Observations of the Interaction and Transport of Fine Mode Aerosols With Cloud and/or Fog in Northeast Asia From Aerosol Robotic Network and Satellite Remote Sensing

• Main Authors: Govindaraju, R. C., Hyer, E., Kim, K. C., O’Neill, N. T., Xian, P., Xia, X., Sayer, A. M., Choi, M., Koo, J.-H., Schafer, J. S., Buchard, V., Levy, R. C., Slutsker, I., Reid, J. S., Eck, T. F., Sano, I., Giles, D. M., Arola, A., Munchak, L. A., Sinyuk, A., Wang, P., Kim, J., Hsu, N. C., Lyapustin, A., Holben, B. N., Crawford, J. H., Silva, A. M. Da, Randles, C. A., Smirnov, A.
• Format: Other/Unknown Material
• Language: unknown
• Published: 2018
• Subjects: Earth Resources and Remote Sensing; Aerosol Robotic Network
• Online Access: http://hdl.handle.net/2060/20190027005

Analysis of Sun photometer measured and satellite retrieved aerosol optical depth (AOD) datahas shown that major aerosol pollution events with very highfine mode AOD (>1.0 in midvisible) in theChina/Korea/Japan region are often observed to be associated with significant cloud cover. This makesremote sensing of these events difficult even for high temporal resolution Sun photometer measurements.Possible physical mechanisms for these events that have high AOD include a combination of aerosolhumidification, cloud processing, and meteorological covariation with atmospheric stability andconvergence. The new development of Aerosol Robotic Network Version 3 Level 2 AOD with improved cloudscreening algorithms now allow for unprecedented ability to monitor these extremefine mode pollutionevents. Further, the spectral deconvolution algorithm (SDA) applied to Level 1 data (L1; no cloud screening)provides an even more comprehensive assessment offine mode AOD than L2 in current and previous dataversions. Studying the 2012 winter-summer period, comparisons of Aerosol Robotic Network L1 SDA dailyaveragefine mode AOD data showed that Moderate Resolution Imaging Spectroradiometer satellite remotesensing of AOD often did not retrieve and/or identify some of the highestfine mode AOD events in thisregion. Also, compared to models that include data assimilation of satellite retrieved AOD, the L1 SDAfinemode AOD was significantly higher in magnitude, particularly for the highest AOD events that were oftenassociated with significant cloudiness.