human | Q5 |
P6178 | Dimensions author ID | 0766755575.06 |
P496 | ORCID iD | 0000-0001-6288-310X |
P1153 | Scopus author ID | 55207447000 |
P69 | educated at | University of Cambridge | Q35794 |
Harvard College | Q49123 | ||
University of California, Berkeley | Q168756 | ||
P108 | employer | Brookhaven National Laboratory | Q585777 |
P734 | family name | Schwartz | Q2253414 |
Schwartz | Q2253414 | ||
Schwartz | Q2253414 | ||
P735 | given name | Stephen | Q4927100 |
Stephen | Q4927100 | ||
P106 | occupation | researcher | Q1650915 |
Q57176100 | ATMOSPHERIC SCIENCE: Climate Forcing by Aerosol--a Hazy Picture |
Q58385700 | ATMOSPHERIC SCIENCE:Absorbing Phenomena |
Q58385670 | Aerosol Properties and Processes: A Path from Field and Laboratory Measurements to Global Climate Models |
Q98178986 | Bounding Global Aerosol Radiative Forcing of Climate Change |
Q58385725 | Chemistry with a silver lining |
Q58385711 | Climate response to radiative forcings by sulfate aerosols and greenhouse gases |
Q58385660 | Climatology of aerosol optical depth in north-central Oklahoma: 1992–2008 |
Q58385751 | Comment on "Resonant fluorescence and Raman scattering" |
Q58385675 | Comment on “size distribution of sea-salt emissions as a function of relative humidity” |
Q58385649 | Determination of Earth’s Transient and Equilibrium Climate Sensitivities from Observations Over the Twentieth Century: Strong Dependence on Assumed Forcing |
Q58385647 | Determination of a lower bound on Earth's climate sensitivity |
Q58241808 | Direct aerosol forcing: Calculation from observables and sensitivities to inputs |
Q58385644 | Earth's Climate Sensitivity: Apparent Inconsistencies in Recent Assessments |
Q58385687 | Evaluation of a chemical transport model for sulfate using ACE-2 observations and attribution of sulfate mixing ratios to source regions and formation processes |
Q58241845 | Evaporation of Ammonium Nitrate Aerosol in a Heated Nephelometer: Implications for Field Measurements |
Q58385654 | Feedback and sensitivity in an electrical circuit: an analog for climate models |
Q55887992 | Heat capacity, time constant, and sensitivity of Earth's climate system |
Q58385642 | High-resolution photography of clouds from the surface: Retrieval of optical depth of thin clouds down to centimeter scales |
Q58385721 | Hit or miss? |
Q30675000 | Influence of anthropogenic aerosol on cloud optical depth and albedo shown by satellite measurements and chemical transport modeling |
Q58385713 | Laboratory study of NO2 reaction with DISPERSED and bulk liquid water |
Q58385681 | Modeling atmospheric sulfur over the Northern Hemisphere during the Aerosol Characterization Experiment 2 experimental period |
Q58385678 | New unbiased symmetric metrics for evaluation of air quality models |
Q58385674 | Observation of ambient aerosol particle growth due to in-cloud processes within boundary layers |
Q58385653 | Observing and Modeling Earth’s Energy Flows |
Q58385714 | Optical properties of atmospheric aerosols from moments of the particle size distribution |
Q58241833 | PARAGON: An Integrated Approach for Characterizing Aerosol Climate Impacts and Environmental Interactions |
Q58241818 | Preface to special section: Atmospheric Radiation Measurement Program May 2003 Intensive Operations Period examining aerosol properties and radiative influences |
Q58385657 | Production flux of sea spray aerosol |
Q58385705 | Properties and evolution of aerosols with size distributions having identical moments |
Q58385753 | Pulse‐to‐Analog Converter for Optimizing Signal‐to‐Noise from Photomultipliers at Low Light Intensities |
Q58385663 | Reply 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” |
Q58241793 | Reply to “Comments on ‘Why Hasn't Earth Warmed as Much as Expected?’” |
Q58385658 | Reversible uptake of water on NaCl nanoparticles at relative humidity below deliquescence point observed by noncontact environmental atomic force microscopy |
Q58241834 | Scientific Objectives, Measurement Needs, and Challenges Motivating the PARAGON Aerosol Initiative |
Q58385702 | Six-moment representation of multiple aerosol populations in a sub-hemispheric chemical transformation model |
Q58385640 | The Greenhouse Effect and Climate Change |
Q58385664 | The role of adiabaticity in the aerosol first indirect effect |
Q58385718 | The scavenging of nitrate by clouds and precipitation |
Q58385709 | The whitehouse effect—Shortwave radiative forcing of climate by anthropogenic aerosols: an overview |
Q58385666 | Uncertainty in climate sensitivity: Causes, consequences, challenges |
Q58385638 | Unrealized Global Temperature Increase: Implications of Current Uncertainties |
Q56286592 | Why Hasn’t Earth Warmed as Much as Expected? |
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