The field guide · Earth

Where is Schumann resonance measured?

Schumann resonance is measured at specialized ground stations using electric-field sensors and magnetic induction coils. Documented sites span several continents. A research station, a public chart and a continuously available live feed are three different things.

World map with 21 published ELF research locations across North America, South America, Europe, Asia, New Zealand and Antarctica; a Europe inset separates nearby sites. All names and coordinates are listed in the article.Open figure at full size ↗
Schumann Pulse map · Natural Earth public-domain land geometry. Equirectangular projection; selected published locations, not a census, live-feed guarantee or sensor-precision survey. Station-specific coordinate sources are listed below.

What the station map includes

The map brings together 18 sites used in a 2023 multi-station Schumann resonance study, plus documented locations at Nagycenk, Sierra Nevada and Syowa / West Ongul. It covers sites in the Americas, Europe, Asia, New Zealand and Antarctica. The 18-site paper analysed a January 2019 interval; appearing in that study does not establish a station's operating status in 2026.

Coordinates reproduce the cited research or institutional records. They are not a survey of individual antenna positions, and a research receiver may be away from a main observatory building. In particular, the West Ongul ELF site is separate from the main Syowa station on East Ongul. The labels SNV and SYO are short map identifiers here, not claims of official network codes.

Tomsk remains in the directory below. Its public monitor documents the city, but this review did not establish precise sensor coordinates from a suitable source, so no guessed station pin is added.

Names and coordinates on the map

Latitude is positive north; longitude is positive east. Published coordinate precision varies. The map and this table are generated from the same source registry.

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Site · map label Region Latitude / longitude Coordinate source
Alberta · ALB Canada 51.89°, -111.47° Bozóki et al. 2023, Table 1
Bharati · BRT Antarctica -69.41°, 76.19° Bozóki et al. 2023, Table 1
Boulder Creek · BOU United States 37.19°, -122.12° Bozóki et al. 2023, Table 1
Eskdalemuir · ESK United Kingdom 55.29°, -3.17° Bozóki et al. 2023, Table 1
Fort Churchill · FCHU Canada 58.76°, -94.08° Bozóki et al. 2023, Table 1
Hofuf · HOF Saudi Arabia 25.94°, 48.95° Bozóki et al. 2023, Table 1
Hornsund · HRN Svalbard, Norway 77.00°, 15.60° Bozóki et al. 2023, Table 1
Hugo · HUG United States 38.89°, -103.40° Bozóki et al. 2023, Table 1
Hylaty · HYL Poland 49.19°, 22.55° Bozóki et al. 2023, Table 1
Kevo · KEV Finland 69.75°, 27.02° Bozóki et al. 2023, Table 1
Kilpisjärvi · KIL Finland 69.05°, 20.79° Bozóki et al. 2023, Table 1
Ministik Lake · MSTK Canada 53.35°, -112.97° Bozóki et al. 2023, Table 1
Mondy · MND Russia 51.60°, 100.90° Bozóki et al. 2023, Table 1
Northland · NOR New Zealand -35.11°, 173.49° Bozóki et al. 2023, Table 1
Patagonia · PAT Argentina -51.59°, -69.32° Bozóki et al. 2023, Table 1
Shillong · SHI India 25.60°, 91.90° Bozóki et al. 2023, Table 1
Sodankylä · SOD Finland 67.43°, 26.39° Bozóki et al. 2023, Table 1
Vernadsky · VRN Antarctica (Ukraine) -65.25°, -64.25° Bozóki et al. 2023, Table 1
Nagycenk · NCK Hungary 47.63°, 16.72° Observatory coordinates
Sierra Nevada · SNV Spain 37.03°, -3.32° UGR dataset record
Syowa / West Ongul · SYO Antarctica (Japan) -69.02°, 39.51° MEXT observation programme, ELF site

Selected stations and data access

The entries below identify documented measurements and their institutional or research sources. This is a selected directory, not a complete census or an uptime monitor. A linked station description establishes research provenance; it does not certify that a current public feed is online today.

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Station or research location Region Documented work and access context
Hylaty Poland Jagiellonian University ELF station in the Bieszczady Mountains. Instrumentation and an older quick-look archive are public; archive access is not proof of current data.
Nagycenk / Széchenyi István Geophysical Observatory Hungary Electric and magnetic ELF observations. The observatory and display documentation explain the spectral and mode-parameter products.
Eskdalemuir United Kingdom The British Geological Survey documents induction-coil measurements and resonance research. Research description; current feed availability is not verified here.
Sierra Nevada Spain University research using ground magnetometers is documented in a four-year observational study. This is a research record, not a live dashboard.
Hugo, Colorado United States An ELF station described by Jagiellonian University’s WERA project. Current public stream availability is not asserted.
Patagonia, Río Gallegos Argentina The AGH University WERA account documents its 2016 installation as part of the array.
Syowa / West Ongul Antarctica Japan’s National Institute of Polar Research metadata documents search-coil observations of resonance-band signals. Data access follows the listed research contacts and archives.
Tomsk Russia Space Observing System 70 publishes a Tomsk sonogram and measurement notes. The public page was accessible during review; check the plot’s own date and time before treating it as current.

Why the station location matters

A globally excited phenomenon is still measured locally. The instrument responds to particular field components at its own position. Nearby electrical equipment can add interference, and different lightning centers contribute differently to a station’s record.

Hylaty’s institutional description is especially useful: it explains the choice of a quiet site away from the power grid. That detail helps explain why a phone, a generic weather station or a bright social-media chart is not equivalent to a dedicated ELF observatory.

Two branches, magnetic induction coils and an electric-field antenna, feed recording and calibration before spectrum or time-frequency analysis.Open figure at full size ↗
Schumann Pulse original measurement-chain schematic, based on the cited Hylaty/WERA and Nagycenk instrument descriptions. Real stations differ; not every station records both field types.

The instrument guide follows both magnetic and electric measurements from sensors through calibration to a spectrum. A map identifies places; it does not make every instrument or display directly comparable.

Why two graphs may disagree

Before calling two plots contradictory, compare their field component, units, frequency range, time zone, averaging window and color limits. One may show a magnetic spectrum, another an electric-field amplitude, and a third a derived index. The numbers do not become comparable just because every chart says “Schumann.”

A multi-station study can ask questions a single screenshot cannot. It can examine whether a feature appears in more than one record and whether differences fit the stations’ positions and instruments. That is a research workflow, not an invitation to average unrelated display values.

The additional mapped sites include Finland's pulsation-magnetometer stations, Canadian sites and Vernadsky in Antarctica. Their inclusion records their use in the cited research. It does not endorse every claim or product associated with an operator.

How to use and credit station data

Public access does not automatically authorize republication. Hylaty’s quick-look archive states conditions for scientific and educational use and asks other users to contact the group. Follow each provider’s terms; preserve the station, original timestamp and scale when quoting a result.

This directory links to sources instead of copying their live plots. Our learning figures are independently authored and labelled. For interpreting a downloaded chart, continue to the chart-reading guide.

Sources

The institutional and paper links in each directory row support that entry. Review date: 21 October 2026. Availability statements above describe this review, not continuous monitoring.

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