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Titel Thermal and near-infrared sounding for weather, air quality and greenhouse gas monitoring in the Arctic from highly elliptical orbits
VerfasserIn K. A. Walker, C. Sioris, J. C. McConnell, H. Buijs, L. Moreau, The PHEMOS Science Team
Konferenz EGU General Assembly 2012
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 14 (2012)
Datensatznummer 250070797
 
Zusammenfassung
The Canadian Space Agency’s PCW (Polar Communications and Weather) mission is a dual satellite mission with each satellite in a highly eccentric orbit with apogee ~42,000 km and a period in the 12-24 hour range to deliver continuous (24x7) communications and meteorological data over the Arctic. The baseline meteorological instrument is a 21-channel spectral imager similar to MODIS or ABI. The PHEMOS (Polar Highly Elliptical Molniya Orbital Science) mission is a science complement to the PCW mission to address weather, climate and air quality issues. The instrument package consists of a Fourier transform spectrometer (FTS) to cover the near-infrared and mid-infrared spectral range and an ultraviolet-visible (UVS) spectrometer. In a phase A study funded by the Canadian Space Agency, we are configuring an FTS instrument for thermal infrared sounding as well as for greenhouse gas monitoring via near-infrared solar reflection. Using imaging detectors allows many measurements in parallel with increased observation time up to 100 s per view. The field-of-regard (FOR) is subdivided into a number of views such that a full measurement of the FOR is completed in about 1 hour. A pointing mirror is used in a step and stare mode. The thermal infrared is covered with two optimized bands; band 1 covers 700 to 1400 cm-1 and band 2 covers 1800 to 2500 cm-1 for which the scientific focus are temperature and water vapour profiles and air quality species (including CO, O3, HNO3, NH3). The spectral resolution is 0.3 cm-1. The near-infrared spectral bands target absorption signatures of CO2, CH4, and O2. The two relevant spectral ranges are 5990-6450 cm-1 and 13060-13168 cm-1 (O2-A band), measured with spectral resolutions of 0.3 and 0.6 cm-1, respectively. The O2-A band is used to determine surface pressure, albedo, and aerosol optical depth and vertical distribution, the latter of which is critical for CO2 retrieval. The FTS instrument design will be presented as well as design challenges and expected performance. Retrieval studies examining the feasibility of measuring CO2, CH4, and aerosol properties as a function of signal-to-noise ratio, radiometric accuracy, surface albedo, and other factors will be presented as well.