Abstract
Reply [to “Comment on ‘Indications of photochemical histories of Pacific air masses from measurements of atmospheric trace species at Point Arena, California’ by D. D. Parrish et al.”
Highlights
Title Reply [to “Comment on ‘Indications of photochemical histories of Pacific air masses from measurements of atmospheric trace species at Point Arena, California’ by D
Finlayson-Pitts has pointed out that the observed slopes are in remarkable agreement, and all are significantly slope of the n-butane to ethane versus propane to ethane smaller than predicted by OH kinetics, which is 2.75 + 0.55 correlationin Figure 9 of Parrish et al [1992] is in closer
Atoms make a substantial contribution to the removal of the These relatively small slopes are characteristic of the free light alkanes from the tropical and temperate marine troposphereand continental air massesas well as the marine troposphere.,we believethat muchmore substantial boundary layer
Summary
Title Reply [to “Comment on ‘Indications of photochemical histories of Pacific air masses from measurements of atmospheric trace species at Point Arena, California’ by D. Atoms make a substantial contribution to the removal of the These relatively small slopes are characteristic of the free light alkanes from the tropical and temperate marine troposphereand continental air massesas well as the marine troposphere.,we believethat muchmore substantial boundary layer. As discussedsemiquantitativeliyn the appendixof Parrish et relative contributions of C1 atom and OH radical reactions to al.
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