The new report “Global Linkages – A graphic look at the changing Arctic”, produced by UN Environment and its collaborating center GRID-Arendal, is a set of maps and graphics, accompanied by short...
The new report “Global Linkages – A graphic look at the changing Arctic”, produced by UN Environment and its collaborating center GRID-Arendal, is a set of maps and graphics, accompanied by short...
On March 15 Sweden presented the "Report for Sweden on assessment of projected progress, March 2017", which provides information on implemented policies and measures and projections of...
This document was prepared in accordance with the Reform Plan of the Environment for Europe process as a proposed outcome of the Eighth Environment for Europe Ministerial Conference. It contains...
This report summarizes the current scientific knowledge on transboundary air pollution issues within the United Nations Economic Commission for Europe region and describes the effectiveness of air...
Abstract - Several studies show that a significant portion of daily air pollution exposure, in particular black carbon (BC), occurs during transport. In a previous work, a model for the in-traffic...
This paper focused on modelling Black Carbon (BC) concentrations in two busy street canyons, the Crown and Belliard Street in Brussels. The used original Operational Street Pollution Model was...
Recently, short-term monitoring campaigns have been carried out to investigate the spatial variation of air pollutants within cities. Typically, such campaigns are based on short-term measurements...
The presence of black carbon, and size-resolved and total particle number concentrations (PNC) were investigated in the vicinity of Schiphol airport in the Netherlands, the fourth busiest airport...
Though many global aerosols models prognose surface deposition, only a few models have been used to directly simulate the radiative effect from black carbon (BC) deposition to snow and sea ice....
The Arctic is a region in transformation. Warming in the region has been amplified, as expected from ice-albedo feedback effects, with the rate of warming observed to be ∼0.60 ±...