Stephen E. Schwartz

researcher, ORCID id # 0000-0001-6288-310X

Stephen E. Schwartz is …
instance of (P31):
humanQ5

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P6178Dimensions author ID0766755575.06
P496ORCID iD0000-0001-6288-310X
P1153Scopus author ID55207447000

P69educated atUniversity of CambridgeQ35794
Harvard CollegeQ49123
University of California, BerkeleyQ168756
P108employerBrookhaven National LaboratoryQ585777
P734family nameSchwartzQ2253414
SchwartzQ2253414
SchwartzQ2253414
P735given nameStephenQ4927100
StephenQ4927100
P106occupationresearcherQ1650915

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author (P50)
Q57176100ATMOSPHERIC SCIENCE: Climate Forcing by Aerosol--a Hazy Picture
Q58385700ATMOSPHERIC SCIENCE:Absorbing Phenomena
Q58385670Aerosol Properties and Processes: A Path from Field and Laboratory Measurements to Global Climate Models
Q98178986Bounding Global Aerosol Radiative Forcing of Climate Change
Q58385725Chemistry with a silver lining
Q58385711Climate response to radiative forcings by sulfate aerosols and greenhouse gases
Q58385660Climatology of aerosol optical depth in north-central Oklahoma: 1992–2008
Q58385751Comment on "Resonant fluorescence and Raman scattering"
Q58385675Comment on “size distribution of sea-salt emissions as a function of relative humidity”
Q58385649Determination of Earth’s Transient and Equilibrium Climate Sensitivities from Observations Over the Twentieth Century: Strong Dependence on Assumed Forcing
Q58385647Determination of a lower bound on Earth's climate sensitivity
Q58241808Direct aerosol forcing: Calculation from observables and sensitivities to inputs
Q58385644Earth's Climate Sensitivity: Apparent Inconsistencies in Recent Assessments
Q58385687Evaluation of a chemical transport model for sulfate using ACE-2 observations and attribution of sulfate mixing ratios to source regions and formation processes
Q58241845Evaporation of Ammonium Nitrate Aerosol in a Heated Nephelometer: Implications for Field Measurements
Q58385654Feedback and sensitivity in an electrical circuit: an analog for climate models
Q55887992Heat capacity, time constant, and sensitivity of Earth's climate system
Q58385642High-resolution photography of clouds from the surface: Retrieval of optical depth of thin clouds down to centimeter scales
Q58385721Hit or miss?
Q30675000Influence of anthropogenic aerosol on cloud optical depth and albedo shown by satellite measurements and chemical transport modeling
Q58385713Laboratory study of NO2 reaction with DISPERSED and bulk liquid water
Q58385681Modeling atmospheric sulfur over the Northern Hemisphere during the Aerosol Characterization Experiment 2 experimental period
Q58385678New unbiased symmetric metrics for evaluation of air quality models
Q58385674Observation of ambient aerosol particle growth due to in-cloud processes within boundary layers
Q58385653Observing and Modeling Earth’s Energy Flows
Q58385714Optical properties of atmospheric aerosols from moments of the particle size distribution
Q58241833PARAGON: An Integrated Approach for Characterizing Aerosol Climate Impacts and Environmental Interactions
Q58241818Preface to special section: Atmospheric Radiation Measurement Program May 2003 Intensive Operations Period examining aerosol properties and radiative influences
Q58385657Production flux of sea spray aerosol
Q58385705Properties and evolution of aerosols with size distributions having identical moments
Q58385753Pulse‐to‐Analog Converter for Optimizing Signal‐to‐Noise from Photomultipliers at Low Light Intensities
Q58385663Reply to comments by G. Foster et al., R. Knutti et al., and N. Scafetta on “Heat capacity, time constant, and sensitivity of Earth's climate system”
Q58241793Reply to “Comments on ‘Why Hasn't Earth Warmed as Much as Expected?’”
Q58385658Reversible uptake of water on NaCl nanoparticles at relative humidity below deliquescence point observed by noncontact environmental atomic force microscopy
Q58241834Scientific Objectives, Measurement Needs, and Challenges Motivating the PARAGON Aerosol Initiative
Q58385702Six-moment representation of multiple aerosol populations in a sub-hemispheric chemical transformation model
Q58385640The Greenhouse Effect and Climate Change
Q58385664The role of adiabaticity in the aerosol first indirect effect
Q58385718The scavenging of nitrate by clouds and precipitation
Q58385709The whitehouse effect—Shortwave radiative forcing of climate by anthropogenic aerosols: an overview
Q58385666Uncertainty in climate sensitivity: Causes, consequences, challenges
Q58385638Unrealized Global Temperature Increase: Implications of Current Uncertainties
Q56286592Why Hasn’t Earth Warmed as Much as Expected?

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