Heat Flow, Arctic Ocean, 1965-2009

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Abstract/Contents

Abstract: This point shapefile contains heat flow data for Arctic Ocean compiled from sources dating from 1965 to 2009. Heat flow is a measure of heat loss across the surface of the Earth and is useful for modeling recent tectonic activity, transport of heat by groundwater, variations in concentrations of the radiogenic elements U, Th and K, glacial dynamics, and recent changes in climate. See attibute table and supplemental documentation for more detail.
Purpose: Global heat flow data are maintained by the International Heat Flow Commission (IHFC) of the International Association of Seismology and Physics of the Earth's Interior (IASPEI).

Type of resource	cartographic, software, multimedia
Form	Shapefile
Extent	0.033
Publisher	International Heat Flow Commission
Publication date	2016
Language	English
Digital origin	born digital
Map data	Scale not given. ; Custom projection W 165°50ʹ--E 174°44ʹ/N 89°36ʹ54ʺ--N 62°1ʹ53ʺ, Scale not given ; EPSG::4326

Creator	International Heat Flow Commission
Creator	International Association of Seismology and Physics of the Earth's Interior
Creator	Oklahoma State University. Department of Geography. Cartography Service

Subject	Terrestrial heat flow
Subject	Arctic Ocean
Subject	1965-2009
Subject	Climatology, Meteorology and Atmosphere
Genre	Geospatial data
Genre	Cartographic dataset

WGS84 Cartographics	This layer is presented in the WGS84 coordinate system for web display purposes. Downloadable data are provided in native coordinate system or projection.
Location	https://purl.stanford.edu/sj355jp0059

Use and reproduction: This item is in the public domain. There are no restrictions on use.
Copyright: This work is in the Public Domain, meaning that it is not subject to copyright.

Preferred citation: Heat Flow, Arctic Ocean, 1965-2009 (2016) .Global Heatflow database from the International Heat Flow Commission 2011. http://purl.stanford.edu/sj355jp0059

Global Heatflow database from the International Heat Flow Commission 2011

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