Latitudinal distribution of reactive nitrogen in the free troposphere over the Pacific Ocean in late winter/early spring. Singh, H., B., Viezee, W., Chen, Y., Thakur, A., N., Kondo, Y., Talbot, R., W., Gregory, G., L., Sachse, G., W., Blake, D., R., Bradshaw, J., D., Wang, Y., & Jacob, D., J. Journal of Geophysical Research, 103(D21):28237-28246, 1998.
abstract   bibtex   
The late boreal winter/early spring (February/March 1994) measurements of Pacific Exploratory Mission-West (PEM-W) B have been analyzed to show latitudinal distributions (45 degrees N to 10 degrees S) of the mixing ratios of reactive nitrogen species (NO, peroxyacetylnitrate (PAN), HNO/sub 3/, and NO/sub y/), ozone, and chemical tracers (CO, NMHCs, acetone, and C/sub 2/Cl/sub 4/) with a focus on the upper troposphere. The Harvard global three-dimensional model of tropospheric chemistry has been used to compare these observations with predictions.
@article{
 title = {Latitudinal distribution of reactive nitrogen in the free troposphere over the Pacific Ocean in late winter/early spring},
 type = {article},
 year = {1998},
 keywords = {AD 1994 02 to 03,Acetone,Atmospheric composition,Chemical tracers,Early boreal spring,Ethene,Free troposphere,HNO/sub 3/,Harvard global 3D model,Late boreal winter,Latitudinal distribution,Mixing ratios,NO/sub y/,Nitrogen compounds,Nonmethane hydrocarbons,O/sub 3/,Ozone,Pacific Exploratory Mission-West B,Pacific Ocean,Peroxyacetylnitrate,Reactive nitrogen,Troposphere,Tropospheric chemistry,Upper troposphere,co,no,pan,pem-w b},
 pages = {28237-28246},
 volume = {103},
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 last_modified = {2015-02-12T20:22:17.000Z},
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 notes = {<m:note>Article<m:linebreak/>American Geophys. Union</m:note>},
 abstract = {The late boreal winter/early spring (February/March 1994) measurements of Pacific Exploratory Mission-West (PEM-W) B have been analyzed to show latitudinal distributions (45 degrees N to 10 degrees S) of the mixing ratios of reactive nitrogen species (NO, peroxyacetylnitrate (PAN), HNO/sub 3/, and NO/sub y/), ozone, and chemical tracers (CO, NMHCs, acetone, and C/sub 2/Cl/sub 4/) with a focus on the upper troposphere. The Harvard global three-dimensional model of tropospheric chemistry has been used to compare these observations with predictions.},
 bibtype = {article},
 author = {Singh, H B and Viezee, W and Chen, Y and Thakur, A N and Kondo, Y and Talbot, R W and Gregory, G L and Sachse, G W and Blake, D R and Bradshaw, J D and Wang, Y and Jacob, D J},
 journal = {Journal of Geophysical Research},
 number = {D21}
}

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