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contributor authorRahnama, Peyman
contributor authorRochon, Yves J.
contributor authorMcDade, Ian C.
contributor authorShepherd, Gordon G.
contributor authorGault, William A.
contributor authorScott, Alan
date accessioned2017-06-09T17:23:10Z
date available2017-06-09T17:23:10Z
date copyright2006/06/01
date issued2006
identifier issn0739-0572
identifier otherams-84264.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227581
description abstractThis paper presents an instrument model and observation simulations for the measurement of stratospheric winds and ozone concentration using a satellite instrument employing imaging and the Doppler Michelson interferometery technique. The measurement technique and instrument concept are described. The instrument model and simulations are based on initial design characteristics of the Canadian Stratospheric Wind Interferometer for Transport Studies (SWIFT) satellite instrument. SWIFT employs an imaging array and a field-widened Michelson interferometer. It will measure stratospheric winds and ozone densities using the wind-induced phase shifts of interferograms from atmospheric limb radiance spectra in the vicinity of the vibration?rotation ozone line at 1133.4335 cm?1. The measurement simulation and analysis tools have been developed to assess the SWIFT instrument performance and to evaluate the impact of instrument and measurement characteristics on expected wind and ozone errors. Sample results of the measurement simulation and the related line-of-sight wind error noise levels are presented.
publisherAmerican Meteorological Society
titleSatellite Measurement of Stratospheric Winds and Ozone Using Doppler Michelson Interferometry. Part I: Instrument Model and Measurement Simulation
typeJournal Paper
journal volume23
journal issue6
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/JTECH1880.1
journal fristpage753
journal lastpage769
treeJournal of Atmospheric and Oceanic Technology:;2006:;volume( 023 ):;issue: 006
contenttypeFulltext


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