TY - JOUR
T1 - Modelling the partitioning of ammonium nitrate in the convective boundary layer
AU - Aan de Brugh, J.M.J.
AU - Henzing, J.S.
AU - Schaap, M.
AU - Morgan, W.T.
AU - Coe, H.
AU - Krol, M.C.
PY - 2011
Y1 - 2011
N2 - Aerosols have a pronounced influence on the climate system, both directly by scattering
and absorbing incoming solar radiation (Hess et al., 1998; Haywood and Boucher,
2000; IPCC, 2007) and indirectly by altering cloud properties (Rosenfeld et al., 2008;
5 Kaufman et al., 2002). The combined climate effect of aerosols is poorly understood
compared to the climate effect of greenhouse gases. In the Netherlands, nearly half
(42 %–48 %) of the fine aerosol (PM2.5) mass consists of secondary inorganic aerosols
(ammonium nitrate and ammonium sulphate) (Weijers et al., 2011), which are the dominant
anthropogenic aerosol species in the size range with maximum light scattering
10 (0.4–1.0 μm) (ten Brink et al., 1997). Also, these secondary inorganic aerosols are
effective cloud condensation nuclei, because of their size and water solubility. Due to
intensive agriculture, the ammonia concentrations in the Netherlands have always been
sufficiently high to neutralise sulphuric and nitric acid. During the last twenty-five years,
sulphur dioxide emissions have decreased much more than those of nitrogen oxides
15 in Europe and especially in the Netherlands (Vestreng et al., 2007, 2009). Therefore,
ammonium nitrate has become increasingly important in comparison to ammonium
sulphate. There are two major physical differences between ammonium nitrate
and ammonium sulphate. First, the water uptake by ammonium nitrate aerosol depends
stronger on the ambient humidity than the water uptake by ammonium sulphate
20 aerosol (Tang, 1996). Hygroscopic growth of aerosols evidently affects the interaction
with solar radiation. Second, ammonium nitrate resides in both the gas phase and in
the aerosol phase while ammonium sulphate resides exclusively in the aerosol phase.
The equilibrium between the gas phase and the aerosol phase depends strongly on
temperature and relative humidity. As a result, the interaction of ammonium nitrate
25 with solar radiation is much stronger at lower temperatures and higher relative humidities.
With ammonium nitrate becoming increasingly important, systematic investigation
of these properties seems appropriate.
AB - Aerosols have a pronounced influence on the climate system, both directly by scattering
and absorbing incoming solar radiation (Hess et al., 1998; Haywood and Boucher,
2000; IPCC, 2007) and indirectly by altering cloud properties (Rosenfeld et al., 2008;
5 Kaufman et al., 2002). The combined climate effect of aerosols is poorly understood
compared to the climate effect of greenhouse gases. In the Netherlands, nearly half
(42 %–48 %) of the fine aerosol (PM2.5) mass consists of secondary inorganic aerosols
(ammonium nitrate and ammonium sulphate) (Weijers et al., 2011), which are the dominant
anthropogenic aerosol species in the size range with maximum light scattering
10 (0.4–1.0 μm) (ten Brink et al., 1997). Also, these secondary inorganic aerosols are
effective cloud condensation nuclei, because of their size and water solubility. Due to
intensive agriculture, the ammonia concentrations in the Netherlands have always been
sufficiently high to neutralise sulphuric and nitric acid. During the last twenty-five years,
sulphur dioxide emissions have decreased much more than those of nitrogen oxides
15 in Europe and especially in the Netherlands (Vestreng et al., 2007, 2009). Therefore,
ammonium nitrate has become increasingly important in comparison to ammonium
sulphate. There are two major physical differences between ammonium nitrate
and ammonium sulphate. First, the water uptake by ammonium nitrate aerosol depends
stronger on the ambient humidity than the water uptake by ammonium sulphate
20 aerosol (Tang, 1996). Hygroscopic growth of aerosols evidently affects the interaction
with solar radiation. Second, ammonium nitrate resides in both the gas phase and in
the aerosol phase while ammonium sulphate resides exclusively in the aerosol phase.
The equilibrium between the gas phase and the aerosol phase depends strongly on
temperature and relative humidity. As a result, the interaction of ammonium nitrate
25 with solar radiation is much stronger at lower temperatures and higher relative humidities.
With ammonium nitrate becoming increasingly important, systematic investigation
of these properties seems appropriate.
U2 - 10.5194/acpd-11-28273-2011
DO - 10.5194/acpd-11-28273-2011
M3 - Article
SN - 1680-7375
VL - 11
SP - 28273
EP - 28317
JO - Atmospheric Chemistry and Physics Discussions
JF - Atmospheric Chemistry and Physics Discussions
ER -