0000000000038557

AUTHOR

Allan K. Bertram

0000-0002-5621-2323

showing 4 related works from this author

Concentrations, composition, and sources of ice-nucleating particles in the Canadian High Arctic during spring 2016

2019

Modelling studies suggest that the climate and the hydrological cycle are sensitive to the concentrations of ice-nucleating particles (INPs). However, the concentrations, composition, and sources of INPs in the atmosphere remain uncertain. Here, we report daily concentrations of INPs in the immersion freezing mode and tracers of mineral dust (Al, Fe, Ti, and Mn), sea spray aerosol (Na+ and Cl−), and anthropogenic aerosol (Zn, Pb, NO3-, NH4+, and non-sea-salt SO42-) at Alert, Canada, during a 3-week campaign in March 2016. In total, 16 daily measurements of INPs are reported. The average INP concentrations measured in the immersion freezing mode were 0.005±0.002, 0.020±0.004, and 0.186±0.040…

Atmospheric Scienceeducation.field_of_study010504 meteorology & atmospheric sciencesChemistryPopulation010501 environmental sciencesMineral dustSea spray01 natural scienceslcsh:QC1-999AerosolAtmospherelcsh:ChemistryArcticlcsh:QD1-999Environmental chemistryParticleeducationSea levellcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Frequent Ultrafine Particle Formation and Growth in the Canadian Arctic Marine Environment

2017

Abstract. The source strength and capability of aerosol particles in the Arctic to act as cloud condensation nuclei have important implications for understanding the indirect aerosol-cloud effect within the polar climate system. It has been shown in several Arctic regions that ultrafine particle (UFP) formation and growth is a key contributor to aerosol number concentrations during the summer. This study uses aerosol number size distribution measurements from ship-board measurement expeditions aboard the research icebreaker CCGS Amundsen in the summers of 2014 and 2016 throughout the Canadian Arctic to gain a deeper understanding of the drivers of UFP formation and growth within this marine…

0301 basic medicinegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAtmospheric sciences01 natural sciencesSink (geography)LatitudeAerosol03 medical and health sciences030104 developmental biologyArctic13. Climate actionUltrafine particleSea iceCloud condensation nucleiEnvironmental science14. Life underwaterPolar climate0105 earth and related environmental sciences
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Observations of atmospheric chemical deposition to high Arctic snow

2017

Abstract. Rapidly rising temperatures and loss of snow and ice cover have demonstrated the unique vulnerability of the high Arctic to climate change. There are major uncertainties in modelling the chemical depositional and scavenging processes of Arctic snow. To that end, fresh snow samples collected on average every 4 days at Alert, Nunavut, from September 2014 to June 2015 were analyzed for black carbon, major ions, and metals, and their concentrations and fluxes were reported. Comparison with simultaneous measurements of atmospheric aerosol mass loadings yields effective deposition velocities that encompass all processes by which the atmospheric species are transferred to the snow. It is…

Atmospheric Science010504 meteorology & atmospheric sciencesClimate changeCarbon black010501 environmental sciencesAtmospheric sciencesSnow01 natural scienceslcsh:QC1-999AerosolSedimentary depositional environmentlcsh:ChemistryDeposition (aerosol physics)Arcticlcsh:QD1-99913. Climate actionClimatologyEnvironmental scienceScavenginghuman activitieslcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Frequent ultrafine particle formation and growth in Canadian Arctic marine and coastal environments

2017

The source strength and capability of aerosol particles in the Arctic to act as cloud condensation nuclei have important implications for understanding the indirect aerosol–cloud effect within the polar climate system. It has been shown in several Arctic regions that ultrafine particle (UFP) formation and growth is a key contributor to aerosol number concentrations during the summer. This study uses aerosol number size distribution measurements from shipboard expeditions aboard the research icebreaker CCGS Amundsen in the summers of 2014 and 2016 throughout the Canadian Arctic to gain a deeper understanding of the drivers of UFP formation and growth within this marine boundary layer. UFP nu…

Atmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences010501 environmental sciences01 natural scienceslcsh:QC1-999Sink (geography)AerosolLatitudelcsh:ChemistryOceanographylcsh:QD1-999Arctic13. Climate actionUltrafine particleSea iceEnvironmental scienceCloud condensation nuclei14. Life underwaterlcsh:PhysicsPolar climate0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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