Multi-Decadal Aerosol Variations from 1980 to 2009: A Perspective from Observations and a Global Model

• Main Authors: Chin, Mian, Kucsera, T. L., Prospero, J. M., Quinn, P. K., Hsu, N. C., Tan, Q., Diehl, T., Bian, H., Strode, S. A., Howell, S. G., Torres, O., Streets, D. G., Kahn, R. A., Holben, B. N., Huebert, B. J., Remer, L. A., Pan, X., Yu, H., Levy, R. C., Mishchenko, M. I., Geogdzhayev, I. V., Zhao, X.-P., Kim, D., Schuster, G. L., Sayer, A. M.
• Format: Other/Unknown Material
• Language: unknown
• Published: 2014
• Subjects: Earth Resources and Remote Sensing; Environment Pollution; North Atlantic
• Online Access: http://hdl.handle.net/2060/20140013029

Aerosol variations and trends over different land and ocean regions during 1980-2009 are analyzed with the Goddard Chemistry Aerosol Radiation and Transport (GOCART) model and observations from multiple satellite sensors and ground-based networks. Excluding time periods with large volcanic influences, the tendency of aerosol optical depth (AOD) and surface concentration over polluted land regions is consistent with the anthropogenic emission changes.The largest reduction occurs over Europe, and regions in North America and Russia also exhibit reductions. On the other hand, East Asia and South Asia show AOD increases, although relatively large amount of natural aerosols in Asia makes the total changes less directly connected to the pollutant emission trends. Over major dust source regions, model analysis indicates that the dust emissions over the Sahara and Sahel respond mainly to the near-surface wind speed, but over Central Asia they are largely influenced by ground wetness. The decreasing dust trend in the tropical North Atlantic is most closely associated with the decrease of Sahel dust emission and increase of precipitation over the tropical North Atlantic, likely driven by the sea surface temperature increase. Despite significant regional trends, the model-calculated global annual average AOD shows little changes over land and ocean in the past three decades, because opposite trends in different regions cancel each other in the global average. This highlights the need for regional-scale aerosol assessment, as the global average value conceals regional changes, and thus is not sufficient for assessing changes in aerosol loading.