Calculate Earth's magnetic field at specific location and time using World Magnetic Model 2010 (WMM2010)
Aerospace Blockset Obsolete Library
The World Magnetic Model 2010 block implements the mathematical representation of the National Geospatial Intelligence Agency (NGA) World Magnetic Model 2010 (WMM2010). The World Magnetic Model 2010 block calculates the Earth's magnetic field vector, horizontal intensity, declination, inclination, and total intensity at a specified location and time. The reference frame is north-east-down (NED).
The WMM2010 specification produces data that is reliable five years after the epoch of the model, which is January 1, 2015.
The internal calculation of decimal year does not take into account local time or leap seconds.
The WMM2010 specification describes only the long-wavelength spatial magnetic fluctuations due to the Earth's core. Intermediate and short-wavelength fluctuations, contributed from the crustal field (the mantle and crust), are not included. Also, the substantial fluctuations of the geomagnetic field, which occur constantly during magnetic storms and almost constantly in the disturbance field (auroral zones), are not included.
You cannot use this block to model the Earth magnetic field above an altitude of 1,000,000 meters.