Professor Shepherd began his research with studies of the aurora borealis, conceiving new instruments for its observation. The implementation was done by his students, postdocs and research associates of which not all can be mentioned here. These began with the Fabry-Perot Interferometer (John Nilson, Leroy Cogger, Steven Peteherych). The most notable was introducing “field-widening” to the Michelson interferometer (Ronald Hilliard, Harold Zwick) and operating it by scanning over a single fringe to obtain atmospheric temperatures from both aurora and airglow.[1] His ground-based observations (Robert Peterson, Kenneth Paulson) were later extended to measurements from rockets (John Miller, Ashley Deans), flown from the Churchill Research Range at Churchill, Manitoba[2] and Cape Parry on the Arctic coastline.[3] He then moved to satellite measurements with the Red Line Photometer (RLP) on the Canadian ISIS-II satellite (Frank Bunn, Frank Thirkettle), launched in 1971.[4] This instrument mapped the auroral O(1D) red line emission, produced by low energy electrons, specifically in the dayside cusp.[5] A wide-angle Michelson interferometer was then conceived for the measurement of winds from space, called the Wind Imaging Interferometer (WINDII), launched on NASA’s Upper Atmosphere Research Satellite (UARS) (William Gault, Brian Solheim, Charles Hersom, Yves Rochon) in 1991.[6] It operated until 2003, providing new information on the dramatic influence of winds on processes in the upper atmosphere through migrating and non-migrating tides and planetary waves (Charles McLandress, Shengpan Zhang),[7] (Guiping Liu, Young-Min Cho).[8] Other versions of the field-widened instrument were developed, the Polarizing Atmospheric Michelson Interferometer and the Spatial Heterodyne Spectrometer (John Bird, Stephen Brown).[9] More recently, the superposition of these zonal waves was proposed for the existence of “bright nights”, a phenomenon known since Roman times of rare nights which were not dark, but exceptionally bright.[10] WINDII data were most recently used to describe the existence of a high-latitude “wind wall”, with reversals of zonal wind from eastward to westward with velocities of up to 600 meters/second (Marianna Shepherd).[11]