J. Zou
University of Toronto
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Geophysical Research Letters | 2005
Peter F. Bernath; C. T. McElroy; M. C. Abrams; C. D. Boone; M. Butler; C. Camy-Peyret; Michel Carleer; Cathy Clerbaux; Pierre-François Coheur; Réginald Colin; P. DeCola; M. DeMazière; James R. Drummond; Denis G. Dufour; Wayne F. J. Evans; H. Fast; Didier Fussen; K. Gilbert; D. E. Jennings; E. J. Llewellyn; R. P. Lowe; Emmanuel Mahieu; J. C. McConnell; Martin J. McHugh; Sean D. McLeod; R. Michaud; Clive Midwinter; Ray Nassar; Florian Nichitiu; Caroline R. Nowlan
SCISAT-1, also known as the Atmospheric Chemistry Experiment (ACE), is a Canadian satellite mission for remote sensing of the Earths atmosphere. It was launched into low Earth circular orbit (altitude 650 km, inclination 74°) on 12 Aug. 2003. The primary ACE instrument is a high spectral resolution (0.02 cm-1) Fourier Transform Spectrometer (FTS) operating from 2.2 to 13.3 μm (750-4400 cm-1). The satellite also features a dual spectrophotometer known as MAESTRO with wavelength coverage of 285-1030 nm and spectral resolution of 1-2 nm. A pair of filtered CMOS detector arrays records images of the Sun at 0.525 and 1.02 μm. Working primarily in solar occultation, the satellite provides altitude profile information (typically 10-100 km) for temperature, pressure, and the volume mixing ratios for several dozen molecules of atmospheric interest, as well as atmospheric extinction profiles over the latitudes 85°N to 85°S. This paper presents a mission overview and some of the first scientific results. Copyright 2005 by the American Geophysical Union.
Journal of Geophysical Research | 2008
Jayanta Kar; Dylan B. A. Jones; James R. Drummond; Jean-Luc Attié; Jane Liu; J. Zou; Florian Nichitiu; M. D. Seymour; David P. Edwards; Merritt N. Deeter; John C. Gille; Andreas Richter
We show that the dayside MOPITT retrievals in the lower troposphere can provide useful information on surface sources of atmospheric CO over the Indian subcontinent. We find that MOPITT retrievals at 850 hPa show localized enhancements over the Indian subcontinent, which correlate with similar enhancements seen in the tropospheric NO2 columns from the SCIAMACHY instrument. In particular, high concentrations of CO over the Indo-Gangetic basin and some prominent cities are captured in the lower-tropospheric retrievals in spring. MOPITT averaging kernels (normalized to take into account the absorber amounts in the layers) indicate that the retrievals are sensitive to CO in the lower troposphere. In winter, MOPITT retrievals at 850 hPa can detect the strongest source areas over the eastern states of Bihar and West Bengal, thus confirming the so-called “Bihar pollution pool,” which was detected earlier in the aerosol measurements by the multiangle imaging spectroradiometer (MISR) aboard Terra. The pollution features are consistent with the spatial distribution of CO emissions in India, as reflected in the GEOS-Chem simulation of CO. Furthermore, these lower-tropospheric features in the simulation are still present after smoothing the modeled fields using the MOPITT averaging kernels and a priori profile, demonstrating that the retrievals do have sensitivity in the lower troposphere. This work indicates that although MOPITT retrievals are often most sensitive to CO in the middle and upper troposphere, they do provide information on lower-tropospheric CO in selected continental regions with strong thermal contrast and could be useful for pollution studies.
Optical Science and Technology, the SPIE 49th Annual Meeting | 2004
Kaley A. Walker; J. Zou; Florian Nichitiu; Kathleen L. Gilbert; David Turnbull; C. Thomas McElroy; Wayne F. J. Evans; Chris Ferguson; Eldon Puckrin; C. D. Boone; Sean D. McLeod; Michael J. Butler; Clive Midwinter; James R. Drummond; Peter F. Bernath
The Atmospheric Chemistry Experiment (ACE) was launched in August 2003 on board the Canadian scientific satellite SciSat-1. The ACE payload consists of two instruments: ACE-FTS, a high resolution (0.02 cm-1) Fourier transform infrared spectrometer and MAESTRO (Measurement of Aerosol Extinction in the Stratosphere and Troposphere Retrieved by Occultation), a dual UV-visible-NIR spectrograph. Primarily, the two instruments use a solar occultation technique to make measurements of trace gases, temperature, pressure and atmospheric extinction. It will also be possible to make near-nadir observations with the ACE instruments. The on-orbit commissioning of the instruments and spacecraft were undertaken in the months following launch. At the end of this period, a series of science-oriented commissioning activities were undertaken. These activities had two aims: the first was to verify and extend the measurement results obtained during the pre-launch Science Calibration Test campaign and the second was to confirm appropriate parameters and establish procedures for operational measurements (occultation and near-nadir observations and exo-atmospheric calibration measurements). One of the most important activities was to determine the relative location of each instrument field of view and optimize the pointing of the sun-tracker to provide the best viewing for both instruments.
international geoscience and remote sensing symposium | 2002
J. Zou; Florian Nichitiu; James R. Drummond
The MOPITT (Measurements Of Pollution In The Troposphere) instrument aboard the Terra Spacecraft was launched on Dec. 18, 1999 and has operated successfully since then. Instrument radiances are calculated from a total of 8 channels, which are combined in a retrieval scheme to measure the carbon monoxide (CO) profile and methane (CH/sub 4/) column in the troposphere. The instrument gain and offset, which are the key parameters to utilize the instrument measurements and to evaluate performance, are determined through an in-flight 2-point calibration scheme. Fluctuations and trends in the gain and offset on various time scales can be understood in terms of the instrument design, its performance, and the thermal environment. Some techniques for optimizing the noise levels as well as alternative methods of data processing, such as are required to cope with instrument anomalies, will be discussed.
Atmospheric Chemistry and Physics | 2008
Michel Carleer; C. D. Boone; Kaley A. Walker; Peter F. Bernath; K. Strong; R. J. Sica; Cora E. Randall; H. Vömel; Jayanta Kar; M. Höpfner; M. Milz; T. von Clarmann; Rigel Kivi; J. Valverde-Canossa; Christopher E. Sioris; M. R. M. Izawa; E. Dupuy; C.T. Mcelroy; James R. Drummond; Caroline R. Nowlan; J. Zou; Florian Nichitiu; Stefan Lossow; J. Urban; Donal P. Murtagh; Denis G. Dufour
Journal of Geophysical Research | 2004
H. Bremer; Jayanta Kar; James R. Drummond; Florian Nichitu; J. Zou; Jane Liu; John C. Gille; Merritt N. Deeter; Gene Francis; Daniel Charles Ziskin; Juying Xie Warner
Advances in Space Research | 2010
James R. Drummond; J. Zou; Florian Nichitiu; Jayanta Kar; Robert Deschambaut; John P. Hackett
Journal of Geophysical Research | 2006
Jane Liu; James R. Drummond; Dylan B. A. Jones; Zuohao Cao; H. Bremer; Jayanta Kar; J. Zou; Florian Nichitiu; John C. Gille
Journal of Geophysical Research | 2010
Christopher E. Sioris; C. D. Boone; Peter F. Bernath; J. Zou; C. T. McElroy; C. A. McLinden
Atmospheric Chemistry and Physics | 2007
A. Fraser; Florence Goutail; K. Strong; Peter F. Bernath; C. D. Boone; W. H. Daffer; James R. Drummond; D.G. Dufour; Tobias Kerzenmacher; G. L. Manney; C.T. Mcelroy; Clive Midwinter; C. A. McLinden; Florian Nichitiu; Caroline R. Nowlan; Jennifer Walker; Kaley A. Walker; Hsi-Jung Wu; J. Zou