Ann‐Lise Norman

ORCID: 0000-0002-5430-7409
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About
Contact & Profiles
Research Areas
  • Atmospheric chemistry and aerosols
  • Atmospheric and Environmental Gas Dynamics
  • Atmospheric Ozone and Climate
  • Atmospheric aerosols and clouds
  • Arctic and Antarctic ice dynamics
  • Air Quality and Health Impacts
  • Groundwater and Isotope Geochemistry
  • Marine and coastal ecosystems
  • Oil Spill Detection and Mitigation
  • Ocean Acidification Effects and Responses
  • Toxic Organic Pollutants Impact
  • Fire effects on ecosystems
  • Methane Hydrates and Related Phenomena
  • Isotope Analysis in Ecology
  • Air Quality Monitoring and Forecasting
  • Vehicle emissions and performance
  • Industrial Gas Emission Control
  • Maritime Transport Emissions and Efficiency
  • Coastal and Marine Management
  • Hydrocarbon exploration and reservoir analysis
  • Odor and Emission Control Technologies
  • Climate change and permafrost
  • Cryospheric studies and observations
  • Petroleum Processing and Analysis
  • Marine Bivalve and Aquaculture Studies

University of Calgary
2014-2025

University of Guelph
2017

Memorial University of Newfoundland
2006

Stratford Hospital
1976

Bellevue Hospital Center
1976

American Geophysical Union
1976

University of Arizona
1971

ADVERTISEMENT RETURN TO ISSUEPREVArticleNEXTOnline Sulfur-Isotope Determination Using an Elemental Analyzer Coupled to a Mass SpectrometerA. Giesemann, H.-J. Jaeger, A. L. Norman, H. R. Krouse, and W. BrandCite this: Anal. Chem. 1994, 66, 18, 2816–2819Publication Date (Print):September 15, 1994Publication History Published online1 May 2002Published inissue 15 September 1994https://pubs.acs.org/doi/10.1021/ac00090a005https://doi.org/10.1021/ac00090a005research-articleACS PublicationsRequest...

10.1021/ac00090a005 article EN Analytical Chemistry 1994-09-15

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

10.5194/acp-19-2527-2019 article EN cc-by Atmospheric chemistry and physics 2019-02-28

Abstract One year of aerosol particle observations from Alert, Nunavut shows that new formation (NPF) is common during clean periods the summertime Arctic associated with attendant low condensation sinks and presence methane sulfonic acid (MSA), a product atmospheric oxidation dimethyl sulfide (DMS). The time periods, defined using distribution refractory black carbon number concentrations, increase in frequency June through August as anthropogenic influence dwindles. During concentrations...

10.12952/journal.elementa.000017 article EN cc-by Elementa Science of the Anthropocene 2013-11-26

The recent decline in sea ice cover the Arctic Ocean could affect regional radiative forcing via changes ice–atmosphere exchange of dimethyl sulfide (DMS) and biogenic aerosols formed from its atmospheric oxidation, such as methanesulfonic acid (MSA). This study examines relationships between total extent north 70°N MSA measurement at Alert, Nunavut, during 1980–2009; Barrow, Alaska, 1997–2008; Ny‐Ålesund, Svalbard, for 1991–2004. During 1980–1989 1990–1997 periods, summer (July–August) June...

10.1029/2011jd017074 article EN Journal of Geophysical Research Atmospheres 2012-05-22

Abstract. Size-segregated aerosol sulfate concentrations were measured on board the Canadian Coast Guard Ship (CCGS) Amundsen in Arctic during July 2014. The objective of this study was to utilize isotopic composition address contribution anthropogenic and biogenic sources aerosols growth different size fractions atmosphere. Non-sea-salt is divided into using stable isotope apportionment techniques. A considerable amount average concentration fine with a diameter < 0.49 µm from (> 63...

10.5194/acp-16-5191-2016 article EN cc-by Atmospheric chemistry and physics 2016-04-26

Abstract. Dimethylsulfide (DMS), outgassed from ocean waters, plays an important role in the climate system, as it oxidizes to methane sulfonic acid (MSA) and sulfur dioxide (SO2), which can lead formation of sulfate aerosol. Newly formed aerosol resulting DMS oxidation may grow by condensation gases, in-cloud oxidation, coagulation sizes where they act cloud nuclei (CCN) influence properties. Under future global warming conditions, sea ice Arctic region is expected decline significantly,...

10.5194/acp-19-6419-2019 article EN cc-by Atmospheric chemistry and physics 2019-05-16

From July 1993 to September 1994, seasonal variations in the sources of SO 4 2− aerosols Arctic lower atmosphere at Alert, Canada, (82°30′N, 62°20′W) were investigated using sulphur isotope abundance as little 10 μg analyzed by combustion‐flow isotope‐ratio mass spectrometry. In conjunction with air trajectories and parallel measurements aerosol composition, composition was used discern . Total is composed sea‐salt , marine biogenic, nonmarine June through fraction biogenic non‐sea‐salt...

10.1029/1999jd900078 article EN Journal of Geophysical Research Atmospheres 1999-05-01

In the agriculture sector, crop production and on-farm fuel use are two main sources of greenhouse gas emissions (GHGs) apart from enteric fermentation. The application conventional synthetic fertilizer for can help to increase yields, but also results in nitrous oxide emissions, polluting waterways, deterioration soil health including damages structure, changes pH, as well decreases carbon content microbial diversity. Most farm machinery is powered by diesel which emits dioxide other air...

10.2139/ssrn.5069952 article EN SSRN Electronic Journal 2025-01-01

[1] Dimethyl sulfide (DMS) and its oxidation products, which have been proposed to provide a climate feedback mechanism by affecting aerosol cloud radiative properties, were measured on board the Canadian Coast Guard ship Amundsen in sampling campaigns Arctic fall of 2007 2008. DMS flux was calculated based surface water measurements yielded 0.1–2.6 μmol m−2 d−1 along Northwest Passage 0.2–1.3 Baffin Bay sulfur dioxide (SO2), methane sulfonic acid (MSA), sulfate aerosols also measured. The...

10.1029/2011jd016336 article EN Journal of Geophysical Research Atmospheres 2011-10-31

Abstract. Atmospheric dimethyl sulfide, DMS(g), is a climatically important sulfur compound and the main source of biogenic sulfate aerosol in Arctic atmosphere. DMS(g) production emission to atmosphere increase during summer due greater ice-free sea surface higher biological activity. We implemented Environment Climate Change Canada’s (ECCC) online air quality forecast model, GEM-MACH (Global Environmental Multiscale–Modelling Air CHemistry), compared model simulations with measurements...

10.5194/acp-19-14455-2019 article EN cc-by Atmospheric chemistry and physics 2019-11-29

10.1023/a:1016105030624 article EN Journal of Atmospheric Chemistry 2002-01-01

Contributions to atmospheric sulphate aerosol and precipitation in the Fraser Valley at Saturna Island, Canada, from oxidation of biogenic dimethyl sulphide were determined using an isotopic mass balance approach. The S‐isotope composition sulphate, sulphur dioxide a variety industrial sources region investigated found have δ 34 S values ranging between −1.6 +9‰. Isotopic analysis suggests U.S. oil refinery and/or H 2 tidal flats on coast contributes load both summer winter. On average,...

10.1029/2002jd003072 article EN Journal of Geophysical Research Atmospheres 2004-03-12

Stable isotope compositions of hydrogen and oxygen for continental condensates are determined foremost by equilibrium kinetic fractionation during evaporation at the oceanic source regions. Subsequently they modified a series in-cloud processes, which include condensation possible admixture vapour from transpiration over continents. The effects on (δ2H) (δ18O) local precipitation discussed in this paper. Using Rayleigh model, described both constant stepwise fluxes. Further, deuterium...

10.3402/tellusb.v57i4.16545 article EN Tellus B 2005-01-01

Firn air and ice have been sampled analyzed for trace gases (CO 2 , N O, CH 4 CO) isotopes ( 14 C, 13 18 O of CO ; 3 H ice) at m intervals from the surface to depth closure 60 on Devon Island Ice Cap, a low‐elevation permanent glacier in Canadian Arctic Islands, investigate firn diffusion effects summer melting. The profile permeable includes 1963 thermonuclear peak 53.9 ± 1.5 m. twofold increase rapid decay that characterize recent atmospheric history provide robust scenario is used with...

10.1029/2006jd007471 article EN Journal of Geophysical Research Atmospheres 2007-01-03

Sulfur (S) isotopes have been used to apportion the amount of biogenic and anthropogenic sulfate in remote environments, an important parameter that is model global radiation budget. A key assumption apportionment calculations there little isotope selectivity as reduced compounds such dimethyl sulfide (DMS) are oxidized. This paper describes a method determine, for first time, S composition methanesulfonic acid (MSA), product DMS oxidation. The MSA was measured directly by EA-IRMS reference...

10.1021/ac0600048 article EN Analytical Chemistry 2006-06-15

Agricultural soils are the dominant contributor to increases in atmospheric nitrous oxide (N 2 O). Few studies have investigated natural N and O isotopic composition of soil O. We collected gas samples using horizontal sampling tubes installed at successive depths under five contrasting agricultural crops (e.g., unamended alfalfa, fertilized cereal), tropospheric air samples. Mean δ 15 18 values ranged from −28.0 +8.9‰, +29.0 +53.6‰. The mean were +4.6 ± 0.7‰ +48.3 0.2‰, respectively. In...

10.1029/2006jd008330 article EN Journal of Geophysical Research Atmospheres 2007-09-18

Abstract The influence of frost flowers and seawater brine on ion chemistry in snow, snowpack, ice cores, aerosols is detected when a lower sulfate to sodium ratio than present polar regions. This evidence can be masked large amounts non‐sea‐salt are from other sources such as biogenic anthropogenic sulfate. Frost flower δ 34 S values were measured for the first time sulfates did not differ significantly sea salt +21‰. A method using stable isotopes introduced determine limit contributions...

10.1002/2013jd020461 article EN Journal of Geophysical Research Atmospheres 2014-01-04

Abstract. Maintaining consistent traceability of high-precision measurements CO2 isotopes is critical in order to obtain accurate atmospheric trends δ13C and δ18O (in CO2). Although a number laboratories/organizations around the world have been conducting baseline for several decades, reports on maintenance are rare. In this paper, principle an approach maintaining isotope (δ13C δ18O) described. The concept Big Delta introduced its role described discussed extensively. uncertainties...

10.5194/amt-6-1685-2013 article EN cc-by Atmospheric measurement techniques 2013-07-17

The early atmospheric detection of carbon dioxide (CO2) leaks from capture and storage (CCS) sites is important both to inform remediation efforts build maintain public support for CCS in mitigating greenhouse gas emissions. A analysis system was developed assess the origin plumes air enriched CO2, as whether CO2 a site or oxidation compounds. measured O2 concentrations different plume samples relative background calculated differential concentration ratio (GDCR = −ΔO2/ΔCO2). experimental...

10.1080/10962247.2016.1176084 article EN Journal of the Air & Waste Management Association 2016-04-22
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