English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Carbon particulate matter constitutes an important portion of the atmospheric aerosol and directly participates in the for- mation of the Earth's radiation balance by inuencing the global and regional climate. Continuous data (March, April, 2002) of 20-minute concentrations of airborne black carbon (BC) particles at the Preila Environmental Pollution Research Station (55-200 N, 21-000 E) have been used for the investigation of diurnal and weekday variation as well as the different air mass inuence on BC transport. The measurement of BC mass concentration with the AethalometerTM, Model AE40 Spectrum, manufactured by Optotek, Slovenia was carried out. The origin of an air mass was detected by using air mass backward tra- jectories calculated by the Hybrid Single-Particle Lagrangian Integrated Trajectories (HYSPLIT) model. Approximately 73% of BC measured concentrations were found in the range of a low value mode centered at »0ñ1000 ng m¡3. The remaining concentrations were in a high-concentration mode at »1000ñ3000 ng m¡3, probably indicating a direct impact of emissions from combustion activities. BC concentration in various air masses over that period varied from the average value of approxi- mately 140 ng m¡3 to the maximum value of 2410 ng m¡3. The highest BC concentrations were associated with the prevailing southern transport air masses. Simultaneously, the daily concentration variation of black carbon and SO2, NO2, O3 was mea- sured and analysed. Total aerosol concentrations and size distributions were measured as well. The aerosol size distribution was plotted as contour plots for each day (as a function of time). Most studies were focused on the BC aerosol particle size distribution and modal aerosol concentration. For each event, the growth rate was calculated graphically from the contour plots (ìbananañplotsî) and was analysed for the possible nucleation events. Some aerosol measurements were carried out at an urban site in order to evaluate the BC concentration of the freshly emitted trafc aerosols.

Black carbon aerosol at the background site in the coastal zone of the Baltic Sea