Role of Seasonality in the Evolution of Climate During the Last 100 Million Years
A simple climate model has been used to calculate the effect of past changes in the land-sea distribution on the seasonal cycle of temperatures during the last 100 million years. Modeled summer temperatures decreased over Greenland by more than 10°C and over Antarctica by 5° to 8°C. For the last 80...
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American Association for the Advancement of Science (AAAS)
1986
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Online Access: | http://dx.doi.org/10.1126/science.231.4738.579 https://www.science.org/doi/pdf/10.1126/science.231.4738.579 |
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craaas:10.1126/science.231.4738.579 2024-10-13T14:03:09+00:00 Role of Seasonality in the Evolution of Climate During the Last 100 Million Years Crowley, Thomas J. Short, David A. Mengel, John G. North, Gerald R. 1986 http://dx.doi.org/10.1126/science.231.4738.579 https://www.science.org/doi/pdf/10.1126/science.231.4738.579 en eng American Association for the Advancement of Science (AAAS) Science volume 231, issue 4738, page 579-584 ISSN 0036-8075 1095-9203 journal-article 1986 craaas https://doi.org/10.1126/science.231.4738.579 2024-09-19T04:01:19Z A simple climate model has been used to calculate the effect of past changes in the land-sea distribution on the seasonal cycle of temperatures during the last 100 million years. Modeled summer temperatures decreased over Greenland by more than 10°C and over Antarctica by 5° to 8°C. For the last 80 million years, this thermal response is comparable in magnitude to estimated atmospheric carbon dioxide effects. Analysis of paleontological data provides some support for the proposed hypothesis that large changes due to seasonality may have sometimes resulted in an ice-free state due to high summer temperatures rather than year-round warmth. Such "cool" non-glacials may have prevailed for as much as one-third of the last 100 million years. Article in Journal/Newspaper Antarc* Antarctica Greenland AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 231 4738 579 584 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
A simple climate model has been used to calculate the effect of past changes in the land-sea distribution on the seasonal cycle of temperatures during the last 100 million years. Modeled summer temperatures decreased over Greenland by more than 10°C and over Antarctica by 5° to 8°C. For the last 80 million years, this thermal response is comparable in magnitude to estimated atmospheric carbon dioxide effects. Analysis of paleontological data provides some support for the proposed hypothesis that large changes due to seasonality may have sometimes resulted in an ice-free state due to high summer temperatures rather than year-round warmth. Such "cool" non-glacials may have prevailed for as much as one-third of the last 100 million years. |
format |
Article in Journal/Newspaper |
author |
Crowley, Thomas J. Short, David A. Mengel, John G. North, Gerald R. |
spellingShingle |
Crowley, Thomas J. Short, David A. Mengel, John G. North, Gerald R. Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
author_facet |
Crowley, Thomas J. Short, David A. Mengel, John G. North, Gerald R. |
author_sort |
Crowley, Thomas J. |
title |
Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
title_short |
Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
title_full |
Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
title_fullStr |
Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
title_full_unstemmed |
Role of Seasonality in the Evolution of Climate During the Last 100 Million Years |
title_sort |
role of seasonality in the evolution of climate during the last 100 million years |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1126/science.231.4738.579 https://www.science.org/doi/pdf/10.1126/science.231.4738.579 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland |
genre_facet |
Antarc* Antarctica Greenland |
op_source |
Science volume 231, issue 4738, page 579-584 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.231.4738.579 |
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Science |
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231 |
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4738 |
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579 |
op_container_end_page |
584 |
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1812819567437676544 |