In-flight validation of Aura MLS ozone with CAFS partial ozone columns Petropavlovskikh, I., et al. (2008), In-flight validation of Aura MLS ozone with CAFS partial ozone columns, J. Geophys. Res., 113, D16S41, doi:10.1029/2007JD008690. Read more about In-flight validation of Aura MLS ozone with CAFS partial ozone columns
Ultraviolet actinic flux in clear and cloudy atmospheres: model calculations and aircraft-based measurements Palancar, G.G., et al. (2011), Ultraviolet actinic flux in clear and cloudy atmospheres: model calculations and aircraft-based measurements, Atmos. Chem. Phys., 11, 5457-5469, doi:10.5194/acp-11-5457-2011. Read more about Ultraviolet actinic flux in clear and cloudy atmospheres: model calculations and aircraft-based measurements
Why do models overestimate surface ozone in the Southeast United States? Travis, K.R., et al. (2016), Why do models overestimate surface ozone in the Southeast United States?, Atmos. Chem. Phys., 16, 13561-13577, doi:10.5194/acp-16-13561-2016. Read more about Why do models overestimate surface ozone in the Southeast United States?
Pressure Stabilization of Criegee Intermediates Formed from Symmetric trans-Alkene Ozonolysis Hakala, J.P., and N.M. Donahue (2018), Pressure Stabilization of Criegee Intermediates Formed from Symmetric trans-Alkene Ozonolysis, J. Phys. Chem. A, 122, 9426-9434, doi:10.1021/acs.jpca.8b09650. Read more about Pressure Stabilization of Criegee Intermediates Formed from Symmetric trans-Alkene Ozonolysis
Cite This: Environ. Sci. Technol. 2018, 52, 13738−13746 pubs.acs.org/est Constraints on Aerosol Nitrate Photolysis as a Potential Source of HONO and NOx Romer, P.S., et al. (2018), Cite This: Environ. Sci. Technol. 2018, 52, 13738−13746 pubs.acs.org/est Constraints on Aerosol Nitrate Photolysis as a Potential Source of HONO and NOx, Environ. Sci. Technol., doi:10.1021/acs.est.8b03861. Read more about Cite This: Environ. Sci. Technol. 2018, 52, 13738−13746 pubs.acs.org/est Constraints on Aerosol Nitrate Photolysis as a Potential Source of HONO and NOx
Pressure-Dependent Criegee Intermediate Stabilization from Alkene Ozonolysis Hakala, J.P., and N.M. Donahue (2016), Pressure-Dependent Criegee Intermediate Stabilization from Alkene Ozonolysis, J. Phys. Chem. A, 120, 2173-2178, doi:10.1021/acs.jpca.6b01538. Read more about Pressure-Dependent Criegee Intermediate Stabilization from Alkene Ozonolysis
Adsorptive uptake of water by semisolid secondary organic aerosols Pajunoja, A., et al. (2015), Adsorptive uptake of water by semisolid secondary organic aerosols, Geophys. Res. Lett., 42, 3063-3068, doi:10.1002/2015GL063142. Read more about Adsorptive uptake of water by semisolid secondary organic aerosols
Reactivity of stabilized Criegee intermediates (sCIs) from isoprene and monoterpene ozonolysis toward SO2 and organic acids Sipilä, M., et al. (2014), Reactivity of stabilized Criegee intermediates (sCIs) from isoprene and monoterpene ozonolysis toward SO2 and organic acids, Atmos. Chem. Phys., 14, 12143-12153, doi:10.5194/acp-14-12143-2014. Read more about Reactivity of stabilized Criegee intermediates (sCIs) from isoprene and monoterpene ozonolysis toward SO2 and organic acids
MRCISD Studies of the Dissociation of Vinylhydroperoxide, CH2CHOOH: There Is a Saddle Point Kurtén, T., and N.M. Donahue (2012), MRCISD Studies of the Dissociation of Vinylhydroperoxide, CH2CHOOH: There Is a Saddle Point, J. Phys. Chem. A, 116, 6823-6830, doi:10.1021/jp302511a. Read more about MRCISD Studies of the Dissociation of Vinylhydroperoxide, CH2CHOOH: There Is a Saddle Point
A cloud algorithm based on the O2-O2 477 nm absorption band featuring an advanced spectral fitting method and the use of surface geometry-dependent Lambertian-equivalent reflectivity Vasilkov, A., et al. (2018), A cloud algorithm based on the O2-O2 477 nm absorption band featuring an advanced spectral fitting method and the use of surface geometry-dependent Lambertian-equivalent reflectivity, Atmos. Meas. Tech., 11, 4093-4107, doi:10.5194/amt-11-4093-2018. Read more about A cloud algorithm based on the O2-O2 477 nm absorption band featuring an advanced spectral fitting method and the use of surface geometry-dependent Lambertian-equivalent reflectivity