Ice and shore formations caused by the movement of lake ice were studied in Lappajärvi from the winter of 1971‑72 to that of 1975‑76. The formations are described and classified on the basis of surveys and transverse sections, and an attempt is made to determine the dependence of these movements and their effects upon meteorological, hydrological and geomorphological factors. The results enable two models of process‑response systems to be set up for thermal and wind‑induced movements of lake ice. The principal regulator of the extent of thermal movement proved to be the depth and heat conductivity of the snow cover, while the form and structure of the ice‑push lake ramparts is governed by the slope, material, frost depth and vegetation cove...
During late winter (18 March–7 April 1994), temperature and current measurements were made in Lake V...
A series of limnological experiments were carried out in Lake Takanamiike, a typical seepage lake, i...
A field study was carried out in three small shallow ice-covered lakes to study heat and mass fluxes...
Exceptionally pronounced thermal movement of lake ice during the winter of 1972‑73 led to the format...
Wintertime observations in Lake Pääjärvi have been made since the beginning of the 20th century. In ...
First, the change in length with temperature of ice frozen on Lake Suwa was measured with an apparat...
During late winter (18 March-7 April 1994), temperature and current measurements were made in Lake V...
In winter in Finland the land is covered by snow, fresh water bodies as well as the neighbouring are...
A field study on the temperature, salt content, and density regime in three shallow ice-covered Kare...
The formation of ice ramparts caused by the thermal expansion of the lake ice is explained statistic...
The environmental conditions of the littoral zone were studied in the regulated Lake Ontojärvi and t...
Lake Pääjärvi in southern Finland freezes over every winter and the ice cover is static. The structu...
About 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the d...
Six visits between July 1996 and July 1997 were made from Finland to measure temperatures at depths ...
Glacial landforms of the Lake Kuittijärvi area, Russian Karelia, which covers an area of more than 7...
During late winter (18 March–7 April 1994), temperature and current measurements were made in Lake V...
A series of limnological experiments were carried out in Lake Takanamiike, a typical seepage lake, i...
A field study was carried out in three small shallow ice-covered lakes to study heat and mass fluxes...
Exceptionally pronounced thermal movement of lake ice during the winter of 1972‑73 led to the format...
Wintertime observations in Lake Pääjärvi have been made since the beginning of the 20th century. In ...
First, the change in length with temperature of ice frozen on Lake Suwa was measured with an apparat...
During late winter (18 March-7 April 1994), temperature and current measurements were made in Lake V...
In winter in Finland the land is covered by snow, fresh water bodies as well as the neighbouring are...
A field study on the temperature, salt content, and density regime in three shallow ice-covered Kare...
The formation of ice ramparts caused by the thermal expansion of the lake ice is explained statistic...
The environmental conditions of the littoral zone were studied in the regulated Lake Ontojärvi and t...
Lake Pääjärvi in southern Finland freezes over every winter and the ice cover is static. The structu...
About 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the d...
Six visits between July 1996 and July 1997 were made from Finland to measure temperatures at depths ...
Glacial landforms of the Lake Kuittijärvi area, Russian Karelia, which covers an area of more than 7...
During late winter (18 March–7 April 1994), temperature and current measurements were made in Lake V...
A series of limnological experiments were carried out in Lake Takanamiike, a typical seepage lake, i...
A field study was carried out in three small shallow ice-covered lakes to study heat and mass fluxes...