Long Range Transport of Air Pollution Into Norway - A Transfer Function Approach

Additional emissions of BrO during the time of the BrO event were observed from 31 March un- til 4 April in Kara Sea, on 1/2 April north of Hudson Bay and on 4/5 April near

3.2 Sulfate as a predominant component of the background Antarctic aerosol number population If the externally mixed sulfate mode observed in the AMS is, in fact, the primary

Results from TEPA ground stations, RCEC/ASNTU Lidar, and continually In- situ IC consistently showed that the transport of air pollutants was prior to the dust aerosol after the

Air parcel trajectories, computed directly from the balloon wind profiles, show three di ff erent transport pathways on 18–19 March: (a) high-altitude advection of the top of the

In the reference run (Fig. 8b), tracer particles are advected to- wards both ridges by upslope winds. Therefore, the largest tracer masses are found with up to 5. The AL and CBL

Airborne aerosol measurements in the central equatorial Pacific during PASE (Pacific Atmospheric Sul- fur Experiment) revealed that cloud condensation nuclei (CCN) activated in

The focus of this paper will be on the interannual variability of long-range transport of East Asian pollution (particularly CO) to the Northeast Pacific between spring 2005 5..

The principal component time series, and hence the phase of the NAO, is significantly correlated to North American CO tracer concentration anomalies over the northwestern At-