[1] Extensive chemical characterization of ozone (O 3 ) depletion events in the Arctic boundary layer during the TOPSE aircraft mission in March-May 2000 enables analysis of the coupled chemical evolution of bromine (BrO x ), chlorine (ClO x ), hydrogen oxide (HO x ) and nitrogen oxide (NO x ) radicals during these events. We project the TOPSE observations onto an O 3 chemical coordinate to construct a chronology of radical chemistry during O 3 depletion events, and we compare this chronology to results from a photochemical model simulation. Comparison of observed trends in ethyne (oxidized by Br) and ethane (oxidized by Cl) indicates that ClO x chemistry is only active during the early stage of O 3 depletion (O 3 > 10 ppbv). We attribute this result to the suppression of BrCl regeneration as O 3 decreases. Formaldehyde and peroxy radical concentrations decline by factors of 4 and 2 respectively during O 3 depletion and we explain both trends on the basis of the reaction of CH 2 O with Br. Observed NO x concentrations decline abruptly in the early stages of O 3 depletion and recover as O 3 drops below 10 ppbv. We attribute the initial decline to BrNO 3 hydrolysis in aerosol, and the subsequent recovery to suppression of BrNO 3 formation as O 3 drops. Under halogen-free conditions we find that HNO 4 heterogeneous chemistry could provide a major NO x sink not included in standard models. Halogen radical chemistry in the model can produce under realistic conditions an oscillatory system with a period of 3 days, which we believe is the fastest oscillation ever reported for a chemical system in the atmosphere.

[1] Inorganic bromine plays a critical role in ozone and mercury depletions events (ODEs and MDEs) in the Arctic marine boundary layer. Direct observations of bromine species other than bromine oxide (BrO) during ODEs are very limited. Here we report the first direct measurements of hypobromous acid (HOBr) as well as observations of BrO and molecular bromine (Br 2 ) by chemical ionization mass spectrometry at Barrow, Alaska in spring 2009 during the Ocean-Atmospheric-Sea Ice-Snowpack (OASIS) campaign. Diurnal profiles of HOBr with maximum concentrations near local noon and no significant concentrations at night were observed. The measured average daytime HOBr mixing ratio was 10 pptv with a maximum value of 26 pptv. The observed HOBr was reasonably well correlated (R 2 = 0.57) with predictions from a simple steady state photochemical model constrained to observed BrO and HO 2 at wind speeds <6 m s À1 . However, predicted HOBr levels were considerably higher than observations at higher wind speeds. This may be due to enhanced heterogeneous loss of HOBr on blowing snow coincident with higher wind speeds. BrO levels were also found to be higher at elevated wind speeds. Br 2 was observed in significant mixing ratios (maximum = 46 pptv; average = 13 pptv) at night and was strongly anti-correlated with ozone. The diurnal speciation of observed gas phase inorganic bromine species can be predicted by a time-dependent box model that includes efficient heterogeneous recycling of HOBr, hydrogen bromide (HBr), and bromine nitrate (BrONO 2 ) back to more reactive forms of bromine.

[1] Airborne measurements of CH 2 O were acquired employing tunable diode laser absorption spectroscopy during the 2001 Transport and Chemical Evolution Over the Pacific (TRACE-P) study onboard NASA's DC-8 aircraft. Above $2.5 km, away from the most extreme pollution influences and heavy aerosol loadings, comprehensive comparisons with a steady state box model revealed agreement to within ±37 pptv in the measurement and model medians binned according to altitude and longitude. Likewise, a near unity slope (0.98 ± 0.03) was obtained from a bivariate fit of the measurements, averaged into 25 pptv model bins, versus the modeled concentrations for values up to $450 pptv. Both observations suggest that there are no systematic biases on average between CH 2 O measurements and box model results out to model values $450 pptv. However, the model results progressively underpredict the observations at higher concentrations, possibly due to transport effects unaccounted for in the steady state model approach. The assumption of steady state also appears to contribute to the scatter observed in the point-by-point comparisons. The measurement-model variance was further studied employing horizontal flight legs. For background legs screened using a variety of nonmethane hydrocarbon (NMHC) tracers, measurement and model variance agreed to within 15%. By contrast, measurement variance was $60% to 80% higher than the model variance, even with small to modest elevations in the NMHC tracers. Measurement-model comparisons of CH 2 O in clouds and in the lower marine troposphere in the presence of marine aerosols suggest rather significant CH 2 O uptake by as much as 85% in one extreme case compared to expectations based on modeled gas phase processes.

[1] A steady state model, constrained by a number of measured quantities, was used to derive peroxy radical levels for the conditions of the Tropospheric Ozone Production about the Spring Equinox (TOPSE) campaign. The analysis is made using data collected aboard the NCAR/NSF C-130 aircraft from February through May 2000 at latitudes from 40°to 85°N, and at altitudes from the surface to 7.6 km. HO 2 + RO 2 radical concentrations were measured during the experiment, which are compared with model results over the domain of the study showing good agreement on the average. Average measurement/model ratios are 1.04 (s = 0.73) and 0.96 (s = 0.52) for the MLB and HLB, respectively. Budgets of total peroxy radical levels as well as of individual free radical members were constructed, which reveal interesting differences compared to studies at lower latitudes. The midlatitude part of the study region is a significant net source of ozone, while the high latitudes constitute a small net sink leading to the hypothesis that transport from the middle latitudes can explain the observed increase in ozone in the high latitudes. Radical reservoir species concentrations are modeled and compared with the observations. For most conditions, the model does a good job of reproducing the formaldehyde observations, but the peroxide observations are significantly less than steady state for this study. Photostationary state (PSS) derived total peroxy radical levels and NO/NO 2 ratios are compared with the measurements and the model; PSS-derived results are higher than observations or the steady state model at low NO concentrations.

O were 1390, 440, and 480 pptv, respectively, more than two times higher than TOPSE measurements and an order of magnitude higher than SONEX measurements. This is attributed to higher solar radiation levels and the more polluted conditions of INTEX-NA. Mixing ratios and variability decreased with altitude for all three gases and on all three campaigns, except for CH 3 OOH during TOPSE. The impact of convection on H 2 O 2 , CH 3 OOH, and CH 2 O is also discussed. Using the ratio H 2 O 2 /CH 3 OOH, convectively influenced air parcels were found to be enhanced in CH 3 OOH, CH 2 O, CO, NO, and NO 2 while H 2 O 2 and HNO 3 were depleted by wet removal. Biomass burning was also shown to increase H 2 O 2 , CH 3 OOH, and CH 2 O mixing ratios up to 1.5, 2, and 1 ppbv, respectively, even after 4-5 days of transit. Results from this study show considerable variability in H 2 O 2 , CH 3 OOH, and CH 2 O throughout the North American and North Atlantic troposphere. The variability in the upper troposphere is driven by local photochemical production and transport via regional convection and long-range pathways, suggesting transport mechanisms are important factors to include in photochemical models simulating H 2 O 2 , CH 3 OOH, CH 2 O, and HO x .

Abstract. Extensive measurements of ozone and its photochemical precursors and coproducts were made in the 1990 Rural Oxidants in the Southern Environment (ROSE) program. Peroxy radical production, loss, and partitioning are described at a rural site in Alabama, showing the important role that biogenic organic compounds play in ozone production. Estimates of the peroxy radical concentration obtained by four methods along with the measured nitric oxide level are used to predict the instantaneous rate of photochemical ozone production at the site. The four methods agree on the diurnal behavior of peroxy radicals and ozone production rates, while consistent discrepancies between the methods generally are within their combined uncertainties. Selected aircraft measurements are used to derive ozone production rates above the ground site, with the highest rates occurring in the boundary layer and in industrial plumes. The dependences of peroxy radical concentration and ozone production rate on the level of nitrogen oxides exhibit good agreement between the various methods and are consistent throughout the lower troposphere. Surface deposition and entrainment are shown to be as important as photochemical production in determining the diurnal evolution of ozone at this site.

Abstract. In a flight through a wave cloud during SUCCESS on 2 sampling opportunity since the particles are only minutes old and May 1996, simultaneous forward-and aft-facing NOy inlets were likely nucleated on sulfuric acid aerosols [Jensen et al., this issue]. used to infer the amount of condensed-phase NOy present on ice particles that were up to a few minutes old. Condensed-phase 2. Measurements amounts were 25-75 pptv, or 10-20% of gas-phase NOy. Given The "aft-inlet" NOy was sampled through a horizontal inlet the rapid HNO 3 uptake on ice observed in the laboratory, a model calculation implies that virtually all of the gas-phase HNO3 will be tube oriented perpendicular to the aircraft window. The tube's end depleted in the first 1-2 minutes after the appearance of ice. Thus face was a 45" cut, oriented 45" away from directly aft. This inlet , though for the ice cloud ice particles is the subject of this paper. particles of interest here, 10-20 [tm in diameter, the enhancement The partitioning of NOy between the gas and condensed phases factors are very close to the high-mass limit and so not as sizeis an important aspect of the NOy budget. Species will be subject dependent as for the smaller particles in PSCs. Since the highto different chemical and transport processes depending on mass limit is well-defined, and simply equal to the ratio of the true whether they are in the gas or condensed phase. Photolytic and air speed and the known flow velocity inside the inlet tube, chemical reactions will be different, and the vertical transport will enhancement factor errors due to flow around the inlet are be different, as particles will sediment. The presence of NOy minimal. The high-mass enhancement factor is altitude-dependent species in ice particles could result from several processes: (1) since a constant mass flow is drawn into the inlet. It has a value of They could be in the ice nuclei responsible for ice formation. (2) 43 for the case described in this paper at 41 kft. Integrations of Their presence could result from chemical conversions that occur the size-dependent enhancement factor over the particle size in/on the particles and that leave the product species in the spectrum give values which are generally within a few percent of condensed phase. Or, (3) they could be adsorbed onto the ice this upper limit when in the wave cloud and not at the very edge. surface during or after growth.On the other hand, the flow around the fuselage could also impact During SUCCESS we employed forward-and aft-facing inlets particle concentrations. Using the semi-empirical approach of to measure NOy. Since cloud ice particles are collected with King [1984], we have estimated a shadow zone depth for 10o[tm enhanced efficiency by the forward-facing inlet and discriminated diameter particles of 4 cm at the fuselage station (530 in.) of the against by the aft, the difference between the two simultaneous inlet. The inlet stuck out 37 cm into the flow, and at this point the NOy measurements enables a measurement of the amount...

During the Mauna Loa Observatory Photochemistry Experiment (MLOPEX 2), simultaneous clear sky measurements of [NOel, [NO], [Oa], and NO2 photodissociation rate were collected during autumn TOOT, winter, spring, and summer 1992 intensive measurement periods at Mauna Loa Observatory (MLO), Hawaii. These measurements were used to assess the Oa-NO-NO2 photostationary state, and to infer peroxy radical concentration, ozone photochemical production and destruction rates, as well as the relationship between the deviation of the photostationary state parameter, 0 = j2[NO2]/k•[Oa][NO], from unity and environmental variables. In addition, a photochemical box model was used for the purpose of comparison with observations and interpretation of the results. A systematic deviation of 6 from unity was determined from measurements, this parameter reached values of 1.5-2 for high-sun conditions depending on the season. The inferred total peroxy radical concentrations were generally larger (25-70 pptv for high-sun conditions depending on the season) than those directly measured (20-25 pptv during noontime). Model results seem generally to underestimate the value of 6 and to overpredict the hydroxyl and total peroxy radical concentrations, suggesting loss processes not accounted for in the model for these species. Analysis of the contributions to the net ozone photochemical production indicates total production and destruction terms reaching 10-15 ppbv/day which tend to nearly cancel on a daily average basis. High-sun values of 6-T were shown to be independent of NOs (= NO + NO2) for NOs concentrations above about 50 pptv. However, below this level, observations show that 6-1 generally decreases with increasing nitrogen oxide concentrations. Furthermore, the measured 0-1 correlation with v/[n20]/[oa] suggests the existence of NO to NO2 oxidants not accounted for in a simplified HO• chemistry. From this sequence, NO is rapidly oxidized by Os to