Search Results

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

  • Deep learning x
  • Earth’s Energy Imbalance and Energy Flows through the Climate System x
  • Refine by Access: All Content x
Clear All
Michael Mayer, Steffen Tietsche, Leopold Haimberger, Takamasa Tsubouchi, Johannes Mayer, and Hao Zuo

in the ERA5 results truncated at T180 ( Fig. 5b ). The higher resolution also brings out very clearly the prominent local minimum in air–sea fluxes in the Icelandic Sea that has been documented by Moore et al. (2012) . However, it is evident that at T180 some spectral noise creeps in as well. The air–sea heat flux along the ice edge plays a vital role in open ocean deep convection in Greenland and Iceland Seas that contributes to Denmark Strait overflow water ( Moore et al. 2015 ; Brakstad et

Open access