0000000000038563

AUTHOR

Sangeeta Sharma

showing 9 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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Vertical profile of atmospheric dimethyl sulfide in the Arctic Spring and Summer

2017

Abstract. Vertical distributions of atmospheric dimethyl sulfide (DMS(g)) were sampled aboard the research aircraft Polar 6 near Lancaster Sound, Nunavut, Canada in July 2014 and on pan-Arctic flights in April 2015 that started from Longyearbyen, Spitzbergen, and passed through Alert and Eureka, Nunavut and Inuvik, Northwest Territories. Larger mean DMS(g) mixing ratios were present during April 2015 (campaign-mean of 116±8 pptv) compared to July 2014 (campaign-mean of 20±6 pptv). Observations in July 2014 indicated a decrease in DMS(g) mixing ratios with altitude up to about 3 km, and the largest mixing ratios were found near the surface above ice-edge and open water, coincident with incre…

geographygeography.geographical_feature_categorychemistry.chemical_compoundAltitudeOceanographychemistryArcticArchipelagoEnvironmental scienceDimethyl sulfideSeawaterBaySound (geography)Air mass
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Boundary layer and free-tropospheric dimethyl sulfide in the Arctic spring and summer

2017

Vertical distributions of atmospheric dimethyl sulfide (DMS(g)) were sampled aboard the research aircraft Polar 6 near Lancaster Sound, Nunavut, Canada, in July 2014 and on pan-Arctic flights in April 2015 that started from Longyearbyen, Spitzbergen, and passed through Alert and Eureka, Nunavut, and Inuvik, Northwest Territories. Larger mean DMS(g) mixing ratios were present during April 2015 (campaign mean of 116  ±  8 pptv) compared to July 2014 (campaign mean of 20  ±  6 pptv). During July 2014, the largest mixing ratios were found near the surface over the ice edge and open water. DMS(g) mixing ratios decreased with altitude up to about 3 km. During April 2015, profiles of DMS(g) were m…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric Science010504 meteorology & atmospheric sciencesChemical transport model010501 environmental sciences01 natural scienceslcsh:QC1-999lcsh:ChemistryTropospherechemistry.chemical_compoundOceanographyAltitudelcsh:QD1-999chemistryArctic13. Climate actionEnvironmental scienceSeawaterDimethyl sulfide[PHYS.PHYS.PHYS-CHEM-PH]Physics [physics]/Physics [physics]/Chemical Physics [physics.chem-ph]Baylcsh:PhysicsAir mass0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Modelling Regional Air Quality in the Canadian Arctic: Simulation of an Arctic Summer Field Campaign

2017

Model simulations of an Arctic summer field campaign were carried out. The model results were compared with observational data from both ground-based monitoring and in situ measurements on-board multiple mobile platforms. The model was able to well capture regional sources and transport affecting the Arctic air quality. It is shown that the study area was impacted by North American (NA) regional biomass burning emissions. The model-observation comparison also corroborates previous findings on possible roles of marine-biogenic sources in aerosol production in the Arctic MBL during summertime.

010504 meteorology & atmospheric sciencesArcticClimatologyEnvironmental scienceAtmospheric sciencesBiomass burning01 natural sciencesAir quality indexgeographic locationsField campaign0105 earth and related environmental sciencesAerosolThe arctic
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New insights into aerosol and climate in the Arctic

2018

Abstract. Motivated by the need to predict how the Arctic atmosphere will change in a warming world, this article summarizes recent advances made by the research consortium NETCARE (Network on Climate and Aerosols: Addressing Key Uncertainties in Remote Canadian Environments) that contribute to our fundamental understanding of Arctic aerosol particles as they relate to climate forcing. The overall goal of NETCARE research has been to use an interdisciplinary approach encompassing extensive field observations and a range of chemical transport, earth system, and biogeochemical models. Several major findings and advances have emerged from NETCARE since its formation in 2013 . (1) Unexpectedly …

0301 basic medicineArctic haze010504 meteorology & atmospheric sciences15. Life on landMineral dustAtmospheric sciences01 natural sciencesSea surface microlayerAerosol03 medical and health sciences030104 developmental biologyDeposition (aerosol physics)Arctic13. Climate actionMelt pondIce nucleusEnvironmental science0105 earth and related environmental sciences
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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
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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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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
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High gas-phase mixing ratios of formic and acetic acid in the High Arctic

2018

Abstract. Formic and acetic acid are ubiquitous and abundant in the Earth's atmosphere and are important contributors to cloud water acidity, especially in remote regions. Their global sources are not well understood, as evidenced by the inability of models to reproduce the magnitude of measured mixing ratios, particularly at high northern latitudes. The scarcity of measurements at those latitudes is also a hindrance to understanding these acids and their sources. Here, we present ground-based gas-phase measurements of formic acid (FA) and acetic acid (AA) in the Canadian Arctic collected at 0.5 Hz with a high-resolution chemical ionization time-of-flight mass spectrometer using the iodide …

Atmospheric ScienceChemical ionization010504 meteorology & atmospheric sciencesChemical transport modelChemistryFormic acid010501 environmental sciences01 natural scienceslcsh:QC1-999lcsh:ChemistryAtmosphereAcetic acidchemistry.chemical_compoundOvercastlcsh:QD1-999ArcticReagentEnvironmental chemistrylcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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