El Niño and the Southern Oscillation (ENSO) is a naturally occurring fluctuation of the
climate system that is generated in the tropical Pacific through interactions between the …

Wind is the primary driver of the oceanic general circulation, yet the length scales at which
this energy transfer occurs are unknown. Using satellite data and a recent method to …

Antarctic sea ice extent (SIE) has slightly increased over the satellite observational period
(1979 to the present) despite global warming. Several mechanisms have been invoked to …

Abstract The observed upper (0–50 m) Arctic Ocean warming since 1979 has been primarily
attributed to anthropogenically driven changes in the high latitudes. Here, using both …

The Cross-Calibrated Multi-Platform (CCMP) Ocean vector wind analysis is a level-4 product
that uses a variational method to combine satellite retrievals of ocean winds with a …

The global upper ocean has been warming during the last decades accompanied with a
chlorophyll‐a (Chl‐a) and productivity decrease. Whereas subtropical gyres show similar …

Mesoscale eddies are present everywhere in the ocean and partly determine the mean state
of the circulation and ecosystem. The current feedback on the surface wind stress modulates …

The current feedback to the atmosphere (CFB) contributes to the oceanic circulation by
damping eddies. In an ocean‐atmosphere coupled model, CFB can be correctly accounted …

Wave hindcasts are tools to study climate and are regularly used in offshore and coastal
engineering applications. The growing number of wind datasets and reanalysis products …

The increasing science and society requests for ocean monitoring from global to regional
and local scales, the need for integration and convergence into a globally consistent ocean …