A41K-0234
Airborne Observations of Urban-Derived Water Vapor and Potential Impacts on Chemistry and Clouds

Thursday, 17 December 2015
Poster Hall (Moscone South)
Olivia Elizabeth Salmon1, Paul B Shepson2, Robert M. Grundman II3, Brian H Stirm3, Xinrong Ren4,5, Russell R Dickerson6 and Jose D Fuentes7, (1)Purdue University, Chemistry, West Lafayette, IN, United States, (2)Purdue University, Earth, Atmospheric, and Planetary Sciences, West Lafayette, IN, United States, (3)Purdue University, Aviation Technology, West Lafayette, IN, United States, (4)NOAA Science Center, College Park, MD, United States, (5)University of Maryland College Park, College Park, MD, United States, (6)University of Maryland, Oceanic and Atmospheric Science, College Park, MD, United States, (7)Pennsylvania State University, Meteorology, University Park, PA, United States
Abstract:
Atmospheric conditions typical of wintertime, such as lower boundary layer heights and reduced turbulent mixing, provide a unique environment for anthropogenic pollutants to accumulate and react. Wintertime enhancements in water vapor (H2O) have been observed in urban areas, and are thought to result from fossil fuel combustion and urban heat island-induced evaporation. The contribution of urban-derived water vapor to the atmosphere has the potential to locally influence atmospheric chemistry and weather for the urban area and surrounding region due to interactions between H2O and other chemical species, aerosols, and clouds.

Airborne observations of urban-derived H2O, carbon dioxide (CO2), methane, nitrogen dioxide (NO2), ozone, and aerosols were conducted from Purdue University’s Airborne Laboratory for Atmospheric Research (ALAR) and the University of Maryland’s (UMD) Twin Cessna research aircraft during the winter of 2015. Measurements were conducted as part of the collaborative airborne campaign, Wintertime INvestigation of Transport, Emissions, and Reactivity (WINTER), which investigated seasonal trends in anthropogenic emissions and reactivity in the Northeastern United States. ALAR and the UMD aircraft participated in mass balance experiments around Washington D.C.-Baltimore to determine total city emission rates of H2O and other greenhouse gases.

Average enhancements in H2O mixing ratio of 0.048%, and up to 0.13%, were observed downwind of the urban centers on ten research flights. In some cases, downwind H2O concentrations clearly track CO2 and NO2 enhancements, suggesting a strong combustion signal. Analysis of Purdue and UMD data collected during the WINTER campaign shows an average urban-derived H2O contribution of 5.3%, and as much as 13%, to the local boundary layer from ten research flights flown in February and March of 2015. In this paper, we discuss the potential chemical and physical implications of these results.

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