DMSP satellite plasma flow data from 1987-1990 are used to derive empi
rical models of the polar cap potential for quasi-steady interplanetar
y magnetic field (IMF) conditions. The large data set, due to the high
duty cycle and nearly Sun synchronous DMSP orbits, allowed very strin
gent data selection criteria. The analysis indicates that a good descr
iption of the unskewed (Heppner Maynard pattern A) steady state polar
cap potential is Phi(A) = 10(-4)nu(2)+11.7B sin(3) (theta/2) kV, where
nu is the solar wind velocity in kilometers per second, B is the magn
itude of the interplanetary magnetic field in nanoteslas, and theta =
arccos (B-Z/\B\)(GMS). The IMF-dependent contribution to the cross pol
ar cap potential does not depend significantly on solar wind pressure.
Functional forms for the potential do benefit from inclusion of an IM
F independent term proportional to the solar wind flow energy. Best fi
ts to IMF-independent contributions to the steady state polar cap pote
ntial yield similar to 16 kV for nu(SW) = 400 kilometers per second. D
uring steady IMF the total unskewed polar cap potential drop is shown
to be approximately Phi(A) = 16.5 + 15.5 Kp kV. The distribution of po
tential around the polar cap is examined as a function of magnetic loc
al time. A sinusoidal distribution is an excellent description of the
distribution, and more complex forms are not justified by this data se
t. Analysis of this data set shows no evidence of saturation of the po
lar cap potential for large \IMF\. A simple unified description of the
polar cap potential at all magnetic local times (MLT) and IMF, Phi(IM
F, MLT) = -4.1 + 0.5 sin ((2 pi/24) MLT + 0.056 + 0.015 B-Y(eff))(1.1
x 10-4 nu(2) + 11.1 B sin(3) (theta/2)) kV, is generated, where B-Y(ef
f) is B-Y (-B-y) in the northern (southern) hemisphere. If IMF data is
unavailable, the polar cap potential is well described by Phi(A)(Kp,
MLT) = -4.1 +1/2 sin ((2 pi/24) MLT +phi(HM))(16.4 + 15.2 Kp) kV, wher
e phi(HM) is a small phase correction of (-0.054, -0.031, 0.040) for H
eppner-Maynard convection patterns (BC, A, DE), respectively.