Balmer a intensity measurements made with a dual etalon Fabry-Perot spectro
meter at Haleakala during two campaigns in 1988 are presented. The data fro
m each campaign demonstrate night-to-night stability, despite variations in
geophysical conditions. Analysis of these data using a nonisothermal Lyman
beta radiative transport code, updated solar Lyman beta line-center flux e
stimates, and corrected thermospheric atomic hydrogen density profiles poin
ts to the resolution of the "factor of 2" problem. A careful reassessment o
f other mechanisms for upper atmospheric Balmer a excitation has also been
carried out. (C) 2001 Elsevier Science Ltd. All rights reserved.