Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia

Quantitative reconstructions of mean July temperatures (T (jul)) based on new and previously published pollen-stratigraphical data covering the last 2000 years from 11 lakes in northern Fennoscandia and the Kola Peninsula are presented. T (jul) values are based on a previously published pollen-clima...

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Main Authors: Bjune, AE, Seppa, H, Birks, HJB
Format: Article in Journal/Newspaper
Language:unknown
Published: SPRINGER 2009
Subjects:
Online Access:http://discovery.ucl.ac.uk/162291/
id ftucl:oai:eprints.ucl.ac.uk.OAI2:162291
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:162291 2023-05-15T16:11:41+02:00 Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia Bjune, AE Seppa, H Birks, HJB 2009-01 http://discovery.ucl.ac.uk/162291/ unknown SPRINGER J PALEOLIMNOL , 41 (1) 43 - 56. (2009) Pollen stratigraphy Climate Medieval Warm Period Little Ice Age Fennoscandia Holocene climate change TREE-LINE AREA CENTRAL-SOUTHERN NORWAY ACCUMULATION RATE PAR HOLOCENE VEGETATION WESTERN NORWAY CLIMATE RECONSTRUCTIONS WINTER-PRECIPITATION PLANT MACROFOSSILS FINNISH LAPLAND ATLANTIC REGION Article 2009 ftucl 2017-03-09T23:11:01Z Quantitative reconstructions of mean July temperatures (T (jul)) based on new and previously published pollen-stratigraphical data covering the last 2000 years from 11 lakes in northern Fennoscandia and the Kola Peninsula are presented. T (jul) values are based on a previously published pollen-climate transfer function for the region with a root-mean-square error of prediction (RMSEP) of 0.99A degrees C. The most obvious trend in the inferred temperatures from all sites is the general decrease in T (jul) during the last 2000 years. Pollen-inferred T (jul) values on average 0.18 +/- A 0.56A degrees C (n = 91) higher than present (where "present" refers to the last three decades based on pollen-inferred T (jul) in core-top samples) are indicated between 0 and 1100 AD (2000-850 cal year BP), and temperatures -0.2 +/- A 0.47A degrees C (n = 78) below present are inferred between 1100 and 1900 AD (850-50 cal year BP). No consistent temperature peak is observed during the 'Medieval Warm Period', ca. 900-1200 AD (1100-750 cal year BP), but the cooler period between 1100 and 1900 AD (850-50 cal year BP) corresponds in general with the 'Little Ice Age' (LIA). Consistently with independent stable isotopic data, the composite pollen-based record suggests that the coldest periods of the LIA date to 1500-1600 AD (450-350 cal year BP) and 1800-1850 AD (150-100 cal year BP). An abrupt warming occurred at about 1900 AD and the twentieth century is the warmest century since about 1000 AD (950 cal year BP). Article in Journal/Newspaper Fennoscandia kola peninsula Lapland University College London: UCL Discovery Kola Peninsula Norway
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
topic Pollen stratigraphy
Climate
Medieval Warm Period
Little Ice Age
Fennoscandia
Holocene climate change
TREE-LINE AREA
CENTRAL-SOUTHERN NORWAY
ACCUMULATION RATE PAR
HOLOCENE VEGETATION
WESTERN NORWAY
CLIMATE RECONSTRUCTIONS
WINTER-PRECIPITATION
PLANT MACROFOSSILS
FINNISH LAPLAND
ATLANTIC REGION
spellingShingle Pollen stratigraphy
Climate
Medieval Warm Period
Little Ice Age
Fennoscandia
Holocene climate change
TREE-LINE AREA
CENTRAL-SOUTHERN NORWAY
ACCUMULATION RATE PAR
HOLOCENE VEGETATION
WESTERN NORWAY
CLIMATE RECONSTRUCTIONS
WINTER-PRECIPITATION
PLANT MACROFOSSILS
FINNISH LAPLAND
ATLANTIC REGION
Bjune, AE
Seppa, H
Birks, HJB
Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
topic_facet Pollen stratigraphy
Climate
Medieval Warm Period
Little Ice Age
Fennoscandia
Holocene climate change
TREE-LINE AREA
CENTRAL-SOUTHERN NORWAY
ACCUMULATION RATE PAR
HOLOCENE VEGETATION
WESTERN NORWAY
CLIMATE RECONSTRUCTIONS
WINTER-PRECIPITATION
PLANT MACROFOSSILS
FINNISH LAPLAND
ATLANTIC REGION
description Quantitative reconstructions of mean July temperatures (T (jul)) based on new and previously published pollen-stratigraphical data covering the last 2000 years from 11 lakes in northern Fennoscandia and the Kola Peninsula are presented. T (jul) values are based on a previously published pollen-climate transfer function for the region with a root-mean-square error of prediction (RMSEP) of 0.99A degrees C. The most obvious trend in the inferred temperatures from all sites is the general decrease in T (jul) during the last 2000 years. Pollen-inferred T (jul) values on average 0.18 +/- A 0.56A degrees C (n = 91) higher than present (where "present" refers to the last three decades based on pollen-inferred T (jul) in core-top samples) are indicated between 0 and 1100 AD (2000-850 cal year BP), and temperatures -0.2 +/- A 0.47A degrees C (n = 78) below present are inferred between 1100 and 1900 AD (850-50 cal year BP). No consistent temperature peak is observed during the 'Medieval Warm Period', ca. 900-1200 AD (1100-750 cal year BP), but the cooler period between 1100 and 1900 AD (850-50 cal year BP) corresponds in general with the 'Little Ice Age' (LIA). Consistently with independent stable isotopic data, the composite pollen-based record suggests that the coldest periods of the LIA date to 1500-1600 AD (450-350 cal year BP) and 1800-1850 AD (150-100 cal year BP). An abrupt warming occurred at about 1900 AD and the twentieth century is the warmest century since about 1000 AD (950 cal year BP).
format Article in Journal/Newspaper
author Bjune, AE
Seppa, H
Birks, HJB
author_facet Bjune, AE
Seppa, H
Birks, HJB
author_sort Bjune, AE
title Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
title_short Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
title_full Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
title_fullStr Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
title_full_unstemmed Quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern Fennoscandia
title_sort quantitative summer-temperature reconstructions for the last 2000 years based on pollen-stratigraphical data from northern fennoscandia
publisher SPRINGER
publishDate 2009
url http://discovery.ucl.ac.uk/162291/
geographic Kola Peninsula
Norway
geographic_facet Kola Peninsula
Norway
genre Fennoscandia
kola peninsula
Lapland
genre_facet Fennoscandia
kola peninsula
Lapland
op_source J PALEOLIMNOL , 41 (1) 43 - 56. (2009)
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