0000000000653601

AUTHOR

Desiree Toom

showing 3 related works from this author

Temporally delineated sources of major chemical species in high Arctic snow

2018

Long-range transport of aerosol from lower latitudes to the high Arctic may be a significant contributor to climate forcing in the Arctic. To identify the sources of key contaminants entering the Canadian High Arctic an intensive campaign of snow sampling was completed at Alert, Nunavut, from September 2014 to June 2015. Fresh snow samples collected every few days were analyzed for black carbon, major ions, and metals, and this rich data set provided an opportunity for a temporally refined source apportionment of snow composition via positive matrix factorization (PMF) in conjunction with FLEXPART (FLEXible PARTicle dispersion model) potential emission sensitivity analysis. Seven source fac…

Atmospheric Sciencefood.ingredient010504 meteorology & atmospheric sciences010501 environmental sciences01 natural scienceslcsh:Chemistrychemistry.chemical_compoundfoodNitrateSulfate0105 earth and related environmental sciencesSea salt15. Life on landRadiative forcingSnowlcsh:QC1-999AerosolArctic geoengineeringOceanographychemistryArcticlcsh:QD1-99913. Climate actionEnvironmental chemistryEnvironmental sciencelcsh:PhysicsAtmospheric Chemistry and Physics
researchProduct

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
researchProduct

Observations of Atmospheric Chemical Deposition to High Arctic Snow

2016

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 four days at Alert, Nunavut, from September 2014 to June 2015 were analyzed for black carbon, major ions, and metals, and their concentrations and fluxes reported. Comparison with simultaneous measurements of atmospheric aerosol mass loadings yields effective deposition velocities which encompass all processes by which the atmospheric species are transferred to the snow. It is …

13. Climate actionhuman activities
researchProduct