Andrew O. Langford

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Andrew O. Langford NOAA ESRL Chemical Sciences Division, Boulder, CO Global Monitoring Annual Conference, May 21, 2014

Transcript of Andrew O. Langford

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Andrew O. Langford NOAA ESRL Chemical Sciences Division, Boulder, CO Global Monitoring Annual Conference, May 21, 2014

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May-June

Do stratosphere-to-troposphere (STT) and transport from Asia contribute to high springtime O3 in Clark County, NV?

How do these contributions compare to local production and regional transport from Los Angeles or wildfires?

67 ppbv

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Meiyun Lin, Princeton and NOAA GFDL Stratospheric influx is greatest in the Intermountain West

CC:Asia

CC:STT >20 ppbv

≈5 ppbv

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NOAA/CIRES Christoph Senff, Raul Alvarez, Scott Sandberg, Ann Weickmann, Richard Marchbanks, John Holloway, Eric Williams, Jerome Brioude, Owen Cooper

NOAA/NESDIS Brad Pierce CoDPHe Pat Reddy NOAA GFDL Meiyun Lin Clark County Department of Air Quality

Zheng Li, Dennis Ransel, Mickey Turner, Andy Gagliardo LVOS supported by Clark County DAQ and NASA TOLNet

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• TOPAZ scanning mobile ozone lidar (ARS, NOAA/ESRL/CSD) • In situ O3, CO, and meteorology (Holloway, NOAA/ESRL/CSD/CIRES) • Satellite imagery (Cooper, NOAA/ESRL/CSD/CIRES) • FLEXPART particle dispersion model (Brioude, NOAA/ESRL/CSD/CIRES) • RAQMS forecasts and analyses (Pierce, NOAA/NESDIS) • IPV analyses (Reddy, CoDPHE) • AM3 Model Runs (Lin, NOAA GFDL and Princeton)

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Continuous 5-min winds, T, and RH

Continuous 1-min CO and O3 CO: VUV resonance fluorescence (Holloway et al.) ±4%, ±1 ppbv for 1-min average O3: UV absorption, TECO 49C (Williams et al.)

±2% for a 1-min average

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Stratospheric intrusions

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Biomass Burning and LA Basin

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Marine air and locally produced ozone

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UT/LS: High O3/Low CO/Low H2O

Boundary layer: Low-High O3/High CO/High H2O

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Lo O3/Lo CO Hi H2O MBL

Hi O3/Lo CO Lo H2O UT/LS

Hi O3/Hi CO Med H2O Wildfire/LA

Hi O3/Hi CO Lo H2O Asia

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Negative correlations before each LVOS exceedance day.

Dry air before each LVOS exceedance day.

No significant wildfire contributions to LVOS exceedance days.

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Stratospheric air before each LVOS exceedance.

Asian pollution contributes to first and last exceedances.

No significant wildfire contributions to LVOS exceedance days.

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Exceedances of the current NAAQS on 3 days (May 21, May 25, and June 21)

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• STT contributed to all three O3 NAAQS exceedances during LVOS.

• Exceedances will become more frequent in Clark County if the NAAQS is lowered.

• Much of the Intermountain West will be unable to meet stricter O3 standards.

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Thank you, thank you very much!

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4 stations in exceedance of the current NAAQS on May 25

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Pat Reddy, CoDPHe

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FLEXPART tracers in the PBL (<1.5 km asl)

Biomass Burning CO Asian Transport CO Stratospheric O3

00 UT May 25, 2013

Jerome Brioude, NOAA/ESRL

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Brad Pierce, NOAA/NESDIS

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Emma Yates, NASA Ames/Thierry LeBlanc TMF

≈2130 UT

Table Mountain ozonesonde

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+10 ppbv

Elevated O3 layer above Angel Peak at sunrise

Surface O3 anticorrelated with CO and H2O

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67 ppbv

Highest mean ozone in Clark County mid-May to mid-June

6 days > 75 ppbv 24 days > 70 ppbv 47 days > 65 ppbv