D Simpson, A Benedictow, H Berge… - Atmospheric …, 2012 - acp.copernicus.org
The Meteorological Synthesizing Centre-West (MSC-W) of the European Monitoring and Evaluation Programme (EMEP) has been performing model calculations in support of the …
Forests cover nearly a third of the Earth's land area and exchange mass, momentum, and energy with the atmosphere. Most studies of these exchanges, particularly using numerical …
Dry deposition is an important loss process for atmospheric particles and can be a significant part of total deposition estimates calculated for critical loads analyses. However …
Reactive nitrogen (N r) compounds have different fates in the atmosphere due to differences in the governing processes of physical transport, deposition and chemical transformation. N …
EW Emerson, JM Katich, JP Schwarz… - Journal of …, 2018 - Wiley Online Library
The atmospheric lifetime of black carbon (BC) is controlled by wet and dry deposition, which are poorly constrained by observations. We show that the single‐particle soot photometer …
In the first half of the twentieth century the measurement of rates of exchange of momentum, heat, and especially water between the terrestrial surface and the atmosphere was an …
A Petroff, L Zhang, SC Pryor, Y Belot - Journal of Aerosol Science, 2009 - Elsevier
This paper presents a model to predict transport and dry deposition of aerosols in and to a canopy composed of plane leaves such as a grassland, a crop field or a broadleaf forest …
Frameworks for limiting ecosystem exposure to excess nutrients and acidity require accurate and complete deposition budgets of reactive nitrogen (Nr). While much progress has been …
The removal of ultrafine particles (UFP) by vegetation is now receiving significant attention given their role in cloud physics, human health and respiratory related diseases. Vegetation …