Exploratory analysis of the distribution of condensation nuclei in the Northern Hemisphere upper troposphere and lower stratosphere during the late 1970s

Citation
Ag. Detwiler et al., Exploratory analysis of the distribution of condensation nuclei in the Northern Hemisphere upper troposphere and lower stratosphere during the late 1970s, J GEO RES-A, 105(D7), 2000, pp. 9265-9282
Citations number
60
Categorie Soggetti
Earth Sciences
Volume
105
Issue
D7
Year of publication
2000
Pages
9265 - 9282
Database
ISI
SICI code
Abstract
Data obtained from the Global Atmospheric Sampling Program (GASP) during th e late 1970s are used to evaluate the hypothesis that particulate emissions by aircraft are a significant source for the upper tropospheric/lower stra tospheric fine and ultrafine aerosol. Measurements of condensation nuclei ( CN) were acquired above 6 km mean sea level as part of GASP from October 19 77 through June 1979, using automated packages on up to four commercial air liners simultaneously flying their normal daily routes. These routes spanne d much of the midlatitude Northern Hemisphere, with the notable exceptions of the former Soviet Union and China. The GASP measurements are analyzed to determine the vertical, geographical, and seasonal distribution of upper t ropospheric/lower stratospheric CN in clear air, spanning an altitude range from several kilometers above to several kilometers below the tropopause. The general lack of vertical gradients in median CN mixing ratio at altitud es in the troposphere suggests that CN in the clear troposphere are general ly well mixed. CN mixing ratios decrease with distance above the tropopause , consistent with a tropospheric source for stratospheric CN. Median CN mix ing ratios for selected regions were compared to the Northern Hemisphere me dian, by altitude and season. Regional median CN mixing ratios can differ f rom the hemispheric median by more than a factor of 2 but never an order of magnitude. The lack of vertical variation of CN concentrations in the trop osphere is not at all consistent with the vertical variation of fuel consum ed by aircraft, which peaks at altitudes near the tropopause. The observati ons of CN show some regional medians exceeding Northern Hemisphere medians in some seasons and not others, but the regions with the highest medians ar e not always those with the highest aircraft fuel consumption. We conclude that aircraft emissions are not a major component of the global clear air b ackground CN measured during GASP.