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Paleotemperatures of the Earth’s Surface. 1. Determination of the Average Annual Temperature of the Earth and HemispheresJournal of Engineering Physics and Thermophysics, 95
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More on paleotemperatures of the Earth surface
- Publisher
- Springer Journals
- Copyright
- Copyright © Springer Science+Business Media, LLC, part of Springer Nature 2022
- ISSN
- 1062-0125
- eISSN
- 1573-871X
- DOI
- 10.1007/s10891-022-02484-0
- Publisher site
- See Article on Publisher Site
Abstract
Two methods have been proposed for calculating the midlatitude near-surface heat-capacity of the Earth: 1) using the latitude variation of the Earth temperature, and 2) using the insolation of the Earth in the modern epoch and its variation with time. Using the obtained values of this heat capacity, profiles have been determined for the midlatitude paleotemperatures of the Earth in three extreme epochs in the past 50 thousand years, and the evolution of the paleotemperature in the past 200 thousand years has been calculated.
Journal
Journal of Engineering Physics and Thermophysics – Springer Journals
Published: Mar 1, 2022
Keywords: midlatitude temperature; insolation; heat capacity; paleotemperature; paleoclimate