O 3 measurements during ATTREX
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Post on 23-Feb-2016
DESCRIPTIONO 3 measurements during ATTREX . Ru-Shan Gao and t he O 3 team. NOAA UAS O3 status Instrument performed well so far All data are finalized Instrument flown during SEAC 4 RS - Has since been checked out - Ready for the next ATTREX deployment. - PowerPoint PPT Presentation
<p>PowerPoint Presentation</p> <p>O3 measurements during ATTREX Ru-Shan Gao</p> <p>and </p> <p>the O3 team</p> <p>NOAA UAS O3 status</p> <p> Instrument performed well so far</p> <p> All data are finalized</p> <p> Instrument flown during SEAC4RS- Has since been checked out- Ready for the next ATTREX deployment</p> <p>OH in the tropical upper troposphere (TUT)</p> <p> Low concentration but important for pollutant degradation</p> <p> Direct source:O3 + hn O2 + O(1D)(R1)O(1D) + H2O 2OH(R2)</p> <p> O3, low H2O conditions in the TUT Low OH?- Kley et al., Science 19963Measurements in TUT during STRAT</p> <p>4Data are from the NASA STRAT mission. Only flights based in Hawaii were used in this work. Most tropospheric data are between 19 and 24 latitude, but there are a few short segments of data taken between 0 and 7. In the next figure we will show that OH in these regions (0-7 and 19-24) behave pretty much the same.4</p> <p>5</p> <p>STRAT TUT OH dataO3 + hn O2 + O(1D), O(1D) + H2O 2OH</p> <p>7</p> <p>STRAT TUT OH dataThis figure suggests that perhaps NO has influence on OH, but only at low SZAs doesnt make much sense. Recall that NO correlates with O3 and NOy, the pattern shown here also applies to O3 and NOy (except in plumes, where O3 is not high). HOx partitioning strongly depends on NO. When NO is low, OH is low and HO2 is high (see next figure)8 The cycling time between OH and HO2 is much shorter than the lifetime of HOx </p> <p> OH HO2:OH + CO (+ O2) HO2 + CO2 (R3)HO2 + NO OH + NO2 (R4)</p> <p> OH is controlled by R3, R4, and HOx sources and sinks</p> <p> O3+H2O is not the dominant HOx source</p> <p> Main HOx sink:NOy (high NOy) or HOx self reactions (low NOy)</p> <p>9</p> <p>Measurements in TUT during STRAT1010</p> <p>ATTREX O3</p> <p>ATTREX O3Concluding remarks:</p> <p>1) NOAA UAS O3 worked well and data are finalized</p> <p>2) A simple functional description for OH in the tropical upper troposhpere (TUT) is accurate to 50%- Except for air parcels with very low NO low OH</p> <p>3) It appears that the TUT OH has no dependence on O3 and H2O</p> <p>4) Source of very low NO air parcels: Low NO marine boundary air (low O3 and NOy as well) Strong convection without lightning marine convection Most likely place the west Pacific warm pool Low O3 can be an indicator of low NO and low OH!</p>
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