Leeuwin Current SST perturbation causes significant wind speed and wind stress curl anomalies along the current core

Perturbation wind stress curl drives anomalous downwelling and would reduce surface chlorophyll a concentrations along the LC SST front

The relationships between perturbation SST and perturbation wind and their derivatives in the LC have obvious seasonal variations

Assessment of an eddying 1/12° ocean reanalysis with non-assimilated hydrographic observations along 59.5N in the Atlantic.

Reliable representation of the 0-700 m heat content but flaws in overflow waters due to a lack of deep observations.

Reliable reproduction outside the western boundary current of the major mesoscale eddy features that contribute to the meridional transport.

This paper introduces the Ocean State Ocean Model (OSOM), a Regional Ocean Modeling System (ROMS) implementation focused on the Rhode Island region.

The predictability of the OSOM is evaluated using information theory and initial condition ensembles in summer and winter conditions.

The flushing time scales (freshwater and salinity) of Narragansett and Mt. Hope Bays are calculated and resemble the predictability timescales, indicating that predictability is largely governed by the estuarine circulation in this model.

Eddy kinetic energy (EKE) computed from altimetry crossovers can well represent EKE changes in the Southern Ocean.

No coherent increase in EKE over all areas of the Southern Ocean was identified since 1993.

EKE in the Southern Ocean has increased since 1993 in one region that is downstream of the Campbell Plateau.

70–80% of the dissolved organic carbon exported from the tropical peatlands is remineralized in the Sunda Shelf Sea

This drives a seasonal decline in pH by 0.1 and a net CO₂ efflux of 2.4 – 4.9 mol m^-2 yr^-1 in the central Sunda Shelf

20–30% of the peatland-derived dissolved organic carbon might be relatively refractory and exported to the open Indian Ocean

A realistic sub-ice platelet layer emerges in a one-dimensional thermodynamic sea ice model when suitably forced

Key influences are heat loss to water column, thermal insulation by ice and snow, and brine convection between platelet crystals

The sub-ice platelet layer is stabilized by its high liquid content and isothermal character

Eddies identified and quantified in a new comprehensive census for the Indo-Australian Basin

Newly identified hotspots for eddy activity identified in the eastern basin

More than 41% of eddies detected than in previous surveys

Substantial sea surface temperature cooling occurred in the Banda Sea associated with the 2015 boreal winter Madden-Julian Oscillation.

Enhanced vertical mixing associated with the MJO contributes more than surface heat flux for driving this extreme SST cooling.

Elevated thermocline associated with the 2015 strong El Niño is largely responsible for the intensified SST cooling.

Two types of shoreward nonlinear internal waves south of the Hainan Island are identified by analyzing multiple SAR images.

The two types of nonlinear internal waves have different source sites and generation mechanisms.

Background current can greatly affect the nonlinear evolution of the internal waves.

A deep neural network (DNN) model is developed for the acquisition of significant wave heights from CFOSAT SWIM spectra.

Additional positive impacts are found in the assimilation of the SWIM box SWH from the DNN compared to the assimilation of nadir SWH only.