/202019602020",
language = "English",
volume = "196",
journal = "E3S Web of Conferences",
issn = "2555-0403",
publisher = "EDP Sciences",

}

RIS

TY - JOUR

T1 - Moving daily average of the hourly magnetic field values - The example of usage at Novosibirsk Observatory during 2011 (results and prospects)

AU - Semakov, Nikolay

AU - Kovalev, Aleksandr

AU - Pavlov, Anatoliy

AU - Fedotova, Olga

N1 - Publisher Copyright: © 2020 The Authors, published by EDP Sciences. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.

PY - 2020/10/16

Y1 - 2020/10/16

N2 - The parameters of the equivalent central dipole calculated using hourly values of the magnetic field elements during 2011: the angular elements transformed to the hourly values of the geographic coordinates of the North magnetic pole and the intensity values transformed to local magnetic constant. Next step is the calculation of the daily mean values at every hour. This method applied to both current digital data and historical data presented as monthly tables of hourly values. The advantage of method is its ability to show the changes of the magnetic field independently from daily variation. Using of the "integrate"parameters (the magnetic pole coordinates and local magneto constant) allows detect the regional features of its variations. The features in the daily values compared with anomalous geological and geophysical events observed in the past and predicted in the near future.

AB - The parameters of the equivalent central dipole calculated using hourly values of the magnetic field elements during 2011: the angular elements transformed to the hourly values of the geographic coordinates of the North magnetic pole and the intensity values transformed to local magnetic constant. Next step is the calculation of the daily mean values at every hour. This method applied to both current digital data and historical data presented as monthly tables of hourly values. The advantage of method is its ability to show the changes of the magnetic field independently from daily variation. Using of the "integrate"parameters (the magnetic pole coordinates and local magneto constant) allows detect the regional features of its variations. The features in the daily values compared with anomalous geological and geophysical events observed in the past and predicted in the near future.

UR - http://www.scopus.com/inward/record.url?scp=85097210077&partnerID=8YFLogxK

U2 - 10.1051/e3sconf/202019602020

DO - 10.1051/e3sconf/202019602020

M3 - Conference article

AN - SCOPUS:85097210077

VL - 196

JO - E3S Web of Conferences

JF - E3S Web of Conferences

SN - 2555-0403

M1 - 02020

T2 - 11th International Conference �Solar-Terrestrial Relations and Physics of Earthquake Precursors�, STRPEP 2020

Y2 - 22 September 2020 through 25 September 2020

ER -

ID: 26669502