STEVE-like phenomenon – May 1, 2026

This STEVE event on May 1, 2026 consisted of two distinct phases: an earlier 23:10 UTC exposure showing faint picket fence low above the treeline, followed by a later 23:15–23:16 UTC phase where STEVE appeared alone. The images below document both phases.

Phase 1 — 23:10 UTC (STEVE with faint picket fence)

STEVE observed near zenith with a clean mauve N₂⁺ emission profile. A small outward protrusion on the oval‑facing side of the band marks a localized shear‑flow irregularity within the SAID channel, providing a subtle but important signature that confirms the structure as part of the STEVE system. Note: In this 23:10 UTC exposure, faint picket fence structures are visible low above the treeline. These appear as narrow, vertically aligned pillars and were present only during this earlier phase of the event.

A narrow subauroral arc appeared over Follestaddalen around 23:10 UTC, following a clear separation from the auroral oval. The structure, timing, and behaviour were consistent with a STEVE‑like event. Although the characteristic mauve colour was difficult to see visually due to bright moonlight and a generally bright sky, the camera sequence revealed a narrow, uniform arc crossing directly through zenith.

The viewing geometry is important for interpreting the green structures beneath the arc. Because the STEVE arc passed overhead, the green, vertically structured band (“probable picket fence”) was seen directly from below. This foreshortens the vertical columns and causes them to appear broad, diffuse, and partially overlapping, rather than as the sharp, well‑separated spikes typically seen when picket fence is observed closer to the horizon. The sequence shows a faint but vertically modulated green band near the crossing point, consistent with a weak or developing picket‑fence structure.

This was a short‑lived late‑season event, lasting only a few minutes before fading into the brightening spring sky.

Summary of the May 1, 2026 STEVE Event

The event unfolded in two stages. At 23:10 UTC, a narrow SAID structure appeared above the treeline with faint picket‑fence elements. As the SAID band shifted slightly, the true STEVE arc — a thin mauve N₂⁺ line — became visible behind it, revealing the layered geometry of the system.
By 23:15–23:16 UTC, SAID had weakened into a diffuse green subauroral band, while STEVE remained as a narrow, isolated arc. No picket fence was present in this later phase.

A clean transition was observed:
23:10 — STEVE + faint PF + narrow SAID
23:15–23:16 — STEVE alone + diffuse green band

Please see the entire sequence below.

Image Sequence

Phase 2 — STEVE alone

The picket fence was visible only in the earlier 23:10 UTC exposure.
In this later phase (23:15–23:16), STEVE appears alone in the images; the green diffuse emission below the band is not picket fence.
The difference between the two frames may explain why some external pages interpreted the later image as containing picket fence.
The green diffuse emission below the STEVE band is not picket fence.
This is a weak subauroral green emission layer that often appears with STEVE, but is physically separate from the STEVE mechanism. However, the diffuse green band beneath STEVE is produced by the same particle‑injection process that creates picket fence, but it is not picket fence itself. When the injections are weak or continuous, the pillars disappear and the emission becomes a smooth green arc.

The green diffuse emission

The green diffuse emission below the STEVE band is not picket fence.
This is a weak subauroral green emission layer caused by low‑level particle precipitation north of the SAID/STEVE region.
It often appears together with STEVE in images, but it is physically separate from the STEVE mechanism and does not form vertical structures.

Phase summary

Phase 1 (23:10): Clear picket fence north of the STEVE region.
Phase 2 (23:15–23:16): STEVE without PF; weak green diffuse emission appears below the band at 23:16.

Color profile

Technical Note (23:10 UTC)
The color profile at 23:10 UTC captures the STEVE arc at its peak, when the mauve band was widest and most intense near zenith. The profile shows dominant N₂⁺ emission with minimal green contamination, consistent with a fully developed SAID channel during the brightest phase of the event. A faint mauve halo surrounds the central structure, reflecting strong N₂⁺ excitation in the core of the arc.
Technical Note (23:16 UTC)
Post‑peak profile showing dominant N₂⁺ emission as the SAID channel weakens. No 5577 Å contribution is present inside the mauve band.

Scientific summary

  • STEVE observed between 23:10–23:16 UTC
  • Faint picket fence present only at 23:10 UTC
  • No picket fence visible in the 23:15–23:16 UTC phase
  • Green diffuse emission present in both frames
  • Geometry consistent with low‑altitude subauroral structures

Equipment: Canon EOS 650D with an 8 mm fisheye lens, ISO 1600, and varying exposure times depending on sky brightness.

Blue auroral corona – 20 April

Blue‑tinged auroral corona observation
20 April 2026 — Ørsta, Norway

Time: 23:15–23:30 UTC (initial structured onset ~23:18 UTC)

Observation type: DSLR documentation of a partial auroral corona with blue‑violet lower emission.

Observer: Geir T. Birkeland Øye
Location: Ørsta, Norway

Instrument: Canon 650D, 8 mm fisheye, ISO 1600, short‑exposure sequence

Summary

A short‑exposure DSLR sequence recorded the development of a partial auroral corona directly overhead. The first structured rays appeared around 23:18 UTC, marking a brief local intensification during otherwise quiet geomagnetic conditions.

The lower part of the structure showed a blue‑violet tint, transitioning into green emission at higher altitudes. This colour impression is consistent with mixed auroral emissions and may include contributions from molecular nitrogen processes (N₂ / N₂⁺), although no spectroscopic data are available to confirm line dominance.

Auroral structure

The event formed a corona‑like pattern, with rays converging toward the zenith.
The geometry was not fully symmetric, and the corona did not develop into a stable, mature form.
Such partial or transient corona formations are well‑known during short‑lived intensifications.

Geomagnetic context

Global geomagnetic activity on 20 April 2026 was quiet to moderate (Kp 1–3).
However, regional Scandinavian magnetometer data show small, coincident disturbances during the observation window, consistent with a brief localised enhancement.

Short‑duration variations of this type are not always visible in 3‑hour Kp indices but can still produce brief auroral brightenings.

Geomagnetic data (TRO2A, local time)

TRO2A magnetometer data (local time). The disturbance at 01:20 CEST corresponds to 23:20 UTC and matches the timing of the observed intensification.

Geomagnetic signature (TRO2A magnetometer)

The small disturbance visible around 01:20 local time corresponds to 23:20 UTC on 20 April, matching the timing of the observed auroral intensification.

The H‑component shows a weak but clearly defined negative dip lasting a few minutes, while the D and Z components display synchronous minor variations. Such brief, low‑amplitude deviations are typical of localized auroral onset‑type intensifications and do not necessarily appear in the 3‑hour Kp index.

This signature supports the interpretation of a short‑lived auroral intensification with partial corona formation.

Source: Tromsø Geophysical Observatory (TRO2A)

The Solund (SOL1A) magnetometer shows weak but coincident variations around 23:20 UTC that correlate with the TRO2A negative dip. Although the SOL1A signal is smaller, the synchronous behaviour supports that the brief intensification observed in Ørsta was a real regional (localized) auroral enhancement rather than an instrumental anomaly.

Seasonal light conditions

At this time of year, the Sun remains only a few degrees below the horizon.
This twilight regime in the upper atmosphere can:

  • increase contrast between aurora and background sky
  • make faint emissions more visually apparent
  • influence colour balance in photographic recordings

It does not increase auroral emission strength itself.

Interpretation

The event is best described as a short‑lived auroral intensification with partial corona formation, displaying a visually enhanced blue‑violet lower region.
The colour impression likely reflects a combination of:

  • molecular nitrogen emissions
  • rapid temporal changes during onset
  • viewing geometry near zenith
  • seasonal twilight contrast

Norsk

Ein kort eksponeringssekvens viste ei delvis nordlyskrone rett over observatøren. Rundt 23:18 UTC oppstod ei kortvarig intensivering med blåleg/lilla innslag i nedre del av strukturen.

Den globale geomagnetiske aktiviteten var låg til moderat (Kp 1–3), men regionale magnetometerdata viser små samtidige variasjonar som kan forklare ei kort lokal forsterking.

Sesongmessig skumringslys i høg atmosfære kan gi betre kontrast og påverke fargeinntrykket, utan at sjølve emisjonen blir sterkare.

Hendinga blir tolka som ei kortvarig nordlysintensivering med delvis koronaformasjon, der fargeinntrykket kan vere påverka av nitrogenprosessar, rask utvikling og siktlinje nær zenit.

Corrected master version (cyan/blue reduction applied).

Additional reading

Article by Dr. Tony Phillips – Spaceweather.com

Article by Elisabetta Intini – Focus.it

Leo Triplet. April 15, 2026.

Three spiral galaxies — M65, M66, and NGC 3628 — captured in a single frame, revealing the graceful diversity of galactic forms across deep space.

Zwo Seestar S30.

NGC 7023 (Iris Nebula) — Reflection nebula in Cepheus, captured from Ørsta, Norway on April 15,  2026 using Seestar S30.

April 07-08,2026. Starlink Train, and a Bright Meteor.

On Monday, April 6 at 7:50 p.m. PT, Falcon 9 launched 25 Starlink satellites to low-Earth orbit from Space Launch Complex 4 East (SLC-4E) at Vandenberg Space Force Base in California. This corresponds to 04:50 CEST on April 7 in Norway. The Starlink train passed over Norway later that evening at 22:11, and the image above shows the formation as seen from Ørsta.

A colorful meteor streaking the sky in the morning hours of April 08, 2026.

Transient STEVE-like phenomenon. April 02, 2026.

Transient STEVE‑like emission – 2 April 2026

STEVE‑type subauroral emission

2 April 2026 — Ørsta, Norway

Time: 20:16–20:22 UTC
Observation type: DSLR documentation of a transient subauroral STEVE‑like emission
Observer: Geir T. Birkeland Øye
Location: Ørsta, Norway

Instrument: Canon 650D, 8 mm fisheye lens, high‑resolution short‑exposure sequence


Summary

A transient subauroral optical emission consistent with the STEVE (Strong Thermal Emission Velocity Enhancement) phenomenon was observed south of the auroral oval on 2 April 2026. The event began as a compact purple/magenta subauroral blob around 20:16 UTC, which rapidly elongated into a narrow, well‑defined east–west arc. The emission persisted for approximately six minutes before dissipating.

Throughout the entire sequence, the structure displayed a stable purple–magenta continuum with no green (557.7 nm) or red (630.0 nm) oxygen‑line auroral features, and no curtain‑like or rayed morphology. This spectral appearance is characteristic of STEVE, which is known to produce broadband continuum emission rather than discrete auroral lines.

The full evolution—from initial blob to mature arc and final fading—was captured in a time‑stamped DSLR sequence.


Optical and morphological characteristics

  • Initial localized subauroral blob with purple/magenta emission
  • Rapid transition into a narrow, east–west oriented arc
  • No picket‑fence structures, no rayed curtains, and no oxygen‑line signatures
  • Emission remained smooth, featureless, and continuum‑dominated
  • Arc located equatorward of the main auroral oval, consistent with subauroral ion drift regions

This morphology aligns with documented STEVE events associated with SAID/SAPS channels.


Geomagnetic and solar‑wind context

Solar wind conditions on 2 April were already disturbed due to preceding coronal mass ejections (CMEs). Such conditions are favourable for the formation of subauroral ion drift channels, which can generate STEVE‑type emissions.

Key contextual points:

  • Disturbed solar wind from earlier CMEs
  • Enhanced geomagnetic activity at subauroral latitudes
  • Conditions supportive of fast, localized ionospheric flow channels
  • STEVE events are commonly short‑lived under such transient SAID/SAPS regimes

The brief duration (6 minutes) is fully consistent with known STEVE behaviour.


Interpretation

The event is best classified as a STEVE‑type subauroral emission, based on:

  • Subauroral location
  • Purple/magenta continuum emission
  • Absence of discrete auroral lines
  • Rapid blob‑to‑arc evolution
  • Occurrence during disturbed geomagnetic conditions

The high‑resolution, time‑stamped imagery provides a complete record of the event, including the rarely documented initial blob phase, making this a scientifically valuable observation.


Norsk

STEVE‑liknande subauroral emisjon – 2. april 2026

Ei kortvarig subauroral lysfenomen vart observert sør for nordlysovaen i Ørsta mellom 20:16 og 20:22 UTC. Hendinga starta som ein kompakt lilla/magenta “blob”, som raskt strekte seg ut til ein tydeleg aust–vest‑gåande STEVE‑struktur.

Emisjonen hadde gjennom heile forløpet ein jamn lilla/magenta kontinuerleg spektral karakter, utan grøne eller raude oksygenliner og utan gardin‑ eller strålestrukturar. Dette er typisk for STEVE, som ikkje er eit tradisjonelt nordlys, men eit optisk uttrykk for raske subaurorale ionedriftar (SAID/SAPS).

Solvindforholda var forstyrra av tidlegare CME‑ar, noko som gav gode vilkår for slike fenomen. Den korte varigheita er i tråd med kjende STEVE‑observasjonar.

Hendinga er klassifisert som ei STEVE‑type subauroral emisjon, og bileta dokumenterer heile utviklinga frå første blob til bortfall.

CME – Aurora Borealis,-untypical STEVE. March 20-21, 2026.

Nice auroral activity in between the clouds, wind and precipitation. A faint but distinct pink STEVE structure appeared in the eastern sky during an intense auroral outbreak after a CME impact. It was visible only from 22:08 to 22:11 before clouds returned. The images show a clear mauve/pink hue distinct from the surrounding green and violet aurora. This represents an atypical but confirmed STEVE variant. A few images. Details: Canon 650D/RP, fisheye lenses. Various iso and exposure settings. Location: Ørsta, Norway.

CIR impact. A nice auroral display. February 14-15, 2026.

During the CIR-impact on February 14-15, 2026, there was an instance of what looked like RAGDA to the south. A few images from local time 22:31 to 22:36 (or 21:31 to 21:36 UTC, if you wish). Following the RAGDA phenomenon a SAR-arc appeared, it lingered on, here photographed at local time 23:00 (UTC 22:00).

Details: Canon 650D, fisheye lens.


RAGDA


SAR-arc