The Morning NO x maximum in the forest atmosphere boundary layer
Other literature type
Shepson, P. B.
Starn, T. K.
Jobson, B. T.
Wallace, H. W.
Carroll, M. A.
Bertman, S. B.
Edburg, S. L.
(issn: 1680-7324, eissn: 1680-7324)
During the 1998, 2000, 2001, 2008, and 2009 summer intensives of the Program
for Research on Oxidants: PHotochemistry, Emissions and Transport (PROPHET),
ambient measurement of nitrogen oxides (NO + NO<sub>2</sub> = NO<sub>x</sub>) were
conducted. NO and NO<sub>x</sub> mole fractions displayed a diurnal pattern with
NO<sub>x</sub> frequently highest in early morning. This pattern has often been
observed in other rural areas. In this paper, we discuss the potential sources and
contributing factors of the frequently observed morning pulse of NO<sub>x</sub>.
Of the possible potential contributing factors to the observed morning pulse of NO and NO<sub>x</sub>, we
find that surface-layer transport and slow upward mixing from soil
emissions, related to the thermodynamic stability in the nocturnal boundary
layer (NBL) before its morning breakup are the largest contributors. The
morning NO<sub>x</sub> peak can significantly impact boundary layer chemistry,
e.g. through production of HONO on surfaces, and by increasing the
importance of NO<sub>3</sub> chemistry in the morning boundary layer.