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M. C. Barth on Muck Rack

M. C. Barth

As seen in: Color Research & Application
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Articles

Introduction to the Deep Convective Clouds and Chemistry (DC3) 2012 Studies

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By M. C. Barth, S. A. Rutledge, W. H. Brune, C. Bryan Cantrell
| hal.science
Dates et versions Licence Copyright (Tous droits réservés) Identifiants Citer M. Barth, S. Rutledge, W. Brune, C. Cantrell. Introduction to the Deep Convective Clouds and Chemistry (DC3) 2012 Studies. Journal of Geophysical Research: Atmospheres , 2019, 124 (14), pp.8095-8103. ⟨10.1029/2019JD030944⟩ . ⟨hal-04568614⟩
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Using observations and source specific model tracers to characterize pollutant transport during FRAPPÉ and DISCOVER-AQ

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By G. G. Pfister, P. J. Reddy, M. C. Barth, F. Flocke, A. Fried, S. C. Herndon, B. Sive, A. M. Thompson, T. I. Yacovitch, A. J. Weinheimer, J. T. Sullivan, A. Wisthaler
| Color Research & Application Verified
Transport is a key parameter in air quality research and plays a dominant role in the Colorado Northern Front Range Metropolitan Area (NFRMA), where terrain induced flows and recirculation patterns can lead to vigorous mixing of different emission sources. To assess different transport processes and their connection to air quality in the NFRMA during the FRAPPÉ and DISCOVER-AQ campaigns in summer 2014, we use the Weather Research and Forecasting Model with inert tracers.
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Contrasting aerosol refractive index and hygroscopicity in the inflow and outflow of deep convective storms: Analysis of airborne data from DC3

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By Armin Sorooshian, J. Jimenez, D. R. Blake, A. Fried, T. Shingler, E. Crosbie, M. C. Barth, C. R. Homeyer, P. Campuzano-Jost, D. A. Day, K. L. Thornhill, L. D. Ziemba
| Color Research & Application Verified
We examine three case studies during the Deep Convective Clouds and Chemistry (DC3) field experiment when storm inflow and outflow air were sampled for aerosol sub-saturated hygroscopicity and the real part of refractive index (n) with a Differential Aerosol Sizing and Hygroscopicity Probe (DASH-SP) on the NASA DC-8. Relative to inflow aerosol particles, outflow particles were more hygroscopic (by 0.03 based on the estimated ? parameter) in one of the three storms examined.
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