Oceanic current forcing in spectral wave models have recently been demonstrated to have
a large impact on wave heights at scales between one and up to several hundred kilometers. …

Accurate estimates of extreme waves are central for maritime activities, and stochastic wave
models are the best option available for practical applications. However, the way currents …

The Lofoten Maelstrom has been known for centuries as one of the strongest open-ocean
tidal currents in the world, estimated to reach 3 ms −1 , and by some estimates as much as 5 …

Lateral changes in the group velocity of waves propagating in oceanic or coastal waters
causes a deflection in their propagation path. The change in direction is called refraction and …

The attenuation of surface gravity waves is an important process associated with air–sea
and wave–current interactions. Here we investigate experimentally the attenuation of …

Surface currents and turbulent mixing were observed during a near-inertial wave (NIW)
using an accousting doppler current profiler (ADCP) and satellite-tracked drifters. Drifter …

Inertial motion units (IMUs) are used to perform measurements of waves in water covered by
landfast ice close to the ice edge in Svalbard. The effective noise level of the instruments is …

Because of better precision and intercompatibility, the use of lean body mass (LBM) as a
mass estimate in the calculation of SUV (SUL) has become more common in research and …

Due to better precision and intercompatibility, the use of lean body mass (LBM) as mass
estimate in the calculation of standardized uptake values (SUV) has become more common in …

Air bubbles in the upper ocean are generated mainly by wave breaking at the air-sea
interface. As such, after the waves break, entrained air bubbles evolve in the turbulent flow, …