Global tropospheric measurements of mitric acid vapor and particulate nitrate
B. J. Huebert, A. L. Lazrus
Abstract
B. J. Huebert, A. L. Lazrus
Abstract
Measurements of HNO3 vapor and particulate NO3− were made over continental and marine areas, at altitudes from .2 to 7 km, as a part of Project Gametag. HNO3 vapor was found to be as common over marine areas, far from anthropogenic sources of NOx, as over remote continental regions, ranging from < .02 to .3 ppbv. Urban influenced continental values ranged from .3 to .86 ppbv. Comparable HNO3 was found both above and within the boundary layer, in contrast to theoretical predictions of a negative HNO3 gradient with altitude. In many regions of the troposphere there was more HNO3 vapor than participate NO3−, although the reverse is true in the marine boundary layer, where it appears that heterogeneous chemistry converts HNO3 and Cl− to HCl and particulate NO3−. This rather limited data set suggests an HNO3 lifetime on the order of a few days.
OpenAlex reports 57 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Measurements of HNO3 vapor and particulate NO3− were made over continental and marine areas, at altitudes from .2 to 7 km, as a part of Project Gametag. HNO3 vapor was found to be as common over marine areas, far from anthropogenic sources of NOx, as over remote continental regions, ranging from < .02 to .3 ppbv. Urban influenced continental values ranged from .3 to .86 ppbv. Comparable HNO3 was found both above and within the boundary layer, in contrast to theoretical predictions of a negative HNO3 gradient with altitude. In many regions of the troposphere there was more HNO3 vapor than participate NO3−, although the reverse is true in the marine boundary layer, where it appears that heterogeneous chemistry converts HNO3 and Cl− to HCl and particulate NO3−. This rather limited data set suggests an HNO3 lifetime on the order of a few days.
Key concepts: Troposphere, Particulates, Altitude (triangle), Nitrate, Atmospheric sciences, Environmental science, Water vapor, Boundary layer