Mode of forcing a passage through the ice

Englantilaisen tutkimusmatkaajan E. D. Clarken Ahvenanmeren ylitys joulukuussa 1799. - Digitoitu valokuvasta, joka julkaistu kirjassa: R. Knapas & P. Koistinen, Historiallisia kuvia, 1993.

Perilous passage on the ice

London : Joseph Mawman 1802

Travelling on the Ice over the Gulf of Bothnia to Finland

London : Joseph Mawman 1802

World Heritage of the Kvarken Archipelago : Echoes of the Ice Age

The Kvarken Archipelago is Finland’s first Unesco Natural Heritage Site. The story of the Kvarken Archipelago began about 10.000 years ago when the melting of the continental ice sheet as it retreated gave rise to this unique archipelago. The land once forced down by the mass of ice is now gradually rising and continuously creating new landscapes. People, animals and plants have learnt to adjust to their changing conditions in exceptional ways. The Ice Age may be over in Kvarken, but the drama still continues to unfold.

A multibody dynamic model of the cross-country ski-skating technique

The objective of this thesis is the development of a multibody dynamic model matching the observed movements of the lower limb of a skier performing the skating technique in cross-country style. During the construction of this model, the formulation of the equation of motion was made using the Euler - Lagrange approach with multipliers applied to a multibody system in three dimensions. The description of the lower limb of the skate skier and the ski was completed by employing three bodies, one representing the ski, and two representing the natural movements of the leg of the skier. The resultant system has 13 joint constraints due to the interconnection of the bodies, and four prescribed kinematic constraints to account for the movements of the leg, leaving the amount of degrees of freedom equal to one. The push-off force exerted by the skate skier was taken directly from measurements made on-site in the ski tunnel at the Vuokatti facilities (Finland) and was input into the model as a continuous function. Then, the resultant velocities and movement of the ski, center of mass of the skier, and variation of the skating angle were studied to understand the response of the model to the variation of important parameters of the skate technique. This allowed a comparison of the model results with the real movement of the skier. Further developments can be made to this model to better approximate the results to the real movement of the leg. One can achieve this by changing the constraints to include the behavior of the real leg joints and muscle actuation. As mentioned in the introduction of this thesis, a multibody dynamic model can be used to provide relevant information to ski designers and to obtain optimized results of the given variables, which athletes can use to improve their performance.

Track of HSMS Sophia tracing the extent of navigable water along the main northern ice between Spitzbergen and Greenland September 1868 : also showing the nature of the ice and temperature and depth of the sea

Kartta kuuluu A. E. Nordenskiöldin kokoelmaan