Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics

Valentin Krassilov; Sophia Barinova

doi:doi:10.11648/j.earth.20130201.11

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Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics

Valentin Krassilov, Sophia Barinova

Received: 19 January 2013 Accepted: Published: 20 February 2013

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Abstract

The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes

DOI	10.11648/j.earth.20130201.11
Published in	Earth Sciences (Volume 2, Issue 1, February 2013)
Page(s)	1-8
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Sea level; Geomagnetic reversals; Rotation geodynamics; Geochronology

References

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Valentin Krassilov, Sophia Barinova. (2013). Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sciences, 2(1), 1-8. https://doi.org/10.11648/j.earth.20130201.11

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ACS Style

Valentin Krassilov; Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013, 2(1), 1-8. doi: 10.11648/j.earth.20130201.11

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AMA Style

Valentin Krassilov, Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013;2(1):1-8. doi: 10.11648/j.earth.20130201.11

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@article{10.11648/j.earth.20130201.11,
  author = {Valentin Krassilov and Sophia Barinova},
  title = {Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics},
  journal = {Earth Sciences},
  volume = {2},
  number = {1},
  pages = {1-8},
  doi = {10.11648/j.earth.20130201.11},
  url = {https://doi.org/10.11648/j.earth.20130201.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20130201.11},
  abstract = {The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes},
 year = {2013}
}

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TY  - JOUR
T1  - Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics
AU  - Valentin Krassilov
AU  - Sophia Barinova
Y1  - 2013/02/20
PY  - 2013
N1  - https://doi.org/10.11648/j.earth.20130201.11
DO  - 10.11648/j.earth.20130201.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 1
EP  - 8
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20130201.11
AB  - The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes
VL  - 2
IS  - 1
ER  -

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Author Information

Valentin Krassilov

Inst. of Evolution, University of Haifa, Haifa, Israel
Sophia Barinova

Inst. of Evolution, University of Haifa, Haifa, Israel

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Valentin Krassilov, Sophia Barinova. (2013). Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sciences, 2(1), 1-8. https://doi.org/10.11648/j.earth.20130201.11

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ACS Style

Valentin Krassilov; Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013, 2(1), 1-8. doi: 10.11648/j.earth.20130201.11

Copy | Download

AMA Style

Valentin Krassilov, Sophia Barinova. Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics. Earth Sci. 2013;2(1):1-8. doi: 10.11648/j.earth.20130201.11

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@article{10.11648/j.earth.20130201.11,
  author = {Valentin Krassilov and Sophia Barinova},
  title = {Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics},
  journal = {Earth Sciences},
  volume = {2},
  number = {1},
  pages = {1-8},
  doi = {10.11648/j.earth.20130201.11},
  url = {https://doi.org/10.11648/j.earth.20130201.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20130201.11},
  abstract = {The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes},
 year = {2013}
}

Copy | Download

TY  - JOUR
T1  - Sea Level – Geomagnetic Polarity Correlation as Consequence of Rotation Geodynamics
AU  - Valentin Krassilov
AU  - Sophia Barinova
Y1  - 2013/02/20
PY  - 2013
N1  - https://doi.org/10.11648/j.earth.20130201.11
DO  - 10.11648/j.earth.20130201.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 1
EP  - 8
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20130201.11
AB  - The general tendencies of sea level and geomagnetic polarity evolution represented by their respective poly-nomial trend lines are metrically congruent and roughly coincident at the first order and prevailingly at the second order periodicities. Our analysis reveals chronological correlation of sea level highs and lows with the quiet and agitated states of geomagnetic field, both causally related to the density-dependent rotation forcing of oceanic/continental crust and the inner/outer core masses respectively. Their correlation thus confirms the role of rotation perturbations as a common pacesetter of the Earth’s surface and interior processes
VL  - 2
IS  - 1
ER  -

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