Open AccessSeasonal budgets of reactive nitrogen species and ozone over the United States, and export fluxes to the global atmosphere
Author(s) -
Liang Jinyou,
Horowitz Larry W.,
Jacob Daniel J.,
Wang Yuhang,
Fiore Arlene M.,
Logan Jennifer A.,
Gardner Geraldine M.,
Munger J. William
Publication year - 1998
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/97jd03126
Subject(s) - boundary layer , reactive nitrogen , atmospheric sciences , seasonality , ozone , isoprene , atmosphere (unit) , sink (geography) , environmental science , chemical transport model , nitrogen , planetary boundary layer , aerosol , troposphere , climatology , chemistry , geology , meteorology , geography , physics , ecology , thermodynamics , cartography , organic chemistry , biology , copolymer , polymer
A three‐dimensional, continental‐scale photochemical model is used to investigate seasonal budgets of O 3 and NO y species (including NO x and its oxidation products) in the boundary layer over the United States and to estimate the export of these species from the U.S. boundary layer to the global atmosphere. Model results are evaluated with year‐round observations for O 3 , CO, and NO y species at nonurban sites. A seasonal transition from NO x to hydrocarbon‐limited conditions for O 3 production over the eastern United States is found to take place in the fall, with the reverse transition taking place in the spring. The mean NO x /NO y molar ratio in the U.S. boundary layer in the model ranges from 0.2 in summer to 0.6 in winter, in accord with observations, and reflecting largely the seasonal variation in the chemical lifetime of NO x . Formation of hydroxy organic nitrates during oxidation of isoprene, followed by decomposition of these nitrates to HNO 3 , is estimated to account for 30% of the chemical sink of NO x in the U.S. boundary layer in summer. Model results indicate that peroxyacylnitrates (PANs) are most abundant in the U.S. boundary layer in spring (25% of total NO y .), reflecting a combination of active photochemistry and low temperatures. About 20% of the NO x emitted from fossil fuel combustion in the United States in the model is exported out of the U.S. boundary layer as NO x or PANs (15% in summer, 25% in winter). This export responds less than proportionally to changes in NO x emissions in summer, but more than proportionally in winter. The annual mean export of NO x and PANs from the U.S. boundary layer is estimated to be 1.4 Tg N yr −1 , representing an important source of NO x on the scale of the northern hemisphere troposphere. The eventual O 3 production in the global troposphere due to the exported NO x and PANs is estimated to be twice as large, on an annual basis, as the direct export of O 3 pollution from the U.S. boundary layer. Fossil fuel combustion in the United States is estimated to account for about 10% of the total source of O 3 in the northern hemisphere troposphere on an annual basis.