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Interannual Variability and Trends of Combustion Aerosol and Dust in Major Continental Outflows Revealed by MODIS Retrievals and CAM5 Simulations During 2003-2017Emissions and long-range transport of mineral dust and combustion-related aerosol from burning fossil fuels and biomass vary from year to year, driven by the evolution of the economy and changes in meteorological conditions and environmental regulations. This study offers both satellite and model perspectives of interannual variability and possible trend of combustion aerosol and dust in major continental outflow regions over the past 15 years (2003-2017). The decade-long record of aerosol optical depth (AOD, denoted as t), separately for combustion aerosol (τ(sub c)) and dust (τ(sub d)), over global oceans is derived from the Collection 6 aerosol products of the Moderate Resolution Imaging Spectroradiometer (MODIS) onboard both Terra and Aqua. These MODIS/Aqua datasets, complemented by aerosol source-tagged simulations using the Community Atmospheric Model Version 5 (CAM5), are then analyzed to understand the interannual variability and potential trend of τ(sub c) and τ(sub d) in the major continental outflows. Both MODIS and CAM5 consistently yield a similar decreasing trend of -0.017 to - 0.020 decade(exp -1) for τ(sub c) over the North Atlantic Ocean and the Mediterranean Sea that is attributable to reduced emissions from North America and Europe, respectively. On the contrary, both MODIS and CAM5 display an increasing trend of +0.017 to +0.036 decade(exp -1) for τ(sub c) over the tropical Indian Ocean, the Bay of Bengal, and the Arabian Sea, which reflects the influence of increased anthropogenic emissions from South Asia and Middle East in the last two decades. Over the northwestern Pacific Ocean that is often affected by East Asian emissions of pollution and dust, the MODIS retrievals show a decreasing trend of - 0.021 decade(exp -1) for τ(sub c) and -0.012 decade(exp -1) for τ(sub d), which is however not reproduced by the CAM5 model. In other outflow regions strongly influenced by biomass burning smoke or dust, both MODIS retrievals and CAM5 simulations show no statistically significant trends; and the MODIS observed interannual variability is usually larger than that of the CAM5 simulation.
Document ID
20190033294
Acquisition Source
Goddard Space Flight Center
Document Type
Accepted Manuscript (Version with final changes)
External Source(s)
Authors
Hongbin Yu
(Goddard Space Flight Center Greenbelt, Maryland, United States)
Yang Yang
(Pacific Northwest National Laboratory Richland, Washington, United States)
Hailong Wang
(Pacific Northwest National Laboratory Richland, Washington, United States)
Qian Tan
(Bay Area Environmental Research Institute Petaluma, California, United States)
Mian Chin
(Goddard Space Flight Center Greenbelt, Maryland, United States)
Robert C Levy
(Goddard Space Flight Center Greenbelt, Maryland, United States)
Lorraine A Remer
(University of Maryland, Baltimore County Baltimore, Maryland, United States)
Steven J Smith
(Pacific Northwest National Laboratory Richland, Washington, United States)
Tianle Yuan
(University of Maryland, Baltimore County Baltimore, Maryland, United States)
Yingxi Shi
(University of Maryland, Baltimore County Baltimore, Maryland, United States)
Date Acquired
November 29, 2019
Publication Date
January 3, 2020
Publication Information
Publication: Atmospheric Chemistry and Physics
Publisher: European Geosciences Union
Volume: 20
Issue: 1
Issue Publication Date: January 1, 2020
ISSN: 1680-7316
e-ISSN: 1680-7324
URL: https://acp.copernicus.org/articles/20/139/2020/acp-20-139-2020.html
Subject Category
Earth Resources And Remote Sensing
Report/Patent Number
GSFC-E-DAA-TN75699
ISSN: 1680-7316
E-ISSN: 1680-7324
Report Number: GSFC-E-DAA-TN75699
Funding Number(s)
PROJECT: SCMD-EarthScienceSystem_281945
CONTRACT_GRANT: NNX15AT34A
CONTRACT_GRANT: NNX12AD05A
Distribution Limits
Public
Copyright
Use by or on behalf of the US Gov. Permitted.
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