Dj. Wuebbles et al., New methodology for Ozone Depletion Potentials of short-lived compounds: n-propyl bromide as an example, J GEO RES-A, 106(D13), 2001, pp. 14551-14571
A number of the compounds proposed as replacements for substances controlle
d under the Montreal Protocol have extremely short atmospheric lifetimes, o
n the order of days to a few months. An important example is n-propyl bromi
de (also referred to as 1-bromopropane, CH2BrCH2CH3 or simplified as 1-C3H7
Br or nPB). This compound, useful as a solvent, has an atmospheric lifetime
of less than 20 days due to its reaction with hydroxyl. Because nPB contai
ns bromine, any amount reaching the stratosphere has the potential to affec
t concentrations of stratospheric ozone. The definition of Ozone Depletion
Potentials (ODP) needs to be modified for such short-lived compounds to acc
ount for the location and timing of emissions. It is not adequate to treat
these chemicals as if they were uniformly emitted at all latitudes and long
itudes as normally done for longer-lived gases. Thus, for short-lived compo
unds, policymakers will need a table of ODP values instead of the single va
lue generally provided in past studies. This study uses the MOZART2 three-d
imensional chemical-transport model in combination with studies with our le
ss computationally expensive two-dimensional model to examine potential eff
ects of nPB on stratospheric ozone. Multiple facets of this study examine k
ey questions regarding the amount of bromine reaching the stratosphere foll
owing emission of nPB. Our most significant findings from this study for th
e purposes of short-lived replacement compound ozone effects are summarized
as follows. The degradation of nPB produces a significant quantity of brom
oacetone which increases the amount of bromine transported to the stratosph
ere due to nPB. However, much of that effect is not due to bromoacetone its
elf, but instead to inorganic bromine which is produced from tropospheric o
xidation of nPB, bromoacetone, and other degradation products and is transp
orted above the dry and wet deposition processes of the model. The MOZART2
nPB results indicate a minimal correction of the two-dimensional results in
order to derive our final results: an nPB chemical lifetime of 19 days and
an Ozone Depletion Potential range of 0.033 to 0.040 for assumed global em
issions over landmasses, 19 days and 0.021 to 0.028, respectively, for assu
med emissions in the industrialized regions of the Northern Hemisphere, and
9 days and 0.087 to 0.105, respectively, for assumed emission in tropical
Southeast Asia.