J7.3 Observations of Mixing Ratios and Fluxes of Reactive Nitrogen Oxides above a Mixed Hardwood Forest in Central Ontario during the Summer and Fall of 2011

Wednesday, 30 May 2012: 2:15 PM
Kennedy Room (Omni Parker House)
Jeffrey A. Geddes, University of Toronto, Toronto, ON, Canada; and J. G. Murphy

Anthropogenic activities have significantly disrupted the global nitrogen cycle causing numerous environmental problems such as tropospheric ozone and aerosol production, acidification, eutrophication, and biodiversity loss. At the same time, accelerated nitrogen deposition may also be driving increased carbon uptake by the world's forests, but many uncertainties regarding atmospheric nitrogen chemistry in forested environments remain. The work presented here is part of a long-term interdisciplinary project to study carbon and nitrogen cycling at a mid-latitude mixed hardwood forest in central Ontario, where estimates of nitrogen deposition are among the highest in North America.

Measurements of NOx (= NO + NO2) and NOy (= NOx + NO3 + N2O5 + HNO3 + HONO + volatile p-NO3- + organic nitrates) were made above the forest canopy from a 30 m tower by a two-channel chemiluminescence analyzer (Air Quality Design, Inc.), co-located with open path eddy covariance instrumentation for flux measurements. Conversion of NO2 to NO is achieved using a blue LED converter, and NOy to NO by a heated molybdenum converter. Sampling losses are minimized by locating the converters in an inlet case mounted at the top of the tower, connected to the rest of the instrument by 40 m of tubing. Detection limits at 1 Hz were between 10-20 ppt for NOx and NOy during the campaign. Ozone was also measured by a UV photometer (Thermo Scientific).

Dramatic early morning pulses of NO were observed that increased NO mixing ratios from around the detection limit at night to 250 ppt on average during the day. These increases were almost always related to photolytic losses of NO2. Likewise, NO2 levels (on average around 450 ppt throughout the campaign) closely followed photolytic conditions, building up during the day time only when skies were cloudy. Occasional pulses of NOx in the early morning were also observed, which could be associated with soil-level emissions, but may also be related to long-range advection as they recurred on days with similar wind conditions.

NOx oxidation products (NOz = NOy - NOx) during the campaign were usually lowest late at night (on average around 450 ppt) and highest in the late afternoon (on average around 790 ppt), again suggesting mostly photochemical sources. As expected, afternoon O3 was linearly correlated with NOz, with a slope of 19 ppb O3 per ppb of NOx oxidation. Often, increases in NOx oxidation products during the day could not be easily accounted for by photochemical NO2 oxidation alone, without an advective or local source. Ozone levels throughout the period showed the typical diurnal evolution with a minimum around 7 am (on average 22.8 ppb) and a maximum around 4 pm (on average 31.7 ppb).

NOx and NOy fluxes were also measured intermittently throughout the campaign. Here we focus on the NOy flux measurements. Eddy covariance measurements of NOy and vertical wind were averaged over 30 minutes, and corrected for time response and high frequency noise by applying appropriate filters to the CO2 covariances measured by a co-located open path instrument. The direction and magnitude of NOy fluxes were correlated with NOy mixing ratios, with deposition highest at high mixing ratios, and near zero fluxes or emissions at low mixing ratios. The emission fluxes organized even more tightly around NO2 concentrations, with few emission fluxes measured when NO2 was above 400 ppt. It is unclear if this may also be due to other co-variables especially given the diurnal behaviour of NO2. Emission and deposition fluxes each have strong diurnal patterns when treated separately, peaking during the middle of the day. Further investigation will attempt to separate the effect of instrumental difficulties in measuring fluxes during the night which could conceivably contribute to this diurnal pattern. Nevertheless, NOy mixing ratios also follow a diurnal pattern, and Particular cases where NOy mixing ratios were affected by emission fluxes vs. deposition fluxes will be explored. These will be discussed in terms of the chemistry and transport  governing NOy composition during those observations.


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