'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends
Climatic changes resulting from greenhouse gases will be superimposed on natural climatic variations. High-resolution proxy records of past climate can be used to extend our perspective on regional and hemispheric changes of climate back in time by several hundred years. Using historical, tree-ring...
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Online Access: | https://ueaeprints.uea.ac.uk/id/eprint/33813/ https://doi.org/10.1177/095968369300300409 |
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ftuniveastangl:oai:ueaeprints.uea.ac.uk:33813 2023-06-06T11:54:53+02:00 'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends Bradley, Raymond S. Jones, Philip D. 1993 https://ueaeprints.uea.ac.uk/id/eprint/33813/ https://doi.org/10.1177/095968369300300409 unknown Bradley, Raymond S. and Jones, Philip D. (1993) 'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends. The Holocene, 3 (4). pp. 367-376. ISSN 0959-6836 doi:10.1177/095968369300300409 Article PeerReviewed 1993 ftuniveastangl https://doi.org/10.1177/095968369300300409 2023-04-13T22:31:36Z Climatic changes resulting from greenhouse gases will be superimposed on natural climatic variations. High-resolution proxy records of past climate can be used to extend our perspective on regional and hemispheric changes of climate back in time by several hundred years. Using historical, tree-ring and ice core data, we examine climatic variations during the period commonly called the 'Little Ice Age'. The coldest conditions of the last 560 years were between AD 1570 and 1730, and in the nineteenth century. Unusually warm conditions have prevailed since the 1920s, probably related to a relative absence of major explosive volcanic eruptions and higher levels of greenhouse gases. Article in Journal/Newspaper ice core University of East Anglia: UEA Digital Repository The Holocene 3 4 367 376 |
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Open Polar |
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University of East Anglia: UEA Digital Repository |
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ftuniveastangl |
language |
unknown |
description |
Climatic changes resulting from greenhouse gases will be superimposed on natural climatic variations. High-resolution proxy records of past climate can be used to extend our perspective on regional and hemispheric changes of climate back in time by several hundred years. Using historical, tree-ring and ice core data, we examine climatic variations during the period commonly called the 'Little Ice Age'. The coldest conditions of the last 560 years were between AD 1570 and 1730, and in the nineteenth century. Unusually warm conditions have prevailed since the 1920s, probably related to a relative absence of major explosive volcanic eruptions and higher levels of greenhouse gases. |
format |
Article in Journal/Newspaper |
author |
Bradley, Raymond S. Jones, Philip D. |
spellingShingle |
Bradley, Raymond S. Jones, Philip D. 'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
author_facet |
Bradley, Raymond S. Jones, Philip D. |
author_sort |
Bradley, Raymond S. |
title |
'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
title_short |
'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
title_full |
'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
title_fullStr |
'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
title_full_unstemmed |
'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends |
title_sort |
'little ice age' summer temperature variations: their nature and relevance to recent global warming trends |
publishDate |
1993 |
url |
https://ueaeprints.uea.ac.uk/id/eprint/33813/ https://doi.org/10.1177/095968369300300409 |
genre |
ice core |
genre_facet |
ice core |
op_relation |
Bradley, Raymond S. and Jones, Philip D. (1993) 'Little Ice Age' summer temperature variations: Their nature and relevance to recent global warming trends. The Holocene, 3 (4). pp. 367-376. ISSN 0959-6836 doi:10.1177/095968369300300409 |
op_doi |
https://doi.org/10.1177/095968369300300409 |
container_title |
The Holocene |
container_volume |
3 |
container_issue |
4 |
container_start_page |
367 |
op_container_end_page |
376 |
_version_ |
1767961457425645568 |