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Atmospheric Chemistry Experiment (ACE): Organic Molecules from Orbit Peter Bernath Department of Chemistry, University of York Heslington, York, UK
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ACE Satellite Bernath et al. GRL, 32, L15S01 (2005) See http://www.ace.uwaterloo.ca/
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Solar Occultation Advantages: Radiance of sun gives higher S/N than emission Limb view gives longer path length ~500 km (lower detection limits) than nadir “Self-calibrating” so excellent long-term accuracy and precision Disadvantages: Modest global coverage Samples only free troposphere
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Optical Layout (ABB-Bomem)
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ACE-FTS Species Measured Baseline species (version 2.2): H 2 O, O 3, N 2 O, CO, CH 4, NO, NO 2, HNO 3, HF, HCl, N 2 O 5, ClONO 2, CCl 2 F 2, CCl 3 F, as well as pressure and temperature from CO 2 lines Other routine species: COF 2, CHF 2 Cl, CF 4, CH 3 Cl, C 2 H 6, SF 6, OCS, HCN Research species: CCl 4, HOCl, H 2 O 2, HO 2 NO 2, CCl 2 FCClF 2, CH 3 CClF 2, ClO, C 2 H 2, C 2 H 4, C 2 H 6, COFCl, COCl 2, CH 3 OH, H 2 CO, HCOOH, N 2 and additional isotopologues
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VOCs and Air Quality Volatile Organic Compounds (VOCs) lead to the production of tropospheric ozone, a pollutant.
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Formic Acid HCOOH and CH 3 COOH are the most important organic acids in the troposphere. Has an important role in HO X chemistry Main sources: Biomass burning, biogenic (growing season) and anthropogenic (e.g., car exhaust) emissions. Indirect sources from numerous VOCs Most important sinks: OH reaction (slow), dry and wet deposition Generally poor agreement between observations and chemical transport models. Gonzalo Gonzalez Abad et al., ACPD 9, 12465 (2009)
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Previous work Numerous field measurements have been reported, but not many in the upper troposphere. Models are still struggling to predict HCOOH concentrations Rinsland et al. & Coheur et al. report ACE retrievals in biomass burning plumes
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ACE RETRIEVALS: SPECTROSCOPY Spectroscopic parameters for HCOOH taken from Perrin and Vander Auwera (2007) and Vander Auwera et al. (2007). HITRAN 2007 update. ACE retrievals carried out by Chris Boone.
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Annual Average and Seasonal Variation
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AVERAGE PROFILES: 2005
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HCOOH VALIDATION Data from JPL Mark IV balloon FTS (Geoff Toon)
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Ethane, Propane and Acetone
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ACE C 2 H 6 (Geoff Toon) All hydrocarbons have their strongest bands near 3000 cm -1 ; C 2 H 6 and CH 4 dominate the spectrum and need to be improved C 2 H 6 ν 7 band at 2985 cm -1 PQ3PQ3
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Pure Ethane Spectrum - 3 µm (195 K) 7 5 5 + 11 2 + 6 PQ3PQ3
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New Ethane Spectra T=252 K P=100.0, 351.0, and 562.6 Torr of synthetic air (pure spectra also recorded) Spectra recorded at T=300, 270, 250, 215, 195 K for several air pressures
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Propane T=195 K P=40.1 Torr A set of propane spectra have been recorded and acetone is underway.
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Ethane Retrievals 2975.5 – 2977.5 cm -1 microwindow ( P Q 3 ).
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Ethane Retrievals Various microwindows ( P Q branches)
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Cometary Emission (8P/Tuttle) Böhnhardt et al. Ap J, 683, L71 (2008)
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