scholarly journals Results from the implementation of the elastic viscous plastic sea ice rheology in HadCM3

2006 ◽  
Vol 3 (4) ◽  
pp. 777-803
Author(s):  
W. Connolley ◽  
A. Keen ◽  
A. McLaren
Keyword(s):  
Sea Ice ◽  
Large Scale ◽  
Climate Model ◽  
Ice Dynamics ◽  
Sea Ice Dynamics ◽  
Future Improvement ◽  
Physically Based ◽  
Solid Foundation ◽  
Hadley Centre ◽  
Better Than

Abstract. We present results of an implementation of the Elastic Viscous Plastic (EVP) sea ice dynamics scheme into the Hadley Centre coupled ocean-atmosphere climate model HadCM3. Although the large-scale simulation of sea ice in HadCM3 is quite good with this model, the lack of a full dynamical model leads to errors in the detailed representation of sea ice and limits our confidence in its future predictions. We find that introducing the EVP scheme results in a worse initial simulation of the sea ice. This paper documents various improvements made to improve the simulation, resulting in a sea ice simulation that is better than the original HadCM3 scheme overall. Importantly, it is more physically based and provides a more solid foundation for future improvement. We then consider the interannual variability of the sea ice in the new model and demonstrate improvements over the HadCM3 simulation.

scholarly journals Results from the implementation of the Elastic Viscous Plastic sea ice rheology in HadCM3

Ocean Science ◽  
2006 ◽  
Vol 2 (2) ◽  
pp. 201-211 ◽  
Author(s):  
W. M. Connolley ◽  
A. B. Keen ◽  
A. J. McLaren
Keyword(s):  
Sea Ice ◽  
Large Scale ◽  
Climate Model ◽  
Ice Dynamics ◽  
Sea Ice Dynamics ◽  
Ocean Atmosphere ◽  
Physically Based ◽  
Solid Foundation ◽  
Hadley Centre ◽  
Better Than

Abstract. We present results of an implementation of the Elastic Viscous Plastic (EVP) sea ice dynamics scheme into the Hadley Centre coupled ocean-atmosphere climate model HadCM3. Although the large-scale simulation of sea ice in HadCM3 is quite good with this model, the lack of a full dynamical model leads to errors in the detailed representation of sea ice and limits our confidence in its future predictions. We find that introducing the EVP scheme results in a worse initial simulation of the sea ice. This paper documents various enhancements made to improve the simulation, resulting in a sea ice simulation that is better than the original HadCM3 scheme overall. Importantly, it is more physically based and provides a more solid foundation for future development. We then consider the interannual variability of the sea ice in the new model and demonstrate improvements over the HadCM3 simulation.

Sea‐ice dynamics and CO2sensitivity in a global climate model

1994 ◽  
Vol 32 (2) ◽  
pp. 449-467 ◽  
Author(s):  
David Pollard ◽  
Starley L. Thompson
Keyword(s):  
Sea Ice ◽  
Climate Model ◽  
Global Climate ◽  
Global Climate Model ◽  
Ice Dynamics ◽  
Sea Ice Dynamics

scholarly journals On a Simple Sea-Ice Dynamics Model for Climate Studies

1990 ◽  
Vol 14 ◽  
pp. 72-77 ◽  
Author(s):  
G.M. Flato ◽  
W.D. Hibler
Keyword(s):  
Sea Ice ◽  
Large Scale ◽  
Wind Fields ◽  
Fluid Approximation ◽  
Ice Dynamics ◽  
Monthly Average ◽  
Sea Ice Dynamics ◽  
Average Wind ◽  
Cavitating Fluid ◽  
Climate Studies

Sea-ice motion and dynamic thickness build-up play an important role in the transfer of heat between the ocean and the atmosphere and so must be included in large-scale climate studies. A “cavitating-fluid” approximation allows these dynamic processes to be parameterized in a simple way by ignoring shear and tensile strength yet retaining compressive strength. A simple procedure for approximating a cavitating fluid is presented here and is compared to the more complete viscous-plastic sea-ice model by performing several three year simulations with daily varying and monthly average wind forcing. Although differences exist on a monthly basis, the two models compare favourably over a seasonal cycle, particularly when compared to a thermodynamics only model in which ice motion is ignored. The lack of shear strength in a cavitating-fluid approximation makes it less sensitive to smoothing of the wind fields (as demonstrated by the monthly average wind simulations); however it also changes the detailed circulation and thickness build-up patterns somewhat. Overall, the cavitating-fluid approximation shows considerable promise for including sea-ice dynamics in large-scale climate models, especially where averaged wind fields are employed.

scholarly journals Demographic, ecological, and physiological responses of ringed seals to an abrupt decline in sea ice availability

PeerJ ◽  
2017 ◽  
Vol 5 ◽  
pp. e2957 ◽  
Author(s):  
Steven H. Ferguson ◽  
Brent G. Young ◽  
David J. Yurkowski ◽  
Randi Anderson ◽  
Cornelia Willing ◽  
...  
Keyword(s):  
Sea Ice ◽  
Body Condition ◽  
Large Scale ◽  
Southern Oscillation ◽  
High Stress ◽  
Open Water ◽  
Hudson Bay ◽  
Ice Dynamics ◽  
Southern Limit ◽  
Sea Ice Dynamics

To assess whether demographic declines of Arctic species at the southern limit of their range will be gradual or punctuated, we compared large-scale environmental patterns including sea ice dynamics to ringed seal (Pusa hispida) reproduction, body condition, recruitment, and stress in Hudson Bay from 2003 to 2013. Aerial surveys suggested a gradual decline in seal density from 1995 to 2013, with the lowest density occurring in 2013. Body condition decreased and stress (cortisol) increased over time in relation to longer open water periods. The 2010 open water period in Hudson Bay coincided with extremes in large-scale atmospheric patterns (North Atlantic Oscillation, Arctic Oscillation, El Nino-Southern Oscillation) resulting in the earliest spring breakup and the latest ice formation on record. The warming event was coincident with high stress level, low ovulation rate, low pregnancy rate, few pups in the Inuit harvest, and observations of sick seals. Results provide evidence of changes in the condition of Arctic marine mammals in relation to climate mediated sea ice dynamics. We conclude that although negative demographic responses of Hudson Bay seals are occurring gradually with diminishing sea ice, a recent episodic environmental event played a significant role in a punctuated population decline.

scholarly journals Demographic, ecological and physiological responses of ringed seals to an abrupt decline in sea ice availability

2016 ◽  
Author(s):  
Steven H Ferguson ◽  
Brent G Young ◽  
David J Yurkowski ◽  
Randi Anderson ◽  
Cornelia Willing ◽  
...  
Keyword(s):  
Sea Ice ◽  
Body Condition ◽  
Large Scale ◽  
Population Decline ◽  
Open Water ◽  
Hudson Bay ◽  
Ice Dynamics ◽  
Southern Limit ◽  
Environmental Event ◽  
Sea Ice Dynamics

To assess whether demographic declines of Arctic species at the southern limit of their range will be gradual or punctuated, we compared large-scale environmental patterns including sea ice dynamics to ringed seal (Pusa hispida ) reproduction, body condition, recruitment, and stress in Hudson Bay from 2003-2013. Aerial surveys suggested a gradual decline in seal density from 1995-2013, with the lowest density occurring in 2013. Body condition decreased and stress (cortisol) increased over time in relation to longer open waterperiods. The 2010 open water period in Hudson Bay coincided with extremes in large-scale atmospheric patterns (NAO, AO, ENSO) resulting in the earliest spring breakup and the latest ice formation on record. The warming event was coincident with the highest stress levels and the lowest recorded ovulation rate and low pregnancy rate, few pups in the Inuit harvest, and observations of sick seals. We conclude that although negative demographic responses of Hudson Bay seals are occurring gradually with diminishing sea ice, a recent episodic environmental event played a significant role in a punctuated population decline.

scholarly journals On a Simple Sea-Ice Dynamics Model for Climate Studies

1990 ◽  
Vol 14 ◽  
pp. 72-77 ◽  
Author(s):  
G.M. Flato ◽  
W.D. Hibler
Keyword(s):  
Sea Ice ◽  
Large Scale ◽  
Wind Fields ◽  
Fluid Approximation ◽  
Ice Dynamics ◽  
Monthly Average ◽  
Sea Ice Dynamics ◽  
Average Wind ◽  
Cavitating Fluid ◽  
Climate Studies

Sea-ice motion and dynamic thickness build-up play an important role in the transfer of heat between the ocean and the atmosphere and so must be included in large-scale climate studies. A “cavitating-fluid” approximation allows these dynamic processes to be parameterized in a simple way by ignoring shear and tensile strength yet retaining compressive strength. A simple procedure for approximating a cavitating fluid is presented here and is compared to the more complete viscous-plastic sea-ice model by performing several three year simulations with daily varying and monthly average wind forcing. Although differences exist on a monthly basis, the two models compare favourably over a seasonal cycle, particularly when compared to a thermodynamics only model in which ice motion is ignored. The lack of shear strength in a cavitating-fluid approximation makes it less sensitive to smoothing of the wind fields (as demonstrated by the monthly average wind simulations); however it also changes the detailed circulation and thickness build-up patterns somewhat. Overall, the cavitating-fluid approximation shows considerable promise for including sea-ice dynamics in large-scale climate models, especially where averaged wind fields are employed.

Mathematical features of Hibler's model of large-scale sea-ice dynamics

1995 ◽  
Vol 47 (3) ◽  
pp. 179-230 ◽  
Author(s):  
Eckhard Kleine ◽  
Sergey Sklyar
Keyword(s):  
Sea Ice ◽  
Large Scale ◽  
Ice Dynamics ◽  
Sea Ice Dynamics

scholarly journals The Drake Passage opening from an experimental fluid dynamics point of view

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Miklós Vincze ◽  
Tamás Bozóki ◽  
Mátyás Herein ◽  
Ion Dan Borcia ◽  
Uwe Harlander ◽  
...  
Keyword(s):  
Fluid Dynamics ◽  
Sea Ice ◽  
Ocean Circulation ◽  
Climate Model ◽  
Global Climate Model ◽  
Drake Passage ◽  
Laboratory Model ◽  
Climate History ◽  
Ice Dynamics ◽  
Sea Ice Dynamics

AbstractPronounced global cooling around the Eocene–Oligocene transition (EOT) was a pivotal event in Earth’s climate history, controversially associated with the opening of the Drake Passage. Using a physical laboratory model we revisit the fluid dynamics of this marked reorganization of ocean circulation. Here we show, seemingly contradicting paleoclimate records, that in our experiments opening the pathway yields higher values of mean water surface temperature than the “closed” configuration. This mismatch points to the importance of the role ice albedo feedback plays in the investigated EOT-like transition, a component that is not captured in the laboratory model. Our conclusion is supported by numerical simulations performed in a global climate model (GCM) of intermediate complexity, where both “closed” and “open” configurations were explored, with and without active sea ice dynamics. The GCM results indicate that sea surface temperatures would change in the opposite direction following an opening event in the two sea ice dynamics settings, and the results are therefore consistent both with the laboratory experiment (slight warming after opening) and the paleoclimatic data (pronounced cooling after opening). It follows that in the hypothetical case of an initially ice-free Antarctica the continent could have become even warmer after the opening, a scenario not indicated by paleotemperature reconstructions.

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