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An Improved Algorithm for Computing Altitude Dependent Corrected Geomagnetic Coordinates
An improved algorithm for computing altitude dependent corrected geomagnetic (CGM) coordinates from geocentric coordinates (and, where it exists, the inverse) using spherical harmonics is described. The method uses a tenth order spherical harmonic fit to the direction cosines (a unit vector) in a su...
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creator | Bhavnani, K. H Hein, C. A |
description | An improved algorithm for computing altitude dependent corrected geomagnetic (CGM) coordinates from geocentric coordinates (and, where it exists, the inverse) using spherical harmonics is described. The method uses a tenth order spherical harmonic fit to the direction cosines (a unit vector) in a suitably chosen intermediate, altitude adjusted coordinate system. The need for this auxiliary coordinate system is to avoid convergence problems associated with the discontinuity in the CGM latitude at the magnetic equator at non- zero altitude. Altitude dependence is obtained by computing the spherical harmonic fits to CGM (and inverse) at 0, 300 and 1200 km altitude, and using a quadratic fit to interpolate each coefficient. The new algorithm provides a good representation of the CGM compression around the South Atlantic Anomaly in addition to modeling the increasing discontinuity with altitude at the magnetic equator. Comparisons are provided with previous approaches. Accuracy limitations and consistency between the direct and inverse computations are also discussed. |
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A ; RADEX INC BEDFORD MA</creatorcontrib><description>An improved algorithm for computing altitude dependent corrected geomagnetic (CGM) coordinates from geocentric coordinates (and, where it exists, the inverse) using spherical harmonics is described. The method uses a tenth order spherical harmonic fit to the direction cosines (a unit vector) in a suitably chosen intermediate, altitude adjusted coordinate system. The need for this auxiliary coordinate system is to avoid convergence problems associated with the discontinuity in the CGM latitude at the magnetic equator at non- zero altitude. Altitude dependence is obtained by computing the spherical harmonic fits to CGM (and inverse) at 0, 300 and 1200 km altitude, and using a quadratic fit to interpolate each coefficient. The new algorithm provides a good representation of the CGM compression around the South Atlantic Anomaly in addition to modeling the increasing discontinuity with altitude at the magnetic equator. Comparisons are provided with previous approaches. Accuracy limitations and consistency between the direct and inverse computations are also discussed.</description><language>eng</language><subject>ACCURACY ; ALGORITHMS ; ALTITUDE ; ANOMALIES ; COEFFICIENTS ; COMPUTATIONS ; CONVERGENCE ; COORDINATES ; CORRECTED GEOMAGNETIC COORDINATES ; EARTH MODELS ; EQUATORIAL REGIONS ; Geodesy ; Geomagnetism ; GLOBAL ; GLOBAL COORDINATES ; GUSTAFSSON COORDINATES ; INVERSION ; LATITUDE ; LIMITATIONS ; MAPPING(TRANSFORMATIONS) ; PE62101F ; SOUTH ATLANTIC OCEAN ; SPHERICAL HARMONICS ; WUPL7659GYAA</subject><creationdate>1994</creationdate><rights>APPROVED FOR PUBLIC RELEASE</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,776,881,27546,27547</link.rule.ids><linktorsrc>$$Uhttps://apps.dtic.mil/sti/citations/ADA293967$$EView_record_in_DTIC$$FView_record_in_$$GDTIC$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Bhavnani, K. H</creatorcontrib><creatorcontrib>Hein, C. A</creatorcontrib><creatorcontrib>RADEX INC BEDFORD MA</creatorcontrib><title>An Improved Algorithm for Computing Altitude Dependent Corrected Geomagnetic Coordinates</title><description>An improved algorithm for computing altitude dependent corrected geomagnetic (CGM) coordinates from geocentric coordinates (and, where it exists, the inverse) using spherical harmonics is described. The method uses a tenth order spherical harmonic fit to the direction cosines (a unit vector) in a suitably chosen intermediate, altitude adjusted coordinate system. The need for this auxiliary coordinate system is to avoid convergence problems associated with the discontinuity in the CGM latitude at the magnetic equator at non- zero altitude. Altitude dependence is obtained by computing the spherical harmonic fits to CGM (and inverse) at 0, 300 and 1200 km altitude, and using a quadratic fit to interpolate each coefficient. The new algorithm provides a good representation of the CGM compression around the South Atlantic Anomaly in addition to modeling the increasing discontinuity with altitude at the magnetic equator. Comparisons are provided with previous approaches. Accuracy limitations and consistency between the direct and inverse computations are also discussed.</description><subject>ACCURACY</subject><subject>ALGORITHMS</subject><subject>ALTITUDE</subject><subject>ANOMALIES</subject><subject>COEFFICIENTS</subject><subject>COMPUTATIONS</subject><subject>CONVERGENCE</subject><subject>COORDINATES</subject><subject>CORRECTED GEOMAGNETIC COORDINATES</subject><subject>EARTH MODELS</subject><subject>EQUATORIAL REGIONS</subject><subject>Geodesy</subject><subject>Geomagnetism</subject><subject>GLOBAL</subject><subject>GLOBAL COORDINATES</subject><subject>GUSTAFSSON COORDINATES</subject><subject>INVERSION</subject><subject>LATITUDE</subject><subject>LIMITATIONS</subject><subject>MAPPING(TRANSFORMATIONS)</subject><subject>PE62101F</subject><subject>SOUTH ATLANTIC OCEAN</subject><subject>SPHERICAL HARMONICS</subject><subject>WUPL7659GYAA</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1994</creationdate><recordtype>report</recordtype><sourceid>1RU</sourceid><recordid>eNqFjDsOwjAQRN1QIOAGFL4ADZFAKa2EX09BF1nxxliKd631hvOzBT3VSO_NzNq8HNpHLkwfCNbNkTjJO9uJ2HaUyyIJo3JJsgSwPRTAACgqmWEUHd2Aso8IkkalxCGhF6hbs5r8XGH3y43ZXy_P7n4IWhyq_oIMrnfHtmlP5-aP_gJKRTeI</recordid><startdate>19941219</startdate><enddate>19941219</enddate><creator>Bhavnani, K. 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A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-dtic_stinet_ADA2939673</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1994</creationdate><topic>ACCURACY</topic><topic>ALGORITHMS</topic><topic>ALTITUDE</topic><topic>ANOMALIES</topic><topic>COEFFICIENTS</topic><topic>COMPUTATIONS</topic><topic>CONVERGENCE</topic><topic>COORDINATES</topic><topic>CORRECTED GEOMAGNETIC COORDINATES</topic><topic>EARTH MODELS</topic><topic>EQUATORIAL REGIONS</topic><topic>Geodesy</topic><topic>Geomagnetism</topic><topic>GLOBAL</topic><topic>GLOBAL COORDINATES</topic><topic>GUSTAFSSON COORDINATES</topic><topic>INVERSION</topic><topic>LATITUDE</topic><topic>LIMITATIONS</topic><topic>MAPPING(TRANSFORMATIONS)</topic><topic>PE62101F</topic><topic>SOUTH ATLANTIC OCEAN</topic><topic>SPHERICAL HARMONICS</topic><topic>WUPL7659GYAA</topic><toplevel>online_resources</toplevel><creatorcontrib>Bhavnani, K. H</creatorcontrib><creatorcontrib>Hein, C. A</creatorcontrib><creatorcontrib>RADEX INC BEDFORD MA</creatorcontrib><collection>DTIC Technical Reports</collection><collection>DTIC STINET</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Bhavnani, K. H</au><au>Hein, C. A</au><aucorp>RADEX INC BEDFORD MA</aucorp><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>An Improved Algorithm for Computing Altitude Dependent Corrected Geomagnetic Coordinates</btitle><date>1994-12-19</date><risdate>1994</risdate><abstract>An improved algorithm for computing altitude dependent corrected geomagnetic (CGM) coordinates from geocentric coordinates (and, where it exists, the inverse) using spherical harmonics is described. The method uses a tenth order spherical harmonic fit to the direction cosines (a unit vector) in a suitably chosen intermediate, altitude adjusted coordinate system. The need for this auxiliary coordinate system is to avoid convergence problems associated with the discontinuity in the CGM latitude at the magnetic equator at non- zero altitude. Altitude dependence is obtained by computing the spherical harmonic fits to CGM (and inverse) at 0, 300 and 1200 km altitude, and using a quadratic fit to interpolate each coefficient. The new algorithm provides a good representation of the CGM compression around the South Atlantic Anomaly in addition to modeling the increasing discontinuity with altitude at the magnetic equator. Comparisons are provided with previous approaches. Accuracy limitations and consistency between the direct and inverse computations are also discussed.</abstract><oa>free_for_read</oa></addata></record> |
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source | DTIC Technical Reports |
subjects | ACCURACY ALGORITHMS ALTITUDE ANOMALIES COEFFICIENTS COMPUTATIONS CONVERGENCE COORDINATES CORRECTED GEOMAGNETIC COORDINATES EARTH MODELS EQUATORIAL REGIONS Geodesy Geomagnetism GLOBAL GLOBAL COORDINATES GUSTAFSSON COORDINATES INVERSION LATITUDE LIMITATIONS MAPPING(TRANSFORMATIONS) PE62101F SOUTH ATLANTIC OCEAN SPHERICAL HARMONICS WUPL7659GYAA |
title | An Improved Algorithm for Computing Altitude Dependent Corrected Geomagnetic Coordinates |
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