DATA_SET_DESCRIPTION |
Data Set Overview
=================
Global Topographic Data Record (GTDR). The range to surface is
derived by fitting altimeter echoes from the fan-beam altimetry
antenna as a function of time to Hagfors' radar backscatter
model templates. The ranges are subtracted from the spacecraft
radial coordinate (derived from Doppler tracking), yielding
measurements of planetary radius. The data are filtered to
remove low-frequency errors in the in-plane elements of each
spacecraft orbit, and then re-sampled into sinusoidal,
Mercator, and north and south polar stereographic projections
at a resolution of about 5x5 kilometers per pixel.
A fifth image contains estimates of the absolute accuracy of
the radius values in each pixel of the sinusoidal projection.
This is derived by taking the root mean square of (a) the
statistical accuracy anticipated from the template fitting and
(b) the systematic errors estimated from the in-plane element
filtration. Note that this is the absolute topographic
accuracy -- relative errors are much smaller, about 10-15
meters in relatively flat areas.
Except in the radius error image, each GTDR pixel is
represented by a 16-bit integer. In sinusoidal images, pixels
lying outside the domain of the projection are set to zero. In
all images, pixels with unknown or unmeasured values are also
set to zero. The remaining values are related to the planetary
radius by the following equation:
DN = (RADIUS ) - 6039999.
In the radius error image, each pixel is represented by an
8-bit integer. Pixels lying outside the domain of the
projection are set to zero, as are all pixels with unknown or
unmeasured values. The remaining values are related to the
radius error by the following equation:
DN = (RADIUS-ERROR * 0.2) + 1.
See: Software Interface Specification Document (Peter G.
Ford, 1991, Global Altimetry and Radiometry Data
Records, MIT-MGN-GxDR SIS Version 2.3, 40 p.) that
is included on the GxDR CD-ROMs.
Note: There exist photoproducts that are identified as GxDRP
(where x is E (Emissivity), S (Slope), RE (Reflectivity),
or T (Topography)) however, they are not generated from
the digital GxDR products. They are instead produced
from the Magellan ARCDR (Altimetry and Radiometry
Composite Data Record) data files.
Processing Level Id : 5
Software Flag : N
Processing Start Time : 1991-06-24T20:11:00.000
Processing Stop Time : 1992-12-04T00:55:49.000
Parameters
==========
Data Set Parameter 'PLANETARY RADIUS'
-------------------------------------
Radial distance from center of planet or satellite to given
location on the surface.
Data Set Parameter Name : PLANETARY RADIUS
Data Set Parameter Unit : METER
Sampling Parameter Name : PIXEL
Sampling Parameter Unit : METER
Minimum Sampling Parameter : N/A
Maximum Sampling Parameter : N/A
Sampling Parameter Resolution : 9282
Sampling Parameter Interval : 4641
Minimum Available Sampling Int : N/A
Noise Level : UNK
Source Instrument Parameters
============================
Instrument Host ID : MGN
Data Set Parameter Name : PLANETARY RADIUS
Instrument Parameter Name : RADAR ECHO POWER
Important Instrument Parameters : 1
Processing
==========
Processing History
------------------
Source Data Set ID : MGN-V-RDRS-5-CDR-ALT/RAD-V1.0
Software : MGMMAP
Product Data Set ID : MGN-V-RDRS-5-GDR-TOPOGRAPHIC-V1.0
Software 'MGMMAP'
-----------------
The MIT Altimetry and Radiometry Mapping Software (MGMMAP)
reads Altimetry and Radiometry Composite Data Records
(ARCDRs), and generates an image of a specified data field i
a specified map projection. Each footprint datum is added
with a weight and horizontal extent proportional to the
appropriate ARCDR elements. This software will be released t
Magellan Data Management Archive Team (DMAT) upon the
completion of the nominal mission.
Software Name : MGMMAP
Software Type : N/A
Software Release Date : N/A
Node ID : N/A
Cognizant Engineer : DR. PETER G. FORD
Software Access Description : N/A
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