Temperature and salt content regimes in three shallow ice-covered lakes 2. Heat and mass fluxes
A field study was carried out in three small shallow ice-covered lakes to study heat and mass fluxes and their spatial and temporal variability. During the main part of the winter, the heat flux at the ice-water interface, being of the order 0.5-1, W m(-2), was dominated by conduction from water to ice and did not show any significant variations in time or space. The heat flux from sediments to wa
