2.3. Instrumentation/Specifications

INTERMAGNET does not specify the type of magnetometer that must be used (although a list of instrument suppliers can be provided on request), however an IMO must try to meet the recommendations listed below. These specifications are used by INTERMAGNET as a guideline for reviewing data quality when data are either submitted for an IMO application, or when definitive data are submitted for inclusion in the INTERMAGNET archive. A scalar magnetometer is not mandatory, but is recommended for data quality monitoring.

2.3.1. Definitive Data

Accuracy

±5nT

2.3.2. Absolute Measurements

See Chapter 4

2.3.3. Vector Magnetometer

Resolution

0.1nT

Dynamic Range

±4000nT High Latitude

±3000nT Mid/Equatorial Latitude

Band pass

D.C. to 0.1Hz

Sampling rate

1Hz

Thermal stability

0.25nT/°C

Long term stability

5nT/year

2.3.4. Scalar Magnetometer

Resolution

0.1nT

Accuracy

1nT

Sampling rate

0.033Hz (30 sec)

2.3.5. Clock Timekeeping

Observatory data logger

5 seconds centered on UTC minute (mm:00)

Data collection platform

±1.5 sec GOES, GMS

±1.0 sec METEOSAT

2.3.6. Recorder

An on-site recorder is necessary so data are not lost as a result of data transmission outages.

2.3.7. Transmission

Transmission to a Geomagnetic Information Node (GIN) must be over the Internet or by satellite, within 72 hours of acquisition or sooner (see Section 6.1.4 ).

Note

Keeping within the time slot for satellite transmission is an important duty of an IMO operator. When advised by a GIN of a time drift, the IMO operator must make the necessary corrections within 24 hours.

2.3.8. Other

Preliminary data

transmitted in IAGA2002 format (IMFV2.83 for satellite)

Definitive data

to be submitted annually for inclusion in the IRDS in IAFV2.11 format

Instrument baseline data

to be submitted annually for inclusion in the IRDS in IBFV2.00 format

Annual means

to be submitted annually for inclusion in the IRDS in IYFV1.02 format

Filtering

to INTERMAGNET standard (Section 2.4 )

For more information see Section 6.1.1 for Data Formats and Section 6.1.2 for Data Types.

2.3.9. Proton Gyromagnetic Ratio

In 2009, INTERMAGNET adopted the new proton gyromagnetic ratio (for H2O, sphere, 25°C) published by the CODATA group in 2006 (see https://physics.nist.gov/cuu/pdf/all_2006.pdf ):

\[g_p = 2.675153362*10^8 . T^{-1}S^{-1}\]

This ratio divided by 2 pi relates the magnetic field strength in T to the output frequency (Larmor frequency) of a proton magnetometer in Hz. For example, a field strength of 50000.00 nT gives a Larmor frequency of 2128.819 Hz.