Search Results

You are looking at 1 - 1 of 1 items for :

  • Diabatic heating x
  • Third THORPEX International Science Symposium x
  • All content x
Clear All
Sharanya J. Majumdar, Kathryn J. Sellwood, Daniel Hodyss, Zoltan Toth, and Yucheng Song

explained by downstream baroclinic development. Processes such as stationary waves initiated by orographic forcing or zonal variations in diabatic heating (e.g., Hoskins and Valdes 1990 ) may act to decrease eddy activity and complicate the picture of downstream baroclinic development over the continent. In summary, baroclinic energy conversion is hypothesized to dominate upstream, in locations over the western Pacific Ocean off Japan, while the storm track is extended in the central Pacific via

Full access