Romain Caneill
YOU?
Author Swipe
View article: Sea-ice turbulent dynamics derived from Lagrangian buoys tracks
Sea-ice turbulent dynamics derived from Lagrangian buoys tracks Open
The Arctic, a central place to our global climate, is mainly covered by sea ice. The motion of sea ice is important as it exports freshwater from the central Arctic to the North Atlantic. The motion itself is on a large scale driven by atm…
View article: The Southern Ocean deep mixing band emerges from a competition between winter buoyancy loss and upper stratification strength
The Southern Ocean deep mixing band emerges from a competition between winter buoyancy loss and upper stratification strength Open
The Southern Ocean hosts a winter deep mixing band (DMB) near the Antarctic Circumpolar Current's (ACC) northern boundary, playing a pivotal role in Subantarctic Mode Water formation. Here, we investigate what controls the presence and geo…
View article: Reply on RC2
Reply on RC2 Open
Abstract. The Southern Ocean hosts a winter deep mixing band (DMB) near the Antarctic Circumpolar Current's (ACC) northern boundary, playing a pivotal role in Subantarctic Mode Water formation. Here, we investigate what controls the presen…
View article: Reply on RC1
Reply on RC1 Open
Abstract. The Southern Ocean hosts a winter deep mixing band (DMB) near the Antarctic Circumpolar Current's (ACC) northern boundary, playing a pivotal role in Subantarctic Mode Water formation. Here, we investigate what controls the presen…
View article: Southern Ocean deep mixing band emerges from a competition between winter buoyancy loss and upper stratification strength
Southern Ocean deep mixing band emerges from a competition between winter buoyancy loss and upper stratification strength Open
The Southern Ocean hosts a winter deep mixing band (DMB) near the Antarctic Circumpolar Current's (ACC) northern boundary, playing a pivotal role in Subantarctic Mode Water formation. Here, we investigate what controls the presence and geo…
View article: NEMO BASIN example for xgcm
NEMO BASIN example for xgcm Open
This is a dataset taken as the time mean of the last 50 years of the reference run of caneill et al. 2022, JPO, The polar transition from alpha to beta regions set by a surface buoyancy flux inversion., https://doi.org/10.1175/JPO-D-21-029…
View article: NEMO BASIN example for xgcm
NEMO BASIN example for xgcm Open
This is a dataset taken as the time mean of the last 50 years of the reference run of caneill et al. 2022, JPO, The polar transition from alpha to beta regions set by a surface buoyancy flux inversion., https://doi.org/10.1175/JPO-D-21-029…
View article: The Influence of Surface Buoyancy Flux and Ekman transport on Upper Ocean Pycnocline Stratification in the Southern Ocean.
The Influence of Surface Buoyancy Flux and Ekman transport on Upper Ocean Pycnocline Stratification in the Southern Ocean. Open
In this study, we examine the factors that influence upper ocean pycnocline (UOP) stratification in the Southern Ocean. The UOP is a layer located just below the mixed layer and its stratification controls the rates of exchange of heat, ca…
View article: Unique thermal expansion properties of water key to the formation of sea ice on Earth
Unique thermal expansion properties of water key to the formation of sea ice on Earth Open
The formation of sea ice in polar regions is possible because a salinity gradient or halocline keeps the water column stable despite intense cooling. Here, we demonstrate that a unique water property is central to the maintenance of the po…
View article: The Polar Transition from Alpha to Beta Regions Set by a Surface Buoyancy Flux Inversion
The Polar Transition from Alpha to Beta Regions Set by a Surface Buoyancy Flux Inversion Open
The stratification is primarily controlled by temperature in subtropical regions (alpha ocean) and by salinity in subpolar regions (beta ocean). Between these two regions lies a transition zone, often characterized by deep mixed layers in …
View article: How nonlinearities of the equation of state of seawater generate the polar halocline and promote sea ice formation
How nonlinearities of the equation of state of seawater generate the polar halocline and promote sea ice formation Open
<p>The equation of state of seawater determines how density varies with temperature and salinity. Although it has long been known that the equation of state is nonlinear, there seems to be an overall feeling in the physical oceanogra…
View article: caneill et al. The polar transition from alpha to beta regions set by a surface buoyancy flux inversion.
caneill et al. The polar transition from alpha to beta regions set by a surface buoyancy flux inversion. Open
NEMO outputs used for the paper Caneill, R., Roquet, F., Madec, G., and Nycander, J. (2022). The polar transition from alpha to beta regions set by a surface buoyancy flux inversion. Journal of Physical Oceanography. https://doi.org/10.117…
View article: caneill et al. The polar transition from alpha to beta regions set by a surface buoyancy flux inversion.
caneill et al. The polar transition from alpha to beta regions set by a surface buoyancy flux inversion. Open
NEMO outputs used for the paper Caneill, R., Roquet, F., Madec, G., and Nycander, J. (2022). The polar transition from alpha to beta regions set by a surface buoyancy flux inversion. Journal of Physical Oceanography. https://doi.org/10.117…
View article: NEMO 4.0 Basin test data
NEMO 4.0 Basin test data Open
Test data from NEMO 4.0. Used for developing python tools to open NEMO raw netCDF output and make them readable by xgcm. This version uses the mesh_mask and domain_cfg_out outputed by only 1 processor.
View article: NEMO 4.0 Basin test data
NEMO 4.0 Basin test data Open
Test data from NEMO 4.0. Used for developing python tools to open NEMO raw netCDF output and make them readable by xgcm. This version uses the mesh_mask and domain_cfg_out outputed by only 1 processor.
View article: NEMO 4.0 Basin test data
NEMO 4.0 Basin test data Open
Test data from NEMO 4.0. Used for developing python tools to open NEMO raw netCDF output and make them readable by xgcm.
View article: What determines the position of the transition zone between alpha and beta regions in the ocean? A model study.
What determines the position of the transition zone between alpha and beta regions in the ocean? A model study. Open
<p>The stratification is primarily controlled by the temperature in subtropical regions (alpha ocean), and by salinity in subpolar regions (beta ocean). Between these two regions lies a transition zone where intense frontal systems a…
View article: NEMO BASIN test data
NEMO BASIN test data Open
Small NEMO dataset, used to develop python tools and documentation.
View article: NEMO BASIN test data
NEMO BASIN test data Open
Small NEMO dataset, used to develop python tools and documentation.
View article: Observation of the process of snow accumulation on the Antarctic Plateau by time lapse laser scanning
Observation of the process of snow accumulation on the Antarctic Plateau by time lapse laser scanning Open
Snow accumulation is the main positive component of the mass balance in Antarctica. In contrast to the major efforts deployed to estimate its overall value on a continental scale – to assess the contribution of the ice sheet to sea level r…