On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal

The study of the climate in the past and the climate change in mainland Portugal using geothermal data has started in 1996. Reconstruction of ground surface temperature (GST) history from temperature logs measured in a 200 m deep borehole located 5 km away from the town of Évora in Portugal, indicat...

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Bibliographic Details
Main Author: António Correia
Format: Article in Journal/Newspaper
Language:English
Spanish
French
Portuguese
Published: CEG 2009
Subjects:
G
Online Access:https://doaj.org/article/66bb0f02be5d4ca6bdb8a209a6d0eac3
id ftdoajarticles:oai:doaj.org/article:66bb0f02be5d4ca6bdb8a209a6d0eac3
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spelling ftdoajarticles:oai:doaj.org/article:66bb0f02be5d4ca6bdb8a209a6d0eac3 2023-05-15T13:32:18+02:00 On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal António Correia 2009-06-01T00:00:00Z https://doaj.org/article/66bb0f02be5d4ca6bdb8a209a6d0eac3 EN ES FR PT eng spa fre por CEG http://www.ceg.ul.pt/finisterra/numeros/2009-87/87_09.pdf https://doaj.org/toc/0430-5027 0430-5027 https://doaj.org/article/66bb0f02be5d4ca6bdb8a209a6d0eac3 Finisterra - Revista Portuguesa de Geografia, Vol XLIV, Iss 87, Pp 109-116 (2009) Climate change Borehole temperatures Paleoclimatology Geography. Anthropology. Recreation G article 2009 ftdoajarticles 2022-12-31T09:10:40Z The study of the climate in the past and the climate change in mainland Portugal using geothermal data has started in 1996. Reconstruction of ground surface temperature (GST) history from temperature logs measured in a 200 m deep borehole located 5 km away from the town of Évora in Portugal, indicates a warming of 1K since the second half of the nineteenth century to the middle of the 90s of the twentieth century, increasing considerably in the last 10 years. Results of the reconstruction (based on a functional space inversion – FSI – method) are compared with air temperatures recorded at the Lisbon meteorological station since 1856. The airtemperature time series display a warming trend with the amplitude about 1K for the same period. The coupling of the air and ground temperature changes and their downward propagation by heat conduction was confirmed by repeated logging in November 2003, 6.7 years after obtaining the first temperature log. The method can be used in paleoclimatic studies in Antarctica as well as in areas with permafrost. Article in Journal/Newspaper Antarc* Antarctic Antarctica permafrost Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Spanish
French
Portuguese
topic Climate change
Borehole temperatures
Paleoclimatology
Geography. Anthropology. Recreation
G
spellingShingle Climate change
Borehole temperatures
Paleoclimatology
Geography. Anthropology. Recreation
G
António Correia
On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
topic_facet Climate change
Borehole temperatures
Paleoclimatology
Geography. Anthropology. Recreation
G
description The study of the climate in the past and the climate change in mainland Portugal using geothermal data has started in 1996. Reconstruction of ground surface temperature (GST) history from temperature logs measured in a 200 m deep borehole located 5 km away from the town of Évora in Portugal, indicates a warming of 1K since the second half of the nineteenth century to the middle of the 90s of the twentieth century, increasing considerably in the last 10 years. Results of the reconstruction (based on a functional space inversion – FSI – method) are compared with air temperatures recorded at the Lisbon meteorological station since 1856. The airtemperature time series display a warming trend with the amplitude about 1K for the same period. The coupling of the air and ground temperature changes and their downward propagation by heat conduction was confirmed by repeated logging in November 2003, 6.7 years after obtaining the first temperature log. The method can be used in paleoclimatic studies in Antarctica as well as in areas with permafrost.
format Article in Journal/Newspaper
author António Correia
author_facet António Correia
author_sort António Correia
title On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
title_short On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
title_full On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
title_fullStr On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
title_full_unstemmed On the possibility of using geothermal data for paleoclimate studies in the Antarctic: the experience from Portugal
title_sort on the possibility of using geothermal data for paleoclimate studies in the antarctic: the experience from portugal
publisher CEG
publishDate 2009
url https://doaj.org/article/66bb0f02be5d4ca6bdb8a209a6d0eac3
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
permafrost
genre_facet Antarc*
Antarctic
Antarctica
permafrost
op_source Finisterra - Revista Portuguesa de Geografia, Vol XLIV, Iss 87, Pp 109-116 (2009)
op_relation http://www.ceg.ul.pt/finisterra/numeros/2009-87/87_09.pdf
https://doaj.org/toc/0430-5027
0430-5027
https://doaj.org/article/66bb0f02be5d4ca6bdb8a209a6d0eac3
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