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    An Intercomparison of Radiation Codes for Retrieving Upper–Tropospheric Humidity in the 6.3–mm Band: A Report from the First GVaP Workshop 

    Source: Bulletin of the American Meteorological Society:;2000:;volume( 081 ):;issue: 004:;page 797
    Author(s): Soden, B.; Tjemkes, S.; Schmetz, J.; Saunders, R.; Bates, J.; Ellingson, B.; Engelen, R.; Garand, L.; Jackson, D.; Jedlovec, G.; Kleespies, T.; Randel, D.; Rayer, P.; Salathe, E.; Schwarzkopf, D.; Scott, N.; Sohn, B.; de Souza-Machado, S.; Strow, L.; Tobin, D.; Turner, D.; van Delst, P.; Wehr, T.
    Publisher: American Meteorological Society
    Abstract: An intercomparison of radiation codes used in retrieving upper?tropospheric humidity (UTH) from observations in the n2 (6.3 mm) water vapor absorption band was performed. This intercomparison is one part of a coordinated ...
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    A Preliminary Synthesis of Modeled Climate Change Impacts on U.S. Regional Ozone Concentrations 

    Source: Bulletin of the American Meteorological Society:;2009:;volume( 090 ):;issue: 012:;page 1843
    Author(s): Weaver, C. P.; Cooter, E.; Gilliam, R.; Gilliland, A.; Grambsch, A.; Grano, D.; Hemming, B.; Hunt, S. W.; Nolte, C.; Winner, D. A.; Liang, X-Z.; Zhu, J.; Caughey, M.; Kunkel, K.; Lin, J-T.; Tao, Z.; Williams, A.; Wuebbles, D. J.; Adams, P. J.; Dawson, J. P.; Amar, P.; He, S.; Avise, J.; Chen, J.; Cohen, R. C.; Goldstein, A. H.; Harley, R. A.; Steiner, A. L.; Tonse, S.; Guenther, A.; Lamarque, J-F.; Wiedinmyer, C.; Gustafson, W. I.; Leung, L. R.; Hogrefe, C.; Huang, H-C.; Jacob, D. J.; Mickley, L. J.; Wu, S.; Kinney, P. L.; Lamb, B.; Larkin, N. K.; McKenzie, D.; Liao, K-J.; Manomaiphiboon, K.; Russell, A. G.; Tagaris, E.; Lynn, B. H.; Mass, C.; Salathé, E.; O'neill, S. M.; Pandis, S. N.; Racherla, P. N.; Rosenzweig, C.; Woo, J-H.
    Publisher: American Meteorological Society
    Abstract: This paper provides a synthesis of results that have emerged from recent modeling studies of the potential sensitivity of U.S. regional ozone (O3) concentrations to global climate change (ca. 2050). This research has been ...
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