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Browsing by Author "Zappa, Christopher J."

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Browsing by Author "Zappa, Christopher J."

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  • McGillis, Wade R.; Edson, James B.; Zappa, Christopher J.; Ware, Jonathan D.; McKenna, Sean P.; Terray, Eugene A.; Hare, Jeffrey E.; Fairall, Christopher W.; Drennan, William M.; Donelan, Mark A.; DeGrandpre, Michael D.; Wanninkhof, Rik; Feely, Richard A. (American Geophysical Union, 2004-08-28)
    GasEx-2001, a 15-day air-sea carbon dioxide (CO2) exchange study conducted in the equatorial Pacific, used a combination of ships, buoys, and drifters equipped with ocean and atmospheric sensors to assess variability and ...
  • Zappa, Christopher J.; McGillis, Wade R.; Raymond, Peter A.; Edson, James B.; Hintsa, Eric J.; Zemmelink, Hendrik J.; Dacey, John W. H.; Ho, David T. (American Geophysical Union, 2007-05-17)
    Air-water gas transfer influences CO2 and other climatically important trace gas fluxes on regional and global scales, yet the magnitude of the transfer is not well known. Widely used models of gas exchange rates are based ...
  • Ho, David T.; Zappa, Christopher J.; McGillis, Wade R.; Bliven, Larry F.; Ward, Brian; Dacey, John W. H.; Schlosser, Peter; Hendricks, Melissa B. (American Geophysical Union, 2004-07-01)
    Rain has been shown to significantly enhance the rate of air-water gas exchange in fresh water environments, and the mechanism behind this enhancement has been studied in laboratory experiments. In the ocean, the effects ...
  • Zappa, Christopher J.; Ho, David T.; McGillis, Wade R.; Banner, Michael L.; Dacey, John W. H.; Bliven, Larry F.; Ma, Barry; Nystuen, Jeffrey A. (American Geophysical Union, 2009-07-09)
    Results from a rain and gas exchange experiment (Bio2 RainX III) at the Biosphere 2 Center demonstrate that turbulence controls the enhancement of the air-sea gas transfer rate (or velocity) k during rainfall, even though ...
  • Edson, James B.; Zappa, Christopher J.; Ware, J. A.; McGillis, Wade R.; Hare, Jeffrey E. (American Geophysical Union, 2004-08-14)
    The most commonly used flux-profile relationships are based on Monin-Obukhov (MO) similarity theory. These flux-profile relationships are required in indirect methods such as the bulk aerodynamic, profile, and inertial ...
  • Farrar, J. Thomas; Zappa, Christopher J.; Weller, Robert A.; Jessup, Andrew T. (American Geophysical Union, 2007-06-20)
    In aerial surveys conducted during the Tropical Ocean–Global Atmosphere Coupled Ocean-Atmosphere Response Experiment and the low-wind component of the Coupled Boundary Layer Air-Sea Transfer (CBLAST-Low) oceanographic field ...
  • Hintsa, Eric J.; Dacey, John W. H.; McGillis, Wade R.; Edson, James B.; Zappa, Christopher J.; Zemmelink, Hendrik J. (American Geophysical Union, 2004-01-30)
    We measured vertical profiles of dimethylsulfide (DMS) in the atmospheric marine boundary layer from R/P FLIP during the 2000 FAIRS cruise. Applying Monin-Obukhov similarity theory to the DMS gradients and simultaneous ...
  • Bigorre, Sebastien P.; Weller, Robert A.; Lord, Jeffrey; Galbraith, Nancy R.; Whelan, Sean P.; Zappa, Christopher J.; Otto, William; Ram, Jessica; Vasquez, Raul; Suhm, Diane (Woods Hole Oceanographic Institution, 2010-05)
    The Ocean Reference Station at 20°S, 85°W under the stratus clouds west of northern Chile is being maintained to provide ongoing climate-quality records of surface meteorology, air-sea fluxes of heat, freshwater, and ...
  • Whelan, Sean P.; Lord, Jeffrey; Galbraith, Nancy R.; Weller, Robert A.; Farrar, J. Thomas; Grant, David; Grados, Carmen; de Szoeke, Simon P.; Moffat, Carlos F.; Zappa, Christopher J.; Yang, Mingxi; Straneo, Fiamma; Fairall, Christopher W.; Zuidema, Paquita; Wolfe, Dan; Miller, Matthew; Covert, David (Woods Hole Oceanographic Institution, 2009-04)
    The Ocean Reference Station at 20°S, 85°W under the stratus clouds west of northern Chile is being maintained to provide ongoing climate-quality records of surface meteorology; air-sea fluxes of heat, freshwater, and ...
  • Wells, Andrew J.; Cenedese, Claudia; Farrar, J. Thomas; Zappa, Christopher J. (American Meteorological Society, 2009-11)
    The aqueous thermal boundary layer near to the ocean surface, or skin layer, has thickness O(1 mm) and plays an important role in controlling the exchange of heat between the atmosphere and the ocean. Theoretical arguments ...

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