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		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?action=history&amp;feed=atom&amp;title=International_Geomagnetic_Reference_Field_%28IGRF%29</id>
		<title>International Geomagnetic Reference Field (IGRF) - Revision history</title>
		<link rel="self" type="application/atom+xml" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?action=history&amp;feed=atom&amp;title=International_Geomagnetic_Reference_Field_%28IGRF%29"/>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;action=history"/>
		<updated>2026-09-30T08:53:59Z</updated>
		<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1319&amp;oldid=prev</id>
		<title>Yash at 10:51, 23 February 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1319&amp;oldid=prev"/>
				<updated>2018-02-23T10:51:29Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 10:51, 23 February 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. [http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm HOW?]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. [http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm HOW?]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:EMF.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:EMF.png|frame|center&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;|Earth's magnetic field. Image reproduced from [https://commons.wikimedia.org/wiki/File:Earth%27s_magnetic_field,_schematic.svg here]&lt;/ins&gt;]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1006&amp;oldid=prev</id>
		<title>Yash at 02:17, 8 February 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1006&amp;oldid=prev"/>
				<updated>2018-02-08T02:17:54Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 02:17, 8 February 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l3&quot; &gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt; The difference between WMM and IGRF&amp;lt;ref&amp;gt;https://www.ngdc.noaa.gov/geomag/faqgeom.shtml#What_is_the_difference_between_IGRF_and_WMM_models&amp;lt;/ref&amp;gt; is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt; The difference between WMM and IGRF&amp;lt;ref&amp;gt;https://www.ngdc.noaa.gov/geomag/faqgeom.shtml#What_is_the_difference_between_IGRF_and_WMM_models&amp;lt;/ref&amp;gt; is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot;&gt;&amp;#160;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;----&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1005&amp;oldid=prev</id>
		<title>Yash at 02:17, 8 February 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1005&amp;oldid=prev"/>
				<updated>2018-02-08T02:17:32Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 02:17, 8 February 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l3&quot; &gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt;The difference between WMM and IGRF&amp;lt;ref&amp;gt;https://www.ngdc.noaa.gov/geomag/faqgeom.shtml#What_is_the_difference_between_IGRF_and_WMM_models&amp;lt;/ref&amp;gt; is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt; The difference between WMM and IGRF&amp;lt;ref&amp;gt;https://www.ngdc.noaa.gov/geomag/faqgeom.shtml#What_is_the_difference_between_IGRF_and_WMM_models&amp;lt;/ref&amp;gt; is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1004&amp;oldid=prev</id>
		<title>Yash at 02:17, 8 February 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=1004&amp;oldid=prev"/>
				<updated>2018-02-08T02:17:11Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 02:17, 8 February 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. [http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm HOW?]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. [http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm HOW?]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;MagneticField&lt;/del&gt;.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;EMF&lt;/ins&gt;.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt;The difference between WMM and IGRF &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[12] &lt;/del&gt;is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;&amp;#160; https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt;The difference between WMM and IGRF&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;ref&amp;gt;https://www.ngdc.noaa.gov/geomag/faqgeom.shtml#What_is_the_difference_between_IGRF_and_WMM_models&amp;lt;/ref&amp;gt; &lt;/ins&gt;is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== References ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=383&amp;oldid=prev</id>
		<title>Yash at 22:51, 24 January 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=383&amp;oldid=prev"/>
				<updated>2018-01-24T22:51:03Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 22:51, 24 January 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;HOW?&amp;lt;ref&amp;gt;&lt;/del&gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;&amp;lt;\ref&amp;gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[&lt;/ins&gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;HOW?]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=382&amp;oldid=prev</id>
		<title>Yash at 22:50, 24 January 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=382&amp;oldid=prev"/>
				<updated>2018-01-24T22:50:33Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr style=&quot;vertical-align: top;&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 22:50, 24 January 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;(&lt;/del&gt;HOW?&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;)&lt;/del&gt;&amp;lt;ref&amp;gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&amp;lt;\ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. HOW?&amp;lt;ref&amp;gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&amp;lt;\ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;

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&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=381&amp;oldid=prev</id>
		<title>Yash at 22:50, 24 January 2018</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=381&amp;oldid=prev"/>
				<updated>2018-01-24T22:50:13Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class=&quot;diff diff-contentalign-left&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: white; color:black; text-align: center;&quot;&gt;Revision as of 22:50, 24 January 2018&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot; &gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. (HOW? &amp;lt;ref&amp;gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&amp;lt;\ref&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;)&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;color:black; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. (HOW?&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;)&lt;/ins&gt;&amp;lt;ref&amp;gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&amp;lt;\ref&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:MagneticField.png|frame|center]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;&amp;#160;&lt;/td&gt;&lt;td style=&quot;background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Yash</name></author>	</entry>

	<entry>
		<id>https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=380&amp;oldid=prev</id>
		<title>Yash: Created page with &quot;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing cont...&quot;</title>
		<link rel="alternate" type="text/html" href="https://www.aero.iitb.ac.in/satelliteWiki/index.php?title=International_Geomagnetic_Reference_Field_(IGRF)&amp;diff=380&amp;oldid=prev"/>
				<updated>2018-01-24T22:49:49Z</updated>
		
		<summary type="html">&lt;p&gt;Created page with &amp;quot;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing cont...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;Earth has its own magnet which is about tilted by about 11 degrees from the axis passing through the north and south poles. It is made of molten metals and it is changing continuously but slowly that’s why IGRF model is updated in every five years. IGRF model is created by International Association of Geomagnetism and Aeronomy (IAGA using satellites and some observatories. The cool fact about the Earth’s magnetic field is that because of it, we are alive. Yeah! This shield blocks the dangerous cosmic radiation (energetic protons) coming from the Sun. (HOW? &amp;lt;ref&amp;gt;http://ctaps.yu.edu.jo/physics/Courses/Phys102/Phys102_Web_Resources/Mag_field.htm&amp;lt;\ref&amp;gt;)&lt;br /&gt;
[[File:MagneticField.png|frame|center]]&lt;br /&gt;
The IGRF model provides magnetic field vector in NED (North East Down) frame at any given latitude, longitude and altitude. &amp;lt;br \&amp;gt;&lt;br /&gt;
Position of the satellite can be taken from the propagator model and fed into the IGRF model (appropriate conversion is required from ECI to NED frame) and the IGRF model will give magnetic field vector. Magnetic field vector is important for magnetometer sensor and magneto-torquer actuator. &amp;lt;br \&amp;gt;&lt;br /&gt;
Other than IGRF, there are some other models such as World Magnetic Model (WMM).&amp;lt;ref&amp;gt;  https://www.ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml.&amp;lt;/ref&amp;gt;The difference between WMM and IGRF [12] is that WMM is valid for less number of years but more accurate as it is produced by dedicated agencies like NCEI and BGS for US and UK defense purposes.&amp;lt;br \&amp;gt; &amp;lt;br \&amp;gt;&lt;br /&gt;
If you are done reading this page, you can go back to [[Attitude Determination and Control Subsystem]].&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;/div&gt;</summary>
		<author><name>Yash</name></author>	</entry>

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