Fig. 5.From: Swarm SCARF Dedicated Lithospheric Field Inversion chainVertical component of the difference between the gradient (estimated by finite difference between Swarm A and Swarm B data, see the text for details) that would be estimated using lithosphere only data and the gradient obtained from the data imperfectly corrected for the main internal and external source fields. Projection is Mollweide.Back to article page