The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950

Multiple regression analyses were applied to decipher the correlation between monthly discharge, precipitation and temperature records and annual varve-thickness data from river Ångermanälven north-central Sweden between 1860 and 1950. Over the whole 90-year period we found generally a strong correl...

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Published in:The Holocene
Main Authors: Wohlfarth, Barbara, Holmquist, Björn, Cato, Ingemar, Linderson, Hans
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1998
Subjects:
Online Access:http://dx.doi.org/10.1191/095968398668399174
http://journals.sagepub.com/doi/pdf/10.1191/095968398668399174
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spelling crsagepubl:10.1191/095968398668399174 2024-04-28T08:32:37+00:00 The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950 Wohlfarth, Barbara Holmquist, Björn Cato, Ingemar Linderson, Hans 1998 http://dx.doi.org/10.1191/095968398668399174 http://journals.sagepub.com/doi/pdf/10.1191/095968398668399174 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 8, issue 5, page 521-534 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 1998 crsagepubl https://doi.org/10.1191/095968398668399174 2024-04-09T08:01:37Z Multiple regression analyses were applied to decipher the correlation between monthly discharge, precipitation and temperature records and annual varve-thickness data from river Ångermanälven north-central Sweden between 1860 and 1950. Over the whole 90-year period we found generally a strong correlation between spring/summer precipitation and annual varve thickness. However, there are clear indications that precipitation during the months of January and March–May was more important for the formation of varves in the early part of the twentieth century, while January, March, April and June seem to have been more significant during the later part of the nineteenth century. Monthly temperatures and annual varve thickness, on the other hand, did not show any significant correlations over the whole 90-year period, but, when split into 30-year periods, a dependence of varve thickness on October (1862–90) and March (1919–50) temperatures could be observed. Our results show that it is important to test each specific varve record against instrumental data sets before any conclusions can be drawn in terms of precipitation and/or temperature dependence. They also emphasize the necessity to correlate varve-thickness records against long instrumental series in order to detect any changing forcing mechanisms. Article in Journal/Newspaper Northern Sweden SAGE Publications The Holocene 8 5 521 534
institution Open Polar
collection SAGE Publications
op_collection_id crsagepubl
language English
topic Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
spellingShingle Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
Wohlfarth, Barbara
Holmquist, Björn
Cato, Ingemar
Linderson, Hans
The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
topic_facet Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
description Multiple regression analyses were applied to decipher the correlation between monthly discharge, precipitation and temperature records and annual varve-thickness data from river Ångermanälven north-central Sweden between 1860 and 1950. Over the whole 90-year period we found generally a strong correlation between spring/summer precipitation and annual varve thickness. However, there are clear indications that precipitation during the months of January and March–May was more important for the formation of varves in the early part of the twentieth century, while January, March, April and June seem to have been more significant during the later part of the nineteenth century. Monthly temperatures and annual varve thickness, on the other hand, did not show any significant correlations over the whole 90-year period, but, when split into 30-year periods, a dependence of varve thickness on October (1862–90) and March (1919–50) temperatures could be observed. Our results show that it is important to test each specific varve record against instrumental data sets before any conclusions can be drawn in terms of precipitation and/or temperature dependence. They also emphasize the necessity to correlate varve-thickness records against long instrumental series in order to detect any changing forcing mechanisms.
format Article in Journal/Newspaper
author Wohlfarth, Barbara
Holmquist, Björn
Cato, Ingemar
Linderson, Hans
author_facet Wohlfarth, Barbara
Holmquist, Björn
Cato, Ingemar
Linderson, Hans
author_sort Wohlfarth, Barbara
title The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
title_short The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
title_full The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
title_fullStr The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
title_full_unstemmed The climatic significance of clastic varves in the Ångermanälven Estuary, northern Sweden, AD 1860 to 1950
title_sort climatic significance of clastic varves in the ångermanälven estuary, northern sweden, ad 1860 to 1950
publisher SAGE Publications
publishDate 1998
url http://dx.doi.org/10.1191/095968398668399174
http://journals.sagepub.com/doi/pdf/10.1191/095968398668399174
genre Northern Sweden
genre_facet Northern Sweden
op_source The Holocene
volume 8, issue 5, page 521-534
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1191/095968398668399174
container_title The Holocene
container_volume 8
container_issue 5
container_start_page 521
op_container_end_page 534
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