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With a slight modification of the plasma drift velocity the SAMI2 model has been successful in reproducing quiet time ionospheric low latitude features like Equatorial Ionization Anomaly.
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The coupled Earth dynamo can reproduce two of the most salient features of the historical secular variation down-projected at the core-mantle boundary (e.g., Jackson and Finlay 2015), namely its hemispherical dichotomy (the strongest variations occurring in the so-called Atlantic hemisphere) and the westward drift of low-latitude features at a speed of about 15 km/year.
Outside polar latitudes, features corresponding to surface thaw have yet to be identified on Mars.
Because of this rotation, one can expect a modulation of Sq by the Earth's main magnetic field, with its most striking mid-latitude feature being the SAA.
In principle, the optimisation of the absorber orientation depends on the local latitude, climatical features and solar geometry.
In principle, the optimisation of the absorber orientation depends on the local latitude, climatic features and solar geometry.
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At higher latitudes, the features are more subdued, while the low latitudes are full of small- and large-scale features.
These robust low-latitude geomagnetic features (Jackson 2003) are more difficult to reproduce in dynamo models than high-latitude flux patches (Christensen et al. 1998), possibly due to flux dispersion by upwelling (Wicht et al. 2009) that reconnects with the downwellings near the tangent cylinder in the dynamo's meridional circulation (Aubert 2005).
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