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    The MERRA-2 Aerosol Reanalysis, 1980 Onward. Part II: Evaluation and Case Studies

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 017::page 6851
    Author:
    Buchard, V.;Randles, C. A.;da Silva, A. M.;Darmenov, A.;Colarco, P. R.;Govindaraju, R.;Ferrare, R.;Hair, J.;Beyersdorf, A. J.;Ziemba, L. D.;Yu, H.
    DOI: 10.1175/JCLI-D-16-0613.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe Modern-Era Retrospective Analysis for Research and Applications, version 2 (MERRA-2), is NASA?s latest reanalysis for the satellite era (1980 onward) using the Goddard Earth Observing System, version 5 (GEOS-5), Earth system model. MERRA-2 provides several improvements over its predecessor (MERRA-1), including aerosol assimilation for the entire period. MERRA-2 assimilates bias-corrected aerosol optical depth (AOD) from the Moderate Resolution Imaging Spectroradiometer and the Advanced Very High Resolution Radiometer instruments. Additionally, MERRA-2 assimilates (non bias corrected) AOD from the Multiangle Imaging SpectroRadiometer over bright surfaces and AOD from Aerosol Robotic Network sunphotometer stations. This paper, the second of a pair, summarizes the efforts to assess the quality of the MERRA-2 aerosol products. First, MERRA-2 aerosols are evaluated using independent observations. It is shown that the MERRA-2 absorption aerosol optical depth (AAOD) and ultraviolet aerosol index (AI) compare well with Ozone Monitoring Instrument observations. Next, aerosol vertical structure and surface fine particulate matter (PM2.5) are evaluated using available satellite, aircraft, and ground-based observations. While MERRA-2 generally compares well to these observations, the assimilation cannot correct for all deficiencies in the model (e.g., missing emissions). Such deficiencies can explain many of the biases with observations. Finally, a focus is placed on several major aerosol events to illustrate successes and weaknesses of the AOD assimilation: the Mount Pinatubo eruption, a Saharan dust transport episode, the California Rim Fire, and an extreme pollution event over China. The article concludes with a summary that points to best practices for using the MERRA-2 aerosol reanalysis in future studies.
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      The MERRA-2 Aerosol Reanalysis, 1980 Onward. Part II: Evaluation and Case Studies

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    contributor authorBuchard, V.;Randles, C. A.;da Silva, A. M.;Darmenov, A.;Colarco, P. R.;Govindaraju, R.;Ferrare, R.;Hair, J.;Beyersdorf, A. J.;Ziemba, L. D.;Yu, H.
    date accessioned2018-01-03T11:01:00Z
    date available2018-01-03T11:01:00Z
    date copyright6/12/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-16-0613.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246070
    description abstractAbstractThe Modern-Era Retrospective Analysis for Research and Applications, version 2 (MERRA-2), is NASA?s latest reanalysis for the satellite era (1980 onward) using the Goddard Earth Observing System, version 5 (GEOS-5), Earth system model. MERRA-2 provides several improvements over its predecessor (MERRA-1), including aerosol assimilation for the entire period. MERRA-2 assimilates bias-corrected aerosol optical depth (AOD) from the Moderate Resolution Imaging Spectroradiometer and the Advanced Very High Resolution Radiometer instruments. Additionally, MERRA-2 assimilates (non bias corrected) AOD from the Multiangle Imaging SpectroRadiometer over bright surfaces and AOD from Aerosol Robotic Network sunphotometer stations. This paper, the second of a pair, summarizes the efforts to assess the quality of the MERRA-2 aerosol products. First, MERRA-2 aerosols are evaluated using independent observations. It is shown that the MERRA-2 absorption aerosol optical depth (AAOD) and ultraviolet aerosol index (AI) compare well with Ozone Monitoring Instrument observations. Next, aerosol vertical structure and surface fine particulate matter (PM2.5) are evaluated using available satellite, aircraft, and ground-based observations. While MERRA-2 generally compares well to these observations, the assimilation cannot correct for all deficiencies in the model (e.g., missing emissions). Such deficiencies can explain many of the biases with observations. Finally, a focus is placed on several major aerosol events to illustrate successes and weaknesses of the AOD assimilation: the Mount Pinatubo eruption, a Saharan dust transport episode, the California Rim Fire, and an extreme pollution event over China. The article concludes with a summary that points to best practices for using the MERRA-2 aerosol reanalysis in future studies.
    publisherAmerican Meteorological Society
    titleThe MERRA-2 Aerosol Reanalysis, 1980 Onward. Part II: Evaluation and Case Studies
    typeJournal Paper
    journal volume30
    journal issue17
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-16-0613.1
    journal fristpage6851
    journal lastpage6872
    treeJournal of Climate:;2017:;volume( 030 ):;issue: 017
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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