作者: K. Hutter , G. Bauer , Y. Wang , P. Güting
DOI: 10.1029/CE054P0137
关键词: Wave model 、 Geophysics 、 Nonlinear system 、 Climatology 、 Computation 、 Constant (mathematics) 、 Thermocline 、 Baroclinity 、 Barotropic fluid 、 Current (stream) 、 Geography
摘要: We report experiences gained with two different models that allow computation of the wind induced barotropic and baroclinic motion in lakes. These are: Nonlinear dispersive two-layered wave model (SPEM) implicit integration time. The first is used to demonstrate nonlinearities affect fine structure thermocline response when input strong. This shown by means computations a rectangular basin constant depth Lake Constance. version SPEM study Ekman problem trctangle Both concentrate upon role played diffudion predicting current temperature distribution estabished lakes under direct forcing.