Characteristics and Modelling of Physical Limnology Processes |
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_ Fig air/water amplitude atmospheric pressure bottom boundary conditions cause characterizes components considered constant Coriolis Coriolis force current velocity decreases Defant depends depth H described direction drag coefficient drift current dynamical processes effect Ekman energy epilimnion equation evaluated evaporation external finite-difference flow fluid forces friction geomorphometry given gradient currents horizontal Hutchinson l957 hydrostatic equation hypolimnion ice cover increase interface internal waves isotherms Lac Leman Lake of Constance Lake of Zurich lake waters limnology mean water modelling technique momentum motion numerical modelling observed obtain occurs oceanography oscillations oxygen parameter period phenomena physical limnology pressure gradients regions role saline seiche seiche-like shallow water shear stress solar radiation solution speed storm surges surface area surface water thermal thermocline tion turbulent uninodal vertical water basin water circulation water column water level variations water masses water surface water temperature whereas wind action wind velocity wód yields