A magnetic field line is an integral curve tangent to the magnetic field. In coordinates , it obeys wherever the relevant components are nonzero.
A magnetic arcade is a family of arch-shaped magnetic field lines joining two regions of a boundary. The boundary intersections are its footpoints. In a simple line-tied family, paired footpoints can be labelled by Euler potentials. A decaying linear force-free magnetic arcade is one explicitly solvable planar example; a general arcade need not be linear or force-free.
The curvature vector of a magnetic field line parametrized by arc length. For circular lines, it points towards their center and has magnitude . The curvature contribution to magnetic tension is in Gaussian units.
A flux tube is a bundle of magnetic field lines bounded by a surface everywhere tangent to the magnetic field. Gauss's law for magnetism makes the magnetic flux through any transverse cross-section constant along the tube. For a narrow tube with nearly uniform field magnitude and transverse area , this gives .
The cross-sectional area of a narrow flux tube, measured normal to its magnetic field. Constancy of the magnetic flux gives along the tube. This area controls the mass transport when flow follows the field.
The magnetic-field-line equation states that the tangent to a field line is parallel to . In spherical coordinates for an axisymmetric poloidal field, it can be written .
Outside a localized magnetic dipole , the vacuum field in Gaussian conventions isFor a dipole along the polar axis, and .
For coaxial circular loops with radii , the first loop's on-axis magnetic field of a circular current loop has far value . Its near-axis radial magnetic field at the second loop is . Integrating the axial Lorentz force from gives the displayed magnitude. Equal current senses attract; opposite senses repel. This is the leading dipole limit and is not an exact close-coil force law.
For a centred magnetic dipole moment pointing toward geographic south, the field at northern latitude has northward component and downward component . These follow by resolving the magnetic dipole field into local radial and meridional directions. The downward inclination is therefore , while the magnitude is . This ideal aligned-dipole model has no eastward component and does not capture actual geographic departures of the geomagnetic field.
An axisymmetric dipole field line satisfies , where is its equatorial crossing radius. This follows by integrating .
Near the polar axis of a magnetic dipole field, . Conservation of magnetic flux in a flux tube consequently gives . A dipole magnetic-field line intersecting a sphere of radius at small polar angle obeysThis area is for one polar tube. The approximation requires ; the full magnetic dipole field does not remain a narrow polar tube at arbitrarily large radius.
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