Package com.luciad.tea
Class TLcdCoverageAltitudeMode
java.lang.Object
com.luciad.tea.TLcdCoverageAltitudeMode
Enumeration to indicate how coverage computation results should be interpreted.
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Field Summary
Modifier and TypeFieldDescriptionstatic final TLcdCoverageAltitudeMode
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference ellipsoid.static final TLcdCoverageAltitudeMode
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference geoid.static final TLcdCoverageAltitudeMode
Constant indicating that the resulting altitudes should be interpreted as heights above a reference terrain.static final TLcdCoverageAltitudeMode
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference object.static final TLcdCoverageAltitudeMode
Deprecated. -
Method Summary
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Field Details
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ABOVE_GROUND_LEVEL
Constant indicating that the resulting altitudes should be interpreted as heights above a reference terrain. Usually the terrain is defined by an implementation ofALcdTerrainElevationProvider
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ABOVE_OBJECT
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference object. This mode can be used to initialize a line-of-sight coverage or a point-to-point coverage. -
ABOVE_ELLIPSOID
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference ellipsoid. This mode can be used to initialize a line-of-sight coverage or a point-to-point coverage. -
ABOVE_GEOID
Constant indicating that the resulting altitudes should be interpreted as heights relative to a reference geoid. This mode can be used to initialize a line-of-sight coverage or a point-to-point coverage. -
AMSL
Deprecated.Use the equivalent nameABOVE_GEOID
, which is a more accurate description.Constant indicating that the resulting altitudes should be interpreted as heights above mean sea level. In practice, it is taken to be equivalent toABOVE_GEOID
, although the average mean sea level can differ from the geoid, due to currents, prevailing winds, and varying salinity.
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Method Details
ABOVE_GEOID
, which is a more accurate description.