Abstract
Airborne measurements of the hydroxyl radical were performed aboard the NASA P-3B using the Selected Ion Chemical Ionization technique during the Pacific Exploratory Mission (PEM)-Tropics B study. Typical midday boundary layer OH concentrations of 6-7 × 106 molecule cm-3 were observed in the vicinity of Christmas Island (0°-3° N), and 7-8 × 106 molecule cm-3 in the vicinity of Tahiti (17°-22° S). Photochemical box model calculations of the concentration of OH ([OH]) throughout the entire mission yield generally good agreement (slope = 1.26) with a tendency for the model to slightly overestimate the measured OH. Boundary layer measurements of OH in an air mass containing low ozone concentrations (<5 ppbv) yielded a midday [OH] of ∼5 × 106 molecule cm-3, some 45% lower than 7 × 106 molecule cm-3 observed in air masses at the same latitude with more typical ozone concentrations (30-40 ppbv). Measurements performed under clouds yielded [OH] of ∼2.5 × 106 molecule cm-3, a value which is a factor of 2 lower when compared to data taken on either side of the cloud. This decrease corresponds to the decrease in j(O3) to produce O(1D).
| Original language | English |
|---|---|
| Article number | 2000JD900832 |
| Pages (from-to) | 32657-32666 |
| Number of pages | 10 |
| Journal | Journal of Geophysical Research |
| Volume | 106 |
| Issue number | D23 |
| DOIs | |
| State | Published - Dec 16 2001 |
| Externally published | Yes |
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