A33D-0206
Inference of Spatiotemporal Distribution of Black Carbon Aerosols over Northern Pacific from Satellite Observations (2005-2012)
Wednesday, 16 December 2015
Poster Hall (Moscone South)
Zhongshu Li1, Junfeng Liu2, Denise L Mauzerall3, Songmiao Fan4, Larry Wayne Horowitz5, Cenlin He6, Kan Yi2 and Shu Tao2, (1)Princeton University, Princeton, NJ, United States, (2)Peking University, College of Urban and Environmental Sciences, Beijing, China, (3)Princeton Univ, Princeton, NJ, United States, (4)NOAA, Boulder, CO, United States, (5)Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States, (6)University of California Los Angeles, Los Angeles, CA, United States
Abstract:
Knowledge on the spatiotemporal distribution of black carbon aerosol over the Northern Pacific is limited by a deficiency of observations. The HIAPER Pole-to-Pole Observation (HIPPO) program from 2009 to 2011 is the most comprehensive data source available and it reveals a 2 to 10 times overestimates of BC by current global models. Incorporation and assimilation of more data sources is needed to increase our understanding of the spatiotemporal distribution of black carbon aerosol and its corresponding climate effects. Based on measurements from aircraft campaigns and satellites, a robust association is observed between BC concentrations and satellite retrieved CO, tropospheric NO2, and aerosol optical depth (AOD) (R2 > 0.7). Such robust relationships indicate that BC aerosols share a similar emission sources, evolution processes and transport characteristics with other pollutants measured by satellite observations. It also establishes a basis to derive a satellite-based proxy (BC*) over remote oceans. The inferred satellite-based BC* shows that Asian export events in spring bring much more BC aerosols to the mid-Pacific than occurs in other seasons. In addition, inter-annual variability of BC* is seen over the Northern Pacific, with abundances correlated to the springtime Pacific/North American (PNA) index. The inferred BC* dataset also indicates a widespread overestimation of BC loadings by models over most remote oceans beyond the Pacific. Our method presents a novel approach to infer BC concentrations by combining satellite and aircraft observations.
