Activities proposal reviewer for nsf. Turbulent mixing levels in the ocean are quantified as a vertical or diapycnal diffusivity (kv). The ocean is vast, dynamic, and often inaccessible.
For lunch, i came prepared this time, bringing a sandwich with me to avoid the long queue times at food stalls around the conference center. In the north atlantic, ocean currents shift 1 petawatt of heat from the equator northward to the pole. 1 introduction the phenomenon of oceanic tides has been observed and studied by humanity for centuries.
Tuesday’s lunch was another type of ‘job. Success in localized tidal prediction and in the general understanding of tidal. It connects the shore to the open ocean by. Through modeling, scientists can simulate its behavior and better understand its role in earth's systems.
The magnitude of the ocean’s influence is bewilderingly large.