Summertime increases in upper-ocean stratification and mixed-layer depth. [PDF]
Sallée JB +8 more
europepmc +1 more source
Estimation of the Mixed Layer Depth in the Indian Ocean from Surface Parameters: A Clustering-Neural Network Method. [PDF]
Gu C, Qi J, Zhao Y, Yin W, Zhu S.
europepmc +1 more source
The Metabolic Balance of Lake Superior's Mixed Layer
Understanding carbon (C) dynamics in large lake ecosystems poses challenges due to their size, causing uncertainty in their contribution to the global C cycle.
Panditha V. S. L. Gunawardana +5 more
doaj +1 more source
Role of Sea Surface Physical Processes in Mixed-Layer Temperature Changes During Summer Marine Heat Waves in the Chile-Peru Current System. [PDF]
Cooley KM +4 more
europepmc +1 more source
Mixing Within Patterned Vortex Core
The video shows the flow dynamics within inner and outer regions of a vortex core. The observed phenomena mimic a transport process occurring within the Antarctic vortex.
Abderrahmane, Hamid Ait +5 more
core
Seasonal mixed layer depth shapes phytoplankton physiology, viral production, and accumulation in the North Atlantic. [PDF]
Diaz BP +22 more
europepmc +1 more source
Probabilistic Machine Learning Estimation of Ocean Mixed Layer Depth From Dense Satellite and Sparse In Situ Observations. [PDF]
Foster D, Gagne DJ, Whitt DB.
europepmc +1 more source
A unified view of convective transports by stratocumulus clouds, shallow cumulus clouds, and deep convection [PDF]
A bulk planetary boundary layer (PBL) model was developed with a simple internal vertical structure and a simple second-order closure, designed for use as a PBL parameterization in a large-scale model. The model allows the mean fields to vary with height
Randall, David A.
core +1 more source
The origin of large and small particle axial bands in long rotating tumblers is a long-standing question. Using DEM simulations, we show that this axial segregation is due to a Rayleigh-Taylor instability which is characterized by the fact that the ...
Umberto D'Ortona +2 more
doaj +1 more source

