IAGA Magnetic Repeat Station Survey – Condensed Notes
Key Terminology
- Repeat station: fixed ground mark where absolute vector observations are made at a standard height.
- Normal field: main + static crustal field after removing external contributions.
- DIM: Declination–Inclination magnetometer (fluxgate-theodolite).
- PPM: Proton precession (or Overhauser) magnetometer for F.
- Variometer: 3-axis fluxgate (records X,Y,Z or D,H,Z continuously).
- Survey classes
• V – local variometer • M – reference observatory • A – absolutes only
• 1 = full correction; 2 = approx. correction; 3 = spot values.
Accuracy Targets
- Observatory standard: ≤1nT (intensity), ≤0.1′ (direction).
- Practical repeat-station goal: ≈5nT or 1′ D, 0.5′ I.
- Crucial to correct transient fields; more valuable to have few high-quality stations than many poor ones.
Network Design
- Spacing ≈200km (core SV resolves >400km).
- Reoccupation interval:
• Charts only → 5 yr; • SV modelling → 2 yr; • Jerks/high SV → 1 yr. - Use primary + secondary marks (≥200 m apart) to guard against loss/contamination.
Site Selection
- Low field gradients (<50 nT / 10 m).
- Away from magnetic noise (DC rail, power, transmitters).
- Secure, accessible, long-term permanence.
- Provide ≥4 azimuth marks; verify each visit.
Station Construction
- Pillar or ground slab with tripod sockets; record standard instrument height.
- Mark auxiliary F point 5–10 m away.
- Document: coordinates, photos, gradient map, reference-mark diagram.
Instrument Suite
- DIM on non-magnetic theodolite (Zeiss 020B/010B). Align fluxgate; verify offset.
- PPM: set frequencies to 26751.525581×104rad T−1s−1; compare to standard; keep sensor orientation fixed.
- 3-axis variometer: insulate/bury sensor; log 1-min means; determine scale & dE/dT.
Field Procedure (1st-order, on-site variometer)
- Install variometer, level, orient, start clock.
- Verify station & gradients; check reference-mark angles.
- Determine azimuth: preferred Sun hour-angle method; gyro or differential GPS if cloudy.
- Absolute sets (typ. FDI∣I∣DF) early a.m. & late p.m.; aim for night runs; simultaneous F at auxiliary.
- Occupy ≥2 days to tie baselines; repeat on secondary mark for check.
Data Reduction
Using Reference Observatory
E=E<em>o+[E(t)−E</em>o(t)]+(SV−SVo)ΔT
- Assumes identical transients; best when station–obs < few 100 km and mid-year occupation.
Using Local Variometer
- Derive baselines from absolutes; correct minute data → hourly → night quiet means.
- Apply observatory long-term record to offset residual night displacement.
- Compensate temperature drift: fit E<em>bl=a+b(T−T</em>0).
Error Sources
- Instrument: DIM 20′′, ±0.5 nT PPM.
- Mis-centering: error =∇F×δr; control to cm level.
- Observatory mismatch; crustal induction (can vary over <10 km).
- Non-uniform SV when reducing to annual mean.
Special Regions
- Equatorial electrojet (±3° dip): daytime H spikes >100 nT; use stations at same geomag-lat or local variometer; observe <09 LT & >18 LT.
- Auroral zone (geomag lat 60–73∘): frequent night storms; occupy ~1 week; late-summer best; observatory correction unreliable.
- Polar cap (>77∘): summer IMF offsets in Z up to 60 nT; autumn–winter surveys; observatory interpolation often OK.
Reporting (IAGA scheme)
- Submit for each occupation: Regional network description, Record sheet, Computer file.
- Classification code: e.g. V1.0 (local vario, full correction).
- Send to WDC-A (Boulder) & IAGA WG V-8.
Minimal Checklist Before Leaving Site
- Gradient re-measured; photos taken.
- Absolute sets concur (≤1′, 5 nT).
- Variometer clock synced; data backed-up.
- Station description & status report updated.
- Local authorities thanked.