Variations in Solar Radiation and the Cause of Ice Ages

Abstract Most astronomical hypotheses on the causes of ice ages are dynamically untenable. Alterations in the amount of solar radiation, however, have long been recognized as a possible cause, but only with recent progress in the theory of stellar evolution has it become clear that such changes must...

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Published in:Journal of Glaciology
Main Authors: Hoyle, F., Lyttleton, R. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1950
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000012818
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012818
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spelling crcambridgeupr:10.1017/s0022143000012818 2024-03-03T08:46:09+00:00 Variations in Solar Radiation and the Cause of Ice Ages Hoyle, F. Lyttleton, R. A. 1950 http://dx.doi.org/10.1017/s0022143000012818 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012818 en eng Cambridge University Press (CUP) Journal of Glaciology volume 1, issue 08, page 453-455 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1950 crcambridgeupr https://doi.org/10.1017/s0022143000012818 2024-02-08T08:40:23Z Abstract Most astronomical hypotheses on the causes of ice ages are dynamically untenable. Alterations in the amount of solar radiation, however, have long been recognized as a possible cause, but only with recent progress in the theory of stellar evolution has it become clear that such changes must occur. At irregular intervals the sun will pass, and will have passed, with low relative speeds through interstellar hydrogen clouds, and the gravitational action of the sun leads to an increase in the quantity of material falling to the surface with high velocity. The conversion of the kinetic energy of fall of this material results in an increase of emission at the solar surface. Increases of order up to about 10 per cent of the present total radiation could occur, and the process is such that the extra energy would be located mainly in the shorter wavelengths. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 08 453 455
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hoyle, F.
Lyttleton, R. A.
Variations in Solar Radiation and the Cause of Ice Ages
topic_facet Earth-Surface Processes
description Abstract Most astronomical hypotheses on the causes of ice ages are dynamically untenable. Alterations in the amount of solar radiation, however, have long been recognized as a possible cause, but only with recent progress in the theory of stellar evolution has it become clear that such changes must occur. At irregular intervals the sun will pass, and will have passed, with low relative speeds through interstellar hydrogen clouds, and the gravitational action of the sun leads to an increase in the quantity of material falling to the surface with high velocity. The conversion of the kinetic energy of fall of this material results in an increase of emission at the solar surface. Increases of order up to about 10 per cent of the present total radiation could occur, and the process is such that the extra energy would be located mainly in the shorter wavelengths.
format Article in Journal/Newspaper
author Hoyle, F.
Lyttleton, R. A.
author_facet Hoyle, F.
Lyttleton, R. A.
author_sort Hoyle, F.
title Variations in Solar Radiation and the Cause of Ice Ages
title_short Variations in Solar Radiation and the Cause of Ice Ages
title_full Variations in Solar Radiation and the Cause of Ice Ages
title_fullStr Variations in Solar Radiation and the Cause of Ice Ages
title_full_unstemmed Variations in Solar Radiation and the Cause of Ice Ages
title_sort variations in solar radiation and the cause of ice ages
publisher Cambridge University Press (CUP)
publishDate 1950
url http://dx.doi.org/10.1017/s0022143000012818
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000012818
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 1, issue 08, page 453-455
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000012818
container_title Journal of Glaciology
container_volume 1
container_issue 08
container_start_page 453
op_container_end_page 455
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