HelioWebUniversity of Maryland, Department of Chemistry
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I[University of Maryland, Department of Chemistry]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (24)"]
CA["Linked Collaborating Authors (0)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Li Isotopes as a Tracer of Earth Processes
- Atmospheric Boundary Layer Extinction Coefficient from the 2001/2002 Baltimore PM Supersite Experiments
- Emission Rates of PM Constituents from Highly Time-Resolved Ambient Concentration Measurements: A New Paradigm in Air Pollution Management
- Source Attribution of Aerosols during the Baltimore PM Supersite in 2002 from Lidar, a Turbulence Sensor, and Back-Trajectory Analysis
- Overview of the Light Aircraft Aerosol Research Inlet (LAARI)
- Smoke Over Haze: Comparative Analysis of Satellite, Surface Radiometer and Airborne In-Situ Measurements of Aerosol Optical Properties and Radiative Forcing Over the Eastern US
- Accurate Ab Initio Calculation of the Isotopic Exchange Equilibrium 10B(OH)3 + 11B(OH)4- = 11B(OH)3 + 10B(OH)4- In Aqueous Solution
- Experimental determination of boron isotope fractionation in seawater
- 11,10B Isotopic Fractionation Between B(OH)3 and B(OH)4- and an Inorganic Mechanism for their Incorporation Into Calcite
- A Chemical Climatology of the Mid-Atlantic US Lower Troposphere: Implications for Origins and Lifetimes
- Optical Analysis of Coated and Uncoated Soot Particles
- An update on 11B,10B fractionation in the fundamental reaction: 10B(OH)3 + 11B(OH)4- = 11B(OH)3 + 10B(OH)4-
- Optical Analysis of Coated and Uncoated Soot: Data for Global Climate Change Models
- Sulfur Substitution in Oxyanions.
- Comparison of Aerosol Optical Depth Measurements from GOES-13, Aircraft, AERONET and the Surface During DISCOVER-AQ in July 2011
- Modeling the impact of bay breeze circulations on nitrogen deposition
- A Transport Analysis of In Situ Airborne Ozone Measurements from the 2011 DISCOVER-AQ Campaign
- Calculating Subsurface Nucleonic Production of Noble Gas Nuclides: Implications on Crustal and Mantle K, Th, U Abundances
- Analysis of Trends in Total Stratospheric Ozone
- Probability of Limiting Future Warming to 1.5°C and 2.0°C for Various Shared Socioeconomic Pathway Trajectories of Future GHG Abundances
- ECS, Climate Feedback, and TCRE: A Comparison of CMIP6 Values to Estimates Inferred from the Century-Long Climate Record
- Quantification of the Uptake of Anthropogenic Emissions of Atmospheric CO<SUB>2</SUB>
- Comparison of CMIP6 Equilibrium Climate Sensitivity to that Inferred from the Century and a Half Long Climate Record Using an Empirical Model of Global Climate
- Enhanced Terrestrial Carbon Sink Inferred from O<SUB>2</SUB>/N<SUB>2</SUB> Ratio Compared to Dynamic Global Vegetative Models