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From:Atmospheric Chemistry and Physics (Vol. 22, Issue 5) Peer-Reviewed
Atmospheric composition in the European Arctic and 30 years of the Zeppelin Observatory, Ny-Ãlesund.
The Zeppelin Observatory (78.90.sup." N, 11.88.sup." E) is located on Zeppelin Mountain at 472 m a.s.l. on Spitsbergen, the largest island of the Svalbard archipelago. Established in 1989, the observatory is part of... -
From:Atmospheric Measurement Techniques (Vol. 14, Issue 10) Peer-ReviewedLong-term measurements of atmospheric mass concentrations of black carbon (BC) are needed to investigate changes in its emission, transport, and deposition. However, depending on instrumentation, parameters related to BC...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 17) Peer-ReviewedThe scattering and backscattering enhancement factors (f(RH) and f.sub.b (RH)) describe how aerosol particle light scattering and backscattering, respectively, change with relative humidity (RH). They are important...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 3) Peer-Reviewed
The Nordic Centre of Excellence CRAICC (Cryosphere-Atmosphere Interactions in a Changing Arctic Climate), funded by NordForsk in the years 2011-2016, is the largest joint Nordic research and innovation initiative to...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 21) Peer-ReviewedThe study of long-term trends in aerosol optical properties is an important task to understand the underlying aerosol processes influencing the change of climate. The Arctic, as the place where climate change manifests...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 14) Peer-ReviewedIn order to assess the evolution of aerosol parameters affecting climate change, a long-term trend analysis of aerosol optical properties was performed on time series from 52 stations situated across five continents. The...
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From:Bulletin of the American Meteorological Society (Vol. 101, Issue 4) Peer-ReviewedThe sea surface microlayer (SML) occupies the uppermost tens to hundreds of micrometers of the ocean surface. Consequently, it is in direct contact with the atmosphere and covers around 70% of Earth's surface. Compared...
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From:Atmospheric Measurement Techniques (Vol. 9, Issue 8) Peer-ReviewedIn the companion (Part I) paper, we have described and evaluated a new versatile optical particle counter/sizer named LOAC (Light Optical Aerosol Counter), based on scattering measurements at angles of 12 and 60°....
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 3) Peer-Reviewed
Water in the atmosphere can exist in the solid, liquid or gas phase. At high humidities, if the aerosol population remains constant, more water vapour will condense onto the particles and cause them to swell,...
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From:Atmospheric Measurement Techniques (Vol. 9, Issue 4) Peer-ReviewedThe study of aerosols in the troposphere and in the stratosphere is of major importance both for climate and air quality studies. Among the numerous instruments available, optical aerosol particles counters (OPCs)...
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From:Atmospheric Measurement Techniques (Vol. 13, Issue 8) Peer-ReviewedAerosol particles are essential constituents of the Earth's atmosphere, impacting the earth radiation balance directly by scattering and absorbing solar radiation, and indirectly by acting as cloud condensation nuclei....
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 17) Peer-ReviewedThe uptake of water by atmospheric aerosols has a pronounced effect on particle light scattering properties, which in turn are strongly dependent on the ambient relative humidity (RH). Earth system models need to account...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 11) Peer-ReviewedTo constrain uncertainties in radiative forcings associated with aerosol-cloud interactions, improved understanding of Arctic cloud formation is required, yet long-term measurements of the relevant cloud and aerosol...