1. INTRODUCTION
Since the launch of the Landsat 4 Thematic Mapper, scientists interested in studying the long-wave infrared (LWIR) thermal properties of Earth’s surface, atmosphere, and water bodies at high-to-moderate resolution have been limited to making measurements at a 60-120 m ground sample (e.g. Landsat TM, ETM+), in no more than five spectral bands (e.g., Terra ASTER). This barely scratches the surface of the potential that the LWIR region of the spectrum has for quantifying Earth system processes. Operational acquisition of high spatial and spectral resolution LWIR data from Earth orbit would yield an hitherto unattainable measurement record for Earth scientists. Applications include mapping the chemistry of rocks and minerals exposed at Earth’s surface [1], the composition of volcanic gas and ash plumes [2], and quantifying soil moisture content and evapotranspiration [3].