Megan D. Willis

ORCID: 0000-0003-0386-0156
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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
  • Air Quality and Health Impacts
  • Arctic and Antarctic ice dynamics
  • Mass Spectrometry Techniques and Applications
  • Air Quality Monitoring and Forecasting
  • Vehicle emissions and performance
  • Hydrocarbon exploration and reservoir analysis
  • Advanced Chemical Sensor Technologies
  • Methane Hydrates and Related Phenomena
  • Analytical Chemistry and Chromatography
  • Marine and coastal ecosystems
  • Cryospheric studies and observations
  • Catalytic Processes in Materials Science
  • Climate change and permafrost
  • Spectroscopy and Quantum Chemical Studies
  • Maritime Transport Emissions and Efficiency
  • Analytical chemistry methods development
  • Toxic Organic Pollutants Impact
  • Electrohydrodynamics and Fluid Dynamics
  • Molecular Junctions and Nanostructures
  • Innovative Microfluidic and Catalytic Techniques Innovation
  • Spectroscopy and Laser Applications

Colorado State University
2021-2025

Zero to Three
2023

Colorado State University System
2022

University of Toronto
2014-2021

Lawrence Berkeley National Laboratory
2018-2020

Berkeley College
2020

University of California, Berkeley
2020

Environment and Climate Change Canada
2019

Vancouver Island University
2013-2014

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

Summertime Arctic shipboard observations of oxygenated volatile organic compounds (OVOCs) such as acids, key precursors climatically active secondary aerosol (SOA), are consistent with a novel source OVOCs to the marine boundary layer via chemistry at sea surface microlayer. Although this has been studied in laboratory setting, acid emissions from microlayer have not previously observed ambient environments. Correlations between measurements OVOCs, including high levels formic acid,...

10.1073/pnas.1620571114 article EN Proceedings of the National Academy of Sciences 2017-05-30

Abstract The Arctic region is a harbinger of global change and warming at rate higher than the average. While driven by increases in anthropogenic greenhouse gases' combination with local feedback mechanisms, short‐lived climate forcing agents, such as tropospheric aerosol, are also important drivers climate. aerosol‐climate impacts vary seasonally result interplay between aerosol different cloud types, available solar radiation, sea ice, surface albedo, lower latitude removal processes,...

10.1029/2018rg000602 article EN cc-by-nc-nd Reviews of Geophysics 2018-09-28

The application of Electrospray and Electrosonic Spray Ionization Mass Spectrometry (ESI-MS ESSI-MS) to study accelerated reaction kinetics in droplets is examined using numerical models, new experimental data, prior literature.

10.1039/d0sc04611f article EN cc-by-nc Chemical Science 2020-01-01

Abstract. The summertime Arctic lower troposphere is a relatively pristine background aerosol environment dominated by nucleation and Aitken mode particles. Understanding the mechanisms that control formation growth of crucial for our ability to predict cloud properties therefore radiative balance climate. We present an analysis event observed in Canadian Archipelago during summer as part NETCARE project. Under stable clean atmospheric conditions, with low inversion heights, carbon monoxide...

10.5194/acp-16-7663-2016 article EN cc-by Atmospheric chemistry and physics 2016-06-23

Abstract The optical properties of ambient black carbon‐containing particles and the composition their associated coatings were investigated at a downtown site in Toronto, Canada, for 2 weeks June 2013. objective was to assess relationship between carbon (BC) coating composition/thickness absorption. influenced by emissions from local vehicular traffic, wildfires Quebec, transboundary fossil fuel combustion United States. Mass concentrations BC nonrefractory measured using soot...

10.1002/2015jd023382 article EN Journal of Geophysical Research Atmospheres 2015-06-19

Abstract Although it is known that soot particles are emitted in large quantities to the atmosphere, our understanding of their environmental effects limited by knowledge how composition subsequently altered through atmospheric processing. Here we present an on-line mass spectrometric study changing chemical hydrocarbon as they oxidized gas-phase ozone, and show surface-mediated loss rates adsorbed polycyclic aromatic hydrocarbons directly connected a significant increase particle redox...

10.1038/ncomms7812 article EN cc-by Nature Communications 2015-04-15

Abstract. Observations addressing effects of aerosol particles on summertime Arctic clouds are limited. An airborne study, carried out during July 2014 from Resolute Bay, Nunavut, Canada, as part the Canadian NETCARE project, provides a comprehensive in situ look into some liquid clean environment summer. Median cloud droplet number concentrations (CDNC) 62 samples 10 cm−3 for low-altitude (clouds topped below 200 m) and 101 higher-altitude based above m). The lower activation size is ≤ 50...

10.5194/acp-16-11107-2016 article EN cc-by Atmospheric chemistry and physics 2016-09-08

Abstract. Ice nucleating particles (INPs) in the Arctic can influence climate and precipitation region; yet our understanding of concentrations sources INPs this region remain uncertain. In following, we (1) measured immersion mode Canadian marine boundary layer during summer 2014 on board CCGS Amundsen, (2) determined ratios surface areas mineral dust aerosol to sea spray aerosol, (3) investigated source using particle dispersion modelling. Average at −15, −20, −25 ∘C were 0.005, 0.044,...

10.5194/acp-19-1027-2019 article EN cc-by Atmospheric chemistry and physics 2019-01-25

Abstract. Size-resolved and vertical profile measurements of single particle chemical composition (sampling altitude range 50–3000 m) were conducted in July 2014 the Canadian high Arctic during an aircraft-based measurement campaign (NETCARE 2014). We deployed laser ablation aerosol mass spectrometer ALABAMA (vacuum aerodynamic diameter approximately 200–1000 nm) to identify different types their mixing states. On basis analysis, we found that a significant fraction (23 %) all analyzed...

10.5194/acp-17-13747-2017 article EN cc-by Atmospheric chemistry and physics 2017-11-20

Surfaces play a critical role in accelerating reaction rates micro-compartments.

10.1039/d0sc03189e article EN cc-by-nc Chemical Science 2020-01-01

Abstract. Understanding the impact of atmospheric black carbon (BC)-containing particles on human health and radiative forcing requires knowledge mixing state BC, including characteristics materials with which it is internally mixed. In this study, we examine refractory BC (rBC) other aerosol components in an urban environment (downtown Toronto) utilizing Aerodyne soot particle mass spectrometer equipped a light scattering module (LS-SP-AMS). k-means cluster analysis was used to classify...

10.5194/acp-15-1823-2015 article EN cc-by Atmospheric chemistry and physics 2015-02-20

Abstract. The soot-particle aerosol mass spectrometer (SP-AMS) uses an intra-cavity infrared laser to vaporize refractory black carbon (rBC) containing particles, making the particle beam–laser beam overlap critical in determining collection efficiency (CE) for rBC and associated non-refractory particulate matter (NR-PM). This work evaluates ability of SP-AMS quantify NR-PM internally mixed particles with different thicknesses organic coating. Using apparent relative ionization efficiencies...

10.5194/amt-7-4507-2014 article EN cc-by Atmospheric measurement techniques 2014-12-18

Abstract We present vertically resolved observations of aerosol composition during pristine summertime Arctic background conditions. The methansulfonic acid (MSA)‐to‐sulfate ratio peaked near the surface (mean 0.10), indicating a contribution from ocean‐derived biogenic sulfur. Similarly, organic (OA)‐to‐sulfate increased toward 2.0). Both MSA‐to‐sulfate and OA‐to‐sulfate ratios were significantly correlated with FLEXPART‐WRF‐predicted air mass residence time over open water,...

10.1002/2017gl073359 article EN Geophysical Research Letters 2017-06-14

Abstract. Black carbon (BC) contributes to Arctic warming, yet sources of BC and their geographic contributions remain uncertain. We interpret a series recent airborne (NETCARE 2015; PAMARCMiP 2009 2011 campaigns) ground-based measurements (at Alert, Barrow Ny-Ålesund) from multiple methods (thermal, laser incandescence light absorption) with the GEOS-Chem global chemical transport model its adjoint attribute BC. This is first comparison refractory (rBC) at Alert. The springtime performed by...

10.5194/acp-17-11971-2017 article EN cc-by Atmospheric chemistry and physics 2017-10-10

Abstract. Motivated by increasing levels of open ocean in the Arctic summer and lack prior altitude-resolved studies, extensive aerosol measurements were made during 11 flights NETCARE July 2014 airborne campaign from Resolute Bay, Nunavut. Flights included vertical profiles (60 to 3000 m above ground level) over ocean, fast ice, boundary layer clouds fogs. A general conclusion, observations particle numbers between 5 20 nm diameter (N5 − 20), is that ultrafine formation occurs readily...

10.5194/acp-17-5515-2017 article EN cc-by Atmospheric chemistry and physics 2017-05-02

Abstract. Biomass burning organic aerosol (BBOA) can be emitted from natural forest fires and human activities such as agricultural domestic energy generation. BBOA is strongly associated with atmospheric brown carbon (BrC) that absorbs near-ultraviolet visible light, resulting in significant impacts on regional visibility degradation radiative forcing. The mixing state of play a critical role the prediction optical properties. In this work, single-particle measurements Soot-Particle Aerosol...

10.5194/acp-16-5561-2016 article EN cc-by Atmospheric chemistry and physics 2016-05-04

Abstract. The vertical distribution of black carbon (BC) particles in the Arctic atmosphere is one key parameters controlling their radiative forcing and thus role climate change. This work investigates presence properties these light-absorbing aerosols over High Canadian (>70∘ N). Airborne campaigns were performed as part NETCARE project (Network on Climate Aerosols: Addressing Key Uncertainties Remote Environments) provided insights into variability distributions BC summer 2014 spring...

10.5194/acp-19-2361-2019 article EN cc-by Atmospheric chemistry and physics 2019-02-22

Abstract. Summertime Arctic aerosol size distributions are strongly controlled by natural regional emissions. Within this context, we use a chemical transport model with size-resolved microphysics (GEOS-Chem-TOMAS) to interpret measurements of from the Canadian Archipelago during summer 2016, as part “NETwork on Climate and Aerosols: Addressing key uncertainties in Remote Environments” (NETCARE) project. Our simulations suggest that condensation secondary organic (SOA) precursor vapors...

10.5194/acp-19-2787-2019 article EN cc-by Atmospheric chemistry and physics 2019-03-04

Chemical transformations in aerosols impact the lifetime of particle phase species, fate atmospheric pollutants, and both climate- health-relevant aerosol properties. Timescales for multiphase reactions ozone aqueous phases are governed by coupled kinetic processes between gas phase, interface, its bulk, which respond dynamically to reactive consumption O3. However, models reactivity often do not account nature processes. To examine these dynamics, we use new prior experimental observations...

10.1021/acs.jpca.2c03059 article EN The Journal of Physical Chemistry A 2022-07-21

Abstract. The climatic impacts of black carbon (BC) aerosol, an important absorber solar radiation in the atmosphere, remain poorly constrained and are intimately related to its particle-scale physical chemical properties. Using particle-resolved modelling informed by quantitative measurements from a soot-particle aerosol mass spectrometer, we confirm that mixing state (the distribution co-emitted amongst fresh BC-containing particles) at time emission significantly affects BC-aerosol...

10.5194/acp-16-4693-2016 article EN cc-by Atmospheric chemistry and physics 2016-04-14

Abstract. The sources, chemical transformations and removal mechanisms of aerosol transported to the Arctic are key factors that control aerosol–climate interactions. Our understanding sources processes is limited by a lack vertically resolved observations in remote regions. We present trace gases composition High springtime, made largely north 80∘ N, during NETCARE campaign. Trace gas gradients observed on these flights defined polar dome as 66–68∘ 30′ N below potential temperatures...

10.5194/acp-19-57-2019 article EN cc-by Atmospheric chemistry and physics 2019-01-03

Abstract. The springtime composition of the Arctic lower troposphere is to a large extent controlled by transport midlatitude air masses into Arctic. In contrast, precipitation and natural sources play most important role during summer. Within region sloping isentropes create barrier horizontal transport, known as polar dome. dome varies in space time exhibits strong influence on from midlatitudes, enhancing winter inhibiting We analyzed aircraft-based trace gas measurements two NETCARE...

10.5194/acp-19-15049-2019 article EN cc-by Atmospheric chemistry and physics 2019-12-13

Polar environments are among the fastest changing regions on planet. It is a crucial time to make significant improvements in our understanding of how ocean and ice biogeochemical processes linked with atmosphere. This especially true over Antarctica Southern Ocean where observations severely limited environment far from anthropogenic influences. In this commentary, we outline major gaps knowledge, emerging research priorities, upcoming opportunities needs. We then give an overview...

10.1525/elementa.2022.00130 article EN cc-by Elementa Science of the Anthropocene 2023-01-01

Abstract. Transport of anthropogenic aerosol into the Arctic in spring months has potential to affect regional climate; however, modeling estimates direct radiative effect (DRE) are sensitive uncertainties mixing state black carbon (BC). A common approach previous studies is assume an entirely external mixture (all primarily scattering species separate particles from BC) or internal mixed same as BC). To provide constraints on size-resolved BC, we use airborne single-particle soot photometer...

10.5194/acp-18-11345-2018 article EN cc-by Atmospheric chemistry and physics 2018-08-14
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