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	<title>Geomagnetic Indices Kp Dst - Revision history</title>
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	<updated>2026-05-12T11:20:43Z</updated>
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		<id>https://wiki.fusiongirl.app:443/index.php?title=Geomagnetic_Indices_Kp_Dst&amp;diff=7009&amp;oldid=prev</id>
		<title>JonoThora: Psionics expansion (01a + 01b): content authored / LaTeX-restored per local submodule; lint-clean.</title>
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		<updated>2026-05-11T20:48:49Z</updated>

		<summary type="html">&lt;p&gt;Psionics expansion (01a + 01b): content authored / LaTeX-restored per local submodule; lint-clean.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{Audience_Sidebar&lt;br /&gt;
| difficulty   = Intermediate&lt;br /&gt;
| reading_time = 5 minutes&lt;br /&gt;
| prerequisites = [[Psionics_Primer]]; [[Geomagnetic_Field]]; basic statistics.&lt;br /&gt;
| if_too_advanced_see = [[Geomagnetic_Field]]&lt;br /&gt;
| if_you_want_the_math_see = [[Geomagnetic_Indices_Kp_Dst]]&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
== Summary ==&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;Geomagnetic indices&amp;#039;&amp;#039;&amp;#039; are scalar summary measures of geomagnetic activity derived from worldwide magnetometer-station data. The principal indices in routine use:&lt;br /&gt;
&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Kp&amp;#039;&amp;#039;&amp;#039; — global quasi-logarithmic 3-hour index (range 0 to 9, in thirds), introduced by Julius Bartels in 1949.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Dst&amp;#039;&amp;#039;&amp;#039; — disturbance storm-time index (in nT), introduced by Masahisa Sugiura in 1964, measuring ring-current contribution to surface field at low latitudes.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;AE&amp;#039;&amp;#039;&amp;#039; — auroral electrojet index, measuring auroral-zone activity.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;ap&amp;#039;&amp;#039;&amp;#039; — linear 3-hour index derived from Kp.&lt;br /&gt;
&lt;br /&gt;
These indices are the standard quantitative descriptors of [[Space_Weather|space-weather]] conditions and are continuously published by international geophysics centres.&lt;br /&gt;
&lt;br /&gt;
== Kp Index ==&lt;br /&gt;
&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Kp index&amp;#039;&amp;#039;&amp;#039; (Bartels 1949):&lt;br /&gt;
&lt;br /&gt;
* Derived from K-indices at 13 mid-latitude magnetometer stations.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Quasi-logarithmic scale&amp;#039;&amp;#039;&amp;#039;: Kp = 0 corresponds to extremely quiet conditions; Kp = 9 corresponds to extreme storm.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Subscript notation&amp;#039;&amp;#039;&amp;#039; (0-, 0, 0+, 1-, 1, 1+, ...) gives finer 28-step granularity.&lt;br /&gt;
* Updated every 3 hours; provisional values available within hours, final values within weeks.&lt;br /&gt;
&lt;br /&gt;
NOAA / GFZ Potsdam publishes the official series. Kp ≥ 5 is the threshold for a &amp;quot;geomagnetic storm&amp;quot; classification.&lt;br /&gt;
&lt;br /&gt;
== Dst Index ==&lt;br /&gt;
&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Dst index&amp;#039;&amp;#039;&amp;#039; (Sugiura 1964):&lt;br /&gt;
&lt;br /&gt;
* Derived from 4 low-latitude magnetometer stations (Honolulu, San Juan, Hermanus, Kakioka).&lt;br /&gt;
* Measures the &amp;#039;&amp;#039;&amp;#039;horizontal-component depression of the geomagnetic field&amp;#039;&amp;#039;&amp;#039; caused by the storm-time &amp;#039;&amp;#039;&amp;#039;ring current&amp;#039;&amp;#039;&amp;#039; (current of magnetospheric ions encircling the Earth).&lt;br /&gt;
* Linear scale in nT; negative values indicate field depression.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Storm classification&amp;#039;&amp;#039;&amp;#039;: moderate storm Dst &amp;lt; -50 nT; intense storm Dst &amp;lt; -100 nT; great storm Dst &amp;lt; -250 nT.&lt;br /&gt;
* Updated hourly.&lt;br /&gt;
&lt;br /&gt;
The Halloween 2003 storms produced Dst ≈ -422 nT (intense); the 1989 Quebec storm Dst ≈ -589 nT. The 1859 Carrington event is estimated at Dst ~ -1700 nT (extrapolated from auroral observations).&lt;br /&gt;
&lt;br /&gt;
== AE Index ==&lt;br /&gt;
&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;AE index&amp;#039;&amp;#039;&amp;#039; (auroral electrojet) measures auroral-zone disturbance, derived from magnetometer stations within the auroral oval. Used principally for substorm research rather than general storm characterisation.&lt;br /&gt;
&lt;br /&gt;
== Operational Use ==&lt;br /&gt;
&lt;br /&gt;
These indices are the principal inputs to:&lt;br /&gt;
&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Power-grid management&amp;#039;&amp;#039;&amp;#039; — high Kp / large Dst correlates with geomagnetically-induced-current risk to long-distance transmission lines.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Satellite-operation forecasting&amp;#039;&amp;#039;&amp;#039; — storms increase orbital drag on LEO satellites and increase single-event-upset rates on all spacecraft.&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Radio-propagation forecasting&amp;#039;&amp;#039;&amp;#039; — HF radio communications are degraded during ionospheric storms.&lt;br /&gt;
&lt;br /&gt;
== Significance for Psionic Research ==&lt;br /&gt;
&lt;br /&gt;
Geomagnetic indices are the principal &amp;#039;&amp;#039;&amp;#039;operationalised environmental variable&amp;#039;&amp;#039;&amp;#039; for the kind of EM-environment-dependence predictions made by the [[Psionics|psionic framework]]. Multiple independent research programmes have published correlations between Kp / Dst and:&lt;br /&gt;
&lt;br /&gt;
* Reports of anomalous experiences ([[Michael_Persinger|Persinger]]).&lt;br /&gt;
* Random-event-generator deviations ([[Global_Consciousness_Project|GCP]]).&lt;br /&gt;
* Hospital admissions, accident rates (mainstream epidemiology).&lt;br /&gt;
&lt;br /&gt;
Within the framework, the indices provide a quantitative window into the strength of the environmental EM substrate that ψ-field coupling is predicted to modulate.&lt;br /&gt;
&lt;br /&gt;
== See Also ==&lt;br /&gt;
&lt;br /&gt;
* [[Geomagnetic_Field]]&lt;br /&gt;
* [[Space_Weather]]&lt;br /&gt;
* [[Solar_Cycles]]&lt;br /&gt;
* [[Michael_Persinger]]&lt;br /&gt;
* [[Global_Consciousness_Project]]&lt;br /&gt;
&lt;br /&gt;
== External Links ==&lt;br /&gt;
&lt;br /&gt;
* Wikipedia: K-index, Disturbance storm-time index&lt;br /&gt;
* NOAA Space Weather Prediction Center: real-time Kp / Dst.&lt;br /&gt;
* GFZ Potsdam: Kp definitive series.&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
&lt;br /&gt;
* Bartels, J. (1949). &amp;quot;The standardized index, Ks, and the planetary index, Kp.&amp;quot; &amp;#039;&amp;#039;IATME Bulletin&amp;#039;&amp;#039; 12b: 97-120.&lt;br /&gt;
* Sugiura, M. (1964). &amp;quot;Hourly values of equatorial Dst for the IGY.&amp;quot; &amp;#039;&amp;#039;Annals of the International Geophysical Year&amp;#039;&amp;#039; 35: 9-45.&lt;br /&gt;
* Mayaud, P. N. (1980). &amp;#039;&amp;#039;Derivation, Meaning, and Use of Geomagnetic Indices.&amp;#039;&amp;#039; AGU Geophysical Monograph 22.&lt;br /&gt;
&lt;br /&gt;
[[Category:Psionics]]&lt;br /&gt;
[[Category:Environmental EM]]&lt;br /&gt;
[[Category:Space Weather]]&lt;/div&gt;</summary>
		<author><name>JonoThora</name></author>
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