Heat flow is calculated using Fourier’s Law, which states that the flux (heat flow) is equal to the thermal conductivity multiplied by the thermal gradient.
REQUIRED: The name of an organization or individual that developed the data set., REQUIRED: The date when the data set is published or otherwise made available for release., XYheat_flow.Online Links:
- \\DUKE\C\Documents and Settings\jyoburn\Desktop\Geodatabase\heat\XYheat_flow.shp
This is a Vector data set. It contains the following vector data types (SDTS terminology):
Horizontal positions are specified in geographic coordinates, that is, latitude and longitude. Latitudes are given to the nearest 0.000001. Longitudes are given to the nearest 0.000001. Latitude and longitude values are specified in Decimal degrees.
The horizontal datum used is North American Datum of 1927.
The ellipsoid used is Clarke 1866.
The semi-major axis of the ellipsoid used is 6378206.400000.
The flattening of the ellipsoid used is 1/294.978698.
Sequential unique whole numbers that are automatically generated.
Coordinates defining the features.
Data taken from: "A New Global Heat Flow Compilation"; Assembled by Henry N. Pollack, Suzanne J. Hurter, and Jeffrey R. Johnson; Department of Geological Sciences, The University of Michigan. Ann Arbor, Michigan 48109-1063, U.S.A. March, 1991
Jesse Yoburn
Arizona State University
jesse.yoburn@asu.edu
Part of the Geophysics aspect of the Geoinformatics Network project
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- Access_Constraints:
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Downloadable Data
| Data format: | Size: 0.922 |
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