This is a preprint, a preliminary version of a manuscript that has not completed peer review at a journal. Research Square does not conduct peer review prior to posting preprints. The posting of a preprint on this server should not be interpreted as an endorsement of its validity or suitability for dissemination as established information or for guiding clinical practice.
Research article
A.C.T. Nieuwenhuizen
SRON Netherlands Institutefor Space Research, Utrecht, the Netherlands
Corresponding Author
ORCiD: https://orcid.org/0000-0003-3963-9015
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This work is licensed under a CC BY 4.0 License. Read Full License
In an earlier paper De Jager et al. (2018) studied the relation between the intensity variations of the variable equatorial and polar solar magnetic energy sources and that of the average terrestrial northern hemisphere ground temperature. It was found that during the period 1610 to about 1920 the variation in the smoothed terrestrial temperature and those of the solar magnetic radiation are well correlated but that after that an additional temperature increase became prominent, to reach around the year 2000 a value of about one degree above the sun-dependent forecast.
In the present paper an additional aspect of the above material is described, and we find that, apart from the above mentioned features, there is a delayed component of the sun-related heating with a time lag of about 16 years. The resulting relation between the variable flux of the solar magnetic energy and the average - smoothed – northern hemisphere ground temperature is presented in our final diagram, Fig. 13. Our results confirm earlier findings by other authors that ascribe such a time lag to glacier warming and cooling.
Keywords
Global warming, terrestrial temperature, solar magnetic fields, polar fields, equatorial fields, magnetic antipodal flux, correlation, delay
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This is a preprint, a preliminary version of a manuscript that has not completed peer review at a journal. Research Square does not conduct peer review prior to posting preprints. The posting of a preprint on this server should not be interpreted as an endorsement of its validity or suitability for dissemination as established information or for guiding clinical practice.
Research article
A.C.T. Nieuwenhuizen
SRON Netherlands Institutefor Space Research, Utrecht, the Netherlands
Corresponding Author
ORCiD: https://orcid.org/0000-0003-3963-9015
Badges
Prescreen
This manuscript passed our Prescreen assessment
Complete author information
Appropriate declaration statements
Potential risks to human health
Prescreen
History
CURRENT STATUS: Posted
Version 1
Posted 17 Aug, 2020
No community comments so far
Metrics
Comments: 0
PDF Downloads: ...
HTML Views: ...
Subject Areas
Planetary Science
License:
This work is licensed under a CC BY 4.0 License. Read Full License
In an earlier paper De Jager et al. (2018) studied the relation between the intensity variations of the variable equatorial and polar solar magnetic energy sources and that of the average terrestrial northern hemisphere ground temperature. It was found that during the period 1610 to about 1920 the variation in the smoothed terrestrial temperature and those of the solar magnetic radiation are well correlated but that after that an additional temperature increase became prominent, to reach around the year 2000 a value of about one degree above the sun-dependent forecast.
In the present paper an additional aspect of the above material is described, and we find that, apart from the above mentioned features, there is a delayed component of the sun-related heating with a time lag of about 16 years. The resulting relation between the variable flux of the solar magnetic energy and the average - smoothed – northern hemisphere ground temperature is presented in our final diagram, Fig. 13. Our results confirm earlier findings by other authors that ascribe such a time lag to glacier warming and cooling.
Figure 1
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6
Figure 7
Figure 8
Figure 9
Figure 10
Figure 11
Figure 12
Figure 13
The full text of this article is available to read as a PDF.
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