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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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/65286 2024-01-14T10:01:12+01:00 Earth's surface heat flux Davies, J Davies, Rhodri http://hdl.handle.net/1885/65286 https://openresearch-repository.anu.edu.au/bitstream/1885/65286/5/Davies_DR_2010_Earth%2527s_surface.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65286/7/01_Davies_Earth%27s_surface_heat_flux_2010.pdf.jpg unknown Copernicus GmbH 1869-9510 http://hdl.handle.net/1885/65286 https://openresearch-repository.anu.edu.au/bitstream/1885/65286/5/Davies_DR_2010_Earth%2527s_surface.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65286/7/01_Davies_Earth%27s_surface_heat_flux_2010.pdf.jpg Solid Earth Keywords: Antarctica Data sets Earth's surface Geographical information Geologic domains Global estimate Half-space Hotspots Hydrothermal circulation Oceanic crust Oceanic lithosphere Estimation Geographic information systems Geology Heat transfer He Journal article ftanucanberra 2023-12-15T09:32:57Z 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 Australian National University: ANU Digital Collections |
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Australian National University: ANU Digital Collections |
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Keywords: Antarctica Data sets Earth's surface Geographical information Geologic domains Global estimate Half-space Hotspots Hydrothermal circulation Oceanic crust Oceanic lithosphere Estimation Geographic information systems Geology Heat transfer He |
spellingShingle |
Keywords: Antarctica Data sets Earth's surface Geographical information Geologic domains Global estimate Half-space Hotspots Hydrothermal circulation Oceanic crust Oceanic lithosphere Estimation Geographic information systems Geology Heat transfer He Davies, J Davies, Rhodri Earth's surface heat flux |
topic_facet |
Keywords: Antarctica Data sets Earth's surface Geographical information Geologic domains Global estimate Half-space Hotspots Hydrothermal circulation Oceanic crust Oceanic lithosphere Estimation Geographic information systems Geology Heat transfer He |
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, J Davies, Rhodri |
author_facet |
Davies, J Davies, Rhodri |
author_sort |
Davies, J |
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 |
Copernicus GmbH |
url |
http://hdl.handle.net/1885/65286 https://openresearch-repository.anu.edu.au/bitstream/1885/65286/5/Davies_DR_2010_Earth%2527s_surface.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65286/7/01_Davies_Earth%27s_surface_heat_flux_2010.pdf.jpg |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Solid Earth |
op_relation |
1869-9510 http://hdl.handle.net/1885/65286 https://openresearch-repository.anu.edu.au/bitstream/1885/65286/5/Davies_DR_2010_Earth%2527s_surface.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/65286/7/01_Davies_Earth%27s_surface_heat_flux_2010.pdf.jpg |
_version_ |
1788067016689582080 |