scholarly journals Zarys rozwoju badań termiki wód i pokrywy lodowej jezior w polskich Tatrach = A general review of research into waters’ thermal structure and lake ice cover in the Polish Tatra Mountains

2017 ◽  
Vol 89 (3) ◽  
pp. 491-512
Author(s):  
Mirosław Szumny
Keyword(s):  
Thermal Structure ◽  
Ice Cover ◽  
Tatra Mountains ◽  
Lake Ice ◽  
General Review ◽  
Lake Ice Cover

scholarly journals Calving Seasonality Associated With Melt‐Undercutting and Lake Ice Cover

2020 ◽  
Vol 47 (8) ◽  
Author(s):  
Joseph Mallalieu ◽  
Jonathan L. Carrivick ◽  
Duncan J. Quincey ◽  
Mark W. Smith
Keyword(s):  
Ice Cover ◽  
Lake Ice ◽  
Lake Ice Cover

Simulation of North American lake-ice cover characteristics under contemporary and future climate conditions

2011 ◽  
Vol 32 (5) ◽  
pp. 695-709 ◽  
Author(s):  
Yonas Dibike ◽  
Terry Prowse ◽  
Barrie Bonsal ◽  
Laurent de Rham ◽  
Tuomo Saloranta
Keyword(s):  
North American ◽  
Ice Cover ◽  
Future Climate ◽  
Lake Ice ◽  
Climate Conditions ◽  
Lake Ice Cover

scholarly journals Changes in Lake Ice Cover on the Morskie Oko Lake in Poland (1971-2007)

2013 ◽  
Vol 1 (2) ◽  
pp. 71-75
Author(s):  
Choiński Adam ◽  
Kolendowicz Leszek ◽  
Pociask-Karteczka Joanna ◽  
Sobkowiak Leszek
Keyword(s):  
Ice Cover ◽  
Lake Ice ◽  
Lake Ice Cover

scholarly journals Decay of a High Arctic lake-ice cover: observations and modelling

1994 ◽  
Vol 40 (135) ◽  
pp. 283-292 ◽  
Author(s):  
Richard Heron ◽  
Ming-Ko Woo
Keyword(s):  
Energy Balance ◽  
Ice Cover ◽  
High Arctic ◽  
Shortwave Radiation ◽  
Balance Model ◽  
Lake Ice ◽  
Ice Melt ◽  
Density Reduction ◽  
Ice Water ◽  
Lake Ice Cover

AbstractThe decay of a lake-ice cover in the Canadian High Arctic was studied for 2 years. Melt at the upper surface accounted for 75% of the decrease in ice thickness, while 25% occurred at the ice–water interface. An energy-balance model, incorporating density reduction due to internal ice melt, was used to simulate the decay of the ice cover. The overall performance of the model was satisfactory despite periods when computed results differed from the observed ice decay. Energy-balance calculations indicated that the absorption of shortwave radiation within the ice provided 52% of the melt energy while 33 and 15% came from the surface-energy balance and heat flux from the water.

scholarly journals Decay of a High Arctic lake-ice cover: observations and modelling

1994 ◽  
Vol 40 (135) ◽  
pp. 283-292 ◽  
Author(s):  
Richard Heron ◽  
Ming-Ko Woo
Keyword(s):  
Energy Balance ◽  
Ice Cover ◽  
High Arctic ◽  
Shortwave Radiation ◽  
Balance Model ◽  
Lake Ice ◽  
Ice Melt ◽  
Density Reduction ◽  
Ice Water ◽  
Lake Ice Cover

AbstractThe decay of a lake-ice cover in the Canadian High Arctic was studied for 2 years. Melt at the upper surface accounted for 75% of the decrease in ice thickness, while 25% occurred at the ice–water interface. An energy-balance model, incorporating density reduction due to internal ice melt, was used to simulate the decay of the ice cover. The overall performance of the model was satisfactory despite periods when computed results differed from the observed ice decay. Energy-balance calculations indicated that the absorption of shortwave radiation within the ice provided 52% of the melt energy while 33 and 15% came from the surface-energy balance and heat flux from the water.

Decadal Variability of Great Lakes Ice Cover in Response to AMO and PDO, 1963–2017

2018 ◽  
Vol 31 (18) ◽  
pp. 7249-7268 ◽  
Author(s):  
Jia Wang ◽  
James Kessler ◽  
Xuezhi Bai ◽  
Anne Clites ◽  
Brent Lofgren ◽  
...  
Keyword(s):  
Surface Temperature ◽  
Great Lakes ◽  
Regression Model ◽  
Decadal Variability ◽  
Ice Cover ◽  
Lake Surface ◽  
Lake Ice ◽  
Relationship Of ◽  
The Relationship ◽  
Lake Ice Cover

Abstract In this study, decadal variability of ice cover in the Great Lakes is investigated using historical airborne and satellite measurements from 1963 to 2017. It was found that Great Lakes ice cover has 1) a linear relationship with the Atlantic multidecadal oscillation (AMO), similar to the relationship of lake ice cover with the North Atlantic Oscillation (NAO), but with stronger impact than NAO; 2) a quadratic relationship with the Pacific decadal oscillation (PDO), which is similar to the relationship of lake ice cover to Niño-3.4, but with opposite curvature; and 3) decadal variability with a positive (warming) trend in AMO contributes to the decreasing trend in lake ice cover. Composite analyses show that during the positive (negative) phase of AMO, the Great Lakes experience a warm (cold) anomaly in surface air temperature (SAT) and lake surface temperature (LST), leading to less (more) ice cover. During the positive (negative) phase of PDO, the Great Lakes experience a cold (warm) anomaly in SAT and LST, leading to more (less) ice cover. Based on these statistical relationships, the original multiple variable regression model established using the indices of NAO and Niño-3.4 only was improved by adding both AMO and PDO, as well as their interference (interacting or competing) mechanism. With the AMO and PDO added, the correlation between the model and observation increases to 0.69, compared to 0.48 using NAO and Niño-3.4 only. When November lake surface temperature was further added to the regression model, the prediction skill of the coming winter ice cover increased even more.

Coherence between lake ice cover, local climate and teleconnections (Lake Mendota, Wisconsin)

2009 ◽  
Vol 374 (3-4) ◽  
pp. 282-293 ◽  
Author(s):  
Reza Namdar Ghanbari ◽  
Hector R. Bravo ◽  
John J. Magnuson ◽  
William G. Hyzer ◽  
Barbara J. Benson
Keyword(s):  
Ice Cover ◽  
Lake Ice ◽  
Local Climate ◽  
Lake Mendota ◽  
Lake Ice Cover
Sign in / Sign up

Export Citation Format

Share Document