Remote sensing of salinity using satellite-mounted microwave radiometers provides new
perspectives for studying ocean dynamics and the global hydrological cycle. Calibration and …

The dynamic of the thermohaline structure of the upper ocean, which depends on ocean–
atmosphere interactions, drives most near surface oceanic processes, including the control …

Abstract Changes in the Earth's water cycle can be estimated by analyzing sea surface
salinity. This variable reflects the balance between precipitation and evaporation over the …

Previous studies of the barrier layer (BL) and tropical cyclone (TC) intensification show
controversial results. Some studies suggest that the BL is favorable for TC intensification …

Surface layer temperature inversion (SLTI), a warm layer sandwiched between surface and
subsurface colder waters, has been reported to frequently occur in conjunction with barrier …

Future changes in the southeastern tropical Atlantic interannual sea surface temperature
(SST) variability in response to increasing greenhouse gas concentrations are investigated …

An analysis is presented for the spatial and intensity distributions of North Atlantic extreme
atmospheric events crossing the buoyant Amazon‐Orinoco freshwater plume. The sea …

Abstract During the Bay of Bengal (BoB) Boundary Layer Experiment (BoBBLE) in the
southern BoB, time series of microstructure measurements were obtained at 8° N, 89° E from …

In the eastern Gulf of Guinea (GG), freshwater originated from rivers discharges into the
ocean and high precipitation rate are key contributors to the upper ocean vertical density …

The seasonal evolution of vertical diffusivity at the base of the mixed layer (ML) in the Bay of
Bengal (BoB) region was inferred using Argo observations from 2016 to 2018. The ML heat …