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When a stratospheric satellite travels by prevailing winds in the stratosphere, its cross-track displacement needs to be controlled to keep a constant latitude orbital flight.
For a constant latitude there are two annual maxima of the ozone mixing ratio that occur nearly symmetrically about the winter solstice.
This variation was reduced if the index was calculated based on the magnetic field perpendicular to QD contours of constant latitude, scaled by the distance between such contours by use of QD base vectors.
There are also high-altitude cloud bands that wrap around the planet at constant latitude.
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If the electrojet is at near-constant latitude, it develops little Y component.
A major source of the magnetic fields sensed by these magnetometers, especially in the auroral zones, lies in often narrow currents flowing roughly parallel to lines of constant magnetic latitude.
Imager observations revealed that PMCs have essentially the same altitudes in the north and south (82.7 ± 1.3 km) and that cloud altitudes remain essentially constant with latitude.
Data can be profiled along a constant longitude, latitude or height and, in order to increase the visual analysis of the Z (height) dimension, there is a vertical shift of the model and a degree of vertical exaggeration.
Dipole field lines and lines of constant magnetic latitude are included to help visualise the behavior of the wave intensities as a function of L∗ and | λ m |.
Currents 1 … N C shown following lines of constant quasi-dipole latitude, with the satellite crossing the magnetic equator (shown as current j).
The zonal wind velocity at the cloud top is fairly constant in the latitude range of 50° S–50°N, while it is near solid-body rotation (constant angular velocity) below ∼40 km altitude.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com