Nb. Jones et al., Correlation of aerosol and carbon monoxide at 45 degrees S: Evidence of biomass burning emissions, GEOPHYS R L, 28(4), 2001, pp. 709-712
Altitude profiles of Carbon Monoxide (CO) and aerosols have been compared f
rom the Network for Stratospheric Change (NDSC) mid-latitude southern hemis
phere site at Lauder, New Zealand. The CO mixing ratio profile was derived
from infrared spectra recorded with a very high resolution Fourier Transfor
m interferometer using three lines of the (1-0) band between 2057 and 2160
cm(-1). The aerosol surface area was derived from balloon-borne backscatter
radiation at 940 nm. Both datasets show significant enhancements occurring
over the observation site in the austral spring;. When displayed together
their combined effect illustrates the close correlation between CO and aero
sols. Peak concentrations are consistently recorded between September and O
ctober over a five year time frame (1994-1999), with the enhancements typic
ally occurring at heights of between 3 to 8 km. The temporal and spatial co
rrelation between the aerosol plumes and enhanced CO concentrations are int
erpreted in terms of the effect of long range transport of biomass burning:
plumes in combination with the: Fl Nine-Southern Oscillation (ENSO) cycles
influence on southern hemisphere climate dynamics.