Earth's surface heat flux
We present a revised estimate of Earth's surface heat flux that is based upon a heat flow data-set with 38 347 measurements, which is 55% more than used in previous estimates. Our methodology, like others, accounts for hydrothermal circulation in young oceanic crust by utilising a half-space co...
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European Geosciences Union
2010
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:9397 2023-06-11T04:04:33+02:00 Earth's surface heat flux Davies, John Huw Davies, David Rhodri 2010-02-22 application/pdf https://orca.cardiff.ac.uk/id/eprint/9397/ https://doi.org/10.5194/se-1-5-2010 https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf en eng European Geosciences Union https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf Davies, John Huw https://orca.cardiff.ac.uk/view/cardiffauthors/A033374V.html orcid:0000-0003-2656-0260 orcid:0000-0003-2656-0260 and Davies, David Rhodri orcid:0000-0002-7662-9468 orcid:0000-0002-7662-9468 2010. Earth's surface heat flux. Solid Earth 1 (1) , pp. 5-24. 10.5194/se-1-5-2010 https://doi.org/10.5194/se-1-5-2010 file https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf doi:10.5194/se-1-5-2010 cc_by QE Geology Article PeerReviewed 2010 ftunivcardiff https://doi.org/10.5194/se-1-5-2010 2023-05-04T22:33:06Z We present a revised estimate of Earth's surface heat flux that is based upon a heat flow data-set with 38 347 measurements, which is 55% more than used in previous estimates. Our methodology, like others, accounts for hydrothermal circulation in young oceanic crust by utilising a half-space cooling approximation. For the rest of Earth's surface, we estimate the average heat flow for different geologic domains as defined by global digital geology maps; and then produce the global estimate by multiplying it by the total global area of that geologic domain. The averaging is done on a polygon set which results from an intersection of a 1 degree equal area grid with the original geology polygons; this minimises the adverse influence of clustering. These operations and estimates are derived accurately using methodologies from Geographical Information Science. We consider the virtually un-sampled Antarctica separately and also make a small correction for hot-spots in young oceanic lithosphere. A range of analyses is presented. These, combined with statistical estimates of the error, provide a measure of robustness. Our final preferred estimate is 47±2 TW, which is greater than previous estimates. Article in Journal/Newspaper Antarc* Antarctica Cardiff University: ORCA (Online Research @ Cardiff) Solid Earth 1 1 5 24 |
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Open Polar |
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Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
English |
topic |
QE Geology |
spellingShingle |
QE Geology Davies, John Huw Davies, David Rhodri Earth's surface heat flux |
topic_facet |
QE Geology |
description |
We present a revised estimate of Earth's surface heat flux that is based upon a heat flow data-set with 38 347 measurements, which is 55% more than used in previous estimates. Our methodology, like others, accounts for hydrothermal circulation in young oceanic crust by utilising a half-space cooling approximation. For the rest of Earth's surface, we estimate the average heat flow for different geologic domains as defined by global digital geology maps; and then produce the global estimate by multiplying it by the total global area of that geologic domain. The averaging is done on a polygon set which results from an intersection of a 1 degree equal area grid with the original geology polygons; this minimises the adverse influence of clustering. These operations and estimates are derived accurately using methodologies from Geographical Information Science. We consider the virtually un-sampled Antarctica separately and also make a small correction for hot-spots in young oceanic lithosphere. A range of analyses is presented. These, combined with statistical estimates of the error, provide a measure of robustness. Our final preferred estimate is 47±2 TW, which is greater than previous estimates. |
format |
Article in Journal/Newspaper |
author |
Davies, John Huw Davies, David Rhodri |
author_facet |
Davies, John Huw Davies, David Rhodri |
author_sort |
Davies, John Huw |
title |
Earth's surface heat flux |
title_short |
Earth's surface heat flux |
title_full |
Earth's surface heat flux |
title_fullStr |
Earth's surface heat flux |
title_full_unstemmed |
Earth's surface heat flux |
title_sort |
earth's surface heat flux |
publisher |
European Geosciences Union |
publishDate |
2010 |
url |
https://orca.cardiff.ac.uk/id/eprint/9397/ https://doi.org/10.5194/se-1-5-2010 https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf Davies, John Huw https://orca.cardiff.ac.uk/view/cardiffauthors/A033374V.html orcid:0000-0003-2656-0260 orcid:0000-0003-2656-0260 and Davies, David Rhodri orcid:0000-0002-7662-9468 orcid:0000-0002-7662-9468 2010. Earth's surface heat flux. Solid Earth 1 (1) , pp. 5-24. 10.5194/se-1-5-2010 https://doi.org/10.5194/se-1-5-2010 file https://orca.cardiff.ac.uk/id/eprint/9397/1/EARTH_Huw_Davies_2010a.pdf doi:10.5194/se-1-5-2010 |
op_rights |
cc_by |
op_doi |
https://doi.org/10.5194/se-1-5-2010 |
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Solid Earth |
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1 |
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1 |
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5 |
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24 |
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1768388679560069120 |