Atmospheric Chemistry Experiment (ACE): Organic Molecules from Orbit Peter Bernath Department of Chemistry, University of York Heslington, York, UK
ACE Satellite Bernath et al. GRL, 32, L15S01 (2005) See
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
Optical Layout (ABB-Bomem)
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
VOCs and Air Quality Volatile Organic Compounds (VOCs) lead to the production of tropospheric ozone, a pollutant.
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, (2009)
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
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.
Annual Average and Seasonal Variation
AVERAGE PROFILES: 2005
HCOOH VALIDATION Data from JPL Mark IV balloon FTS (Geoff Toon)
Ethane, Propane and Acetone
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
Pure Ethane Spectrum - 3 µm (195 K) PQ3PQ3
New Ethane Spectra T=252 K P=100.0, 351.0, and Torr of synthetic air (pure spectra also recorded) Spectra recorded at T=300, 270, 250, 215, 195 K for several air pressures
Propane T=195 K P=40.1 Torr A set of propane spectra have been recorded and acetone is underway.
Ethane Retrievals – cm -1 microwindow ( P Q 3 ).
Ethane Retrievals Various microwindows ( P Q branches)
Cometary Emission (8P/Tuttle) Böhnhardt et al. Ap J, 683, L71 (2008)