Connor Flynn
Organization:
University of Oklahoma
Pacific Northwest National Laboratory
Email:
Business Phone:
Mobile:
(509) 554-7791
Work:
(405) 325-1631
Business Address:
120 David L Boren Blvd
Norman, OK 73072
United StatesCo-Authored Publications:
- LeBlanc, S., et al. (2022), Airborne observations during KORUS-AQ show that aerosol optical depths are more spatially self-consistent than aerosol intensive properties, Atmos. Chem. Phys., doi:10.5194/acp-22-11275-2022.
- Pistone, K., et al. (2021), Exploring the elevated water vapor signal associated with the free-tropospheric biomass burning plume over the southeast Atlantic Ocean, Atmos. Chem. Phys., doi:10.5194/acp-2020-1322 (submitted).
- Xu, F., et al. (2021), A Combined Lidar-Polarimeter Inversion Approach for Aerosol Remote Sensing Over Ocean, Front. Remote Sens., 2, 1-24, doi:10.3389/frsen.2021.620871.
- Cochrane, S., et al. (2020), The Dependence of Aerosol Radiative Effects on Spectral Aerosol Properties Derived from Aircraft Measurements: Results from the ORACLES 2016 and ORACLES 2017 Experiments, Atmos. Chem. Phys. (manuscript in preparation).
- Shinozuka, Y., et al. (2020), Modeling the smoky troposphere of the southeast Atlantic: a comparison to ORACLES airborne observations from September of 2016, Atmos. Chem. Phys., 20, 11491-11526, doi:10.5194/acp-20-11491-2020.
- Shinozuka, Y., et al. (2020), Daytime aerosol optical depth above low-level clouds is similar to that in adjacent clear skies at the same heights: airborne observation above the southeast Atlantic, Atmos. Chem. Phys., doi:10.5194/acp-2019-1007 (submitted).
- Cochrane, S., et al. (2019), Above-cloud aerosol radiative effects based on ORACLES 2016 and ORACLES 2017 aircraft experiments, Atmos. Meas. Tech., 12, 6505-6528, doi:10.5194/amt-12-6505-2019.
- shinozuka, et al. (2019), Modeling the smoky troposphere of the southeast Atlantic: a comparison to ORACLES airborne observations from September of 2016, Atmos. Chem. Phys. Discuss., doi: https://doi.org/10.5194/acp-2019-678 (submitted).
- Star, T., et al. (2018), 4STAR_codes: 4STAR processing codes, Zenodo, doi:10.5281/zenodo.1492912.
- Dunagan, S. E., et al. (2017), Spectrometer for Sky-Scanning, Sun-Tracking Atmospheric Research (4STAR), doi:20170005591.
- Zhang, D., et al. (2017), The occurrence of ice production in slightly supercooled Arctic stratiform clouds as observed by ground-based remote sensors at the ARM NSA site, J. Geophys. Res., 122, doi:10.1002/2016JD026226.
- Segal-Rozenhaimer, M., et al. (2014), Tracking elevated pollution layers with a newly developed hyperspectral Sun/Sky spectrometer (4STAR): Results from the TCAP 2012 and 2013 campaigns, J. Geophys. Res., 119, doi:10.1002/2013JD020884.
- Dunagan, S. E., et al. (2013), Spectrometer for Sky-Scanning Sun-Tracking Atmospheric Research (4STAR): Instrument Technology, Remote Sens., 5, 3872-3895, doi:10.3390/rs5083872.
- Shinozuka, Y., et al. (2013), Hyperspectral aerosol optical depths from TCAP flights, J. Geophys. Res., 118, 12,180-12,194, doi:10.1002/2013JD020596.
- Kassianov, E., et al. (2012), Initial Assessment of the Spectrometer for Sky-Scanning, Sun-Tracking Atmospheric Research (4STAR)-Based Aerosol Retrieval: Sensitivity Study, Atmosphere, 3, 495-521, doi:10.3390/atmos3040495.
- Dunagan, S. E., et al. (2011), 4STAR Spectrometer for Sky-Scanning Sun-Tracking Atmospheric Research: Instrument Technology Development, 34th International Symposium on Remote Sensing of the Environment, Sydney, Australia, 10-15 Apr 2011.
- Kassianov, E., et al. (2010), Retrieval of aerosol optical depth in vicinity of broken clouds from reflectance ratios: case study, Atmos. Meas. Tech., 3, 1333-1349, doi:10.5194/amt-3-1333-2010.
- Schmid, B., et al. (2009), Validation of aerosol extinction and water vapor profiles from routine Atmospheric Radiation Measurement Program Climate Research Facility measurements, J. Geophys. Res., 114, D22207, doi:10.1029/2009JD012682.
- Alexandrov, M. D., et al. (2007), Optical depth measurements by shadow-band radiometers and their uncertainties, Appl. Opt., 46, 8027-8038.