Arctic marine climate of the early nineteenth century

The climate of the early nineteenth century is likely to have been significantly cooler than that of today, as it was a period of low solar activity (the Dalton minimum) and followed a series of large volcanic eruptions. Proxy reconstructions of the temperature of the period do not agree well on the...

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Main Authors: P. Brohan, C. Ward, G. Willetts, C. Wilkinson, R. Allan, D. Wheeler
Format: Article
Language:English
Published: Copernicus Publications 2010-05-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/6/315/2010/cp-6-315-2010.pdf
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author P. Brohan
C. Ward
G. Willetts
C. Wilkinson
R. Allan
D. Wheeler
author_facet P. Brohan
C. Ward
G. Willetts
C. Wilkinson
R. Allan
D. Wheeler
author_sort P. Brohan
collection DOAJ
description The climate of the early nineteenth century is likely to have been significantly cooler than that of today, as it was a period of low solar activity (the Dalton minimum) and followed a series of large volcanic eruptions. Proxy reconstructions of the temperature of the period do not agree well on the size of the temperature change, so other observational records from the period are particularly valuable. Weather observations have been extracted from the reports of the noted whaling captain William Scoresby Jr., and from the records of a series of Royal Navy expeditions to the Arctic, preserved in the UK National Archives. They demonstrate that marine climate in 1810–1825 was marked by consistently cold summers, with abundant sea-ice. But although the period was significantly colder than the modern average, there was considerable variability: in the Greenland Sea the summers following the Tambora eruption (1816 and 1817) were noticeably warmer, and had less sea-ice coverage, than the years immediately preceding them; and the sea-ice coverage in Lancaster Sound in 1819 and 1820 was low even by modern standards.
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spelling doaj.art-10d487e12561437bbbd38c4b682d438b2022-12-22T00:38:28ZengCopernicus PublicationsClimate of the Past1814-93241814-93322010-05-016331532410.5194/cp-6-315-2010Arctic marine climate of the early nineteenth centuryP. BrohanC. WardG. WillettsC. WilkinsonR. AllanD. WheelerThe climate of the early nineteenth century is likely to have been significantly cooler than that of today, as it was a period of low solar activity (the Dalton minimum) and followed a series of large volcanic eruptions. Proxy reconstructions of the temperature of the period do not agree well on the size of the temperature change, so other observational records from the period are particularly valuable. Weather observations have been extracted from the reports of the noted whaling captain William Scoresby Jr., and from the records of a series of Royal Navy expeditions to the Arctic, preserved in the UK National Archives. They demonstrate that marine climate in 1810–1825 was marked by consistently cold summers, with abundant sea-ice. But although the period was significantly colder than the modern average, there was considerable variability: in the Greenland Sea the summers following the Tambora eruption (1816 and 1817) were noticeably warmer, and had less sea-ice coverage, than the years immediately preceding them; and the sea-ice coverage in Lancaster Sound in 1819 and 1820 was low even by modern standards.http://www.clim-past.net/6/315/2010/cp-6-315-2010.pdf
spellingShingle P. Brohan
C. Ward
G. Willetts
C. Wilkinson
R. Allan
D. Wheeler
Arctic marine climate of the early nineteenth century
Climate of the Past
title Arctic marine climate of the early nineteenth century
title_full Arctic marine climate of the early nineteenth century
title_fullStr Arctic marine climate of the early nineteenth century
title_full_unstemmed Arctic marine climate of the early nineteenth century
title_short Arctic marine climate of the early nineteenth century
title_sort arctic marine climate of the early nineteenth century
url http://www.clim-past.net/6/315/2010/cp-6-315-2010.pdf
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