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- W1663245087 abstract "Publisher Summary This chapter describes a layered wave equation model for thermally stratified flow. The dynamic behavior of stratified bodies of water is dramatically different from that of homogeneous bodies. It is well-known that large amplitude internal waves exist in lakes in temperate climates when thermal stratification develops in the summer months. This motion can induce substantial flows under the right wind conditions and hence, can play a significant role in the transport process in the main body of a lake. It can also induce exchange processes with the adjacent coves and bays. Internal waves have periods that are often orders of magnitude larger than the gravity waves based on the celerity of the same body under homogeneous conditions. The dynamic response of a thermally stratified body of water consists of the superposition of the homogeneous type waves, and the waves arising from stratification. As demonstrated, both waves are important to the solution and hence, the solution techniques must not mask or inadvertently filter out what might otherwise appear to be troublesome higher frequency components of the response." @default.
- W1663245087 created "2016-06-24" @default.
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- W1663245087 date "1988-01-01" @default.
- W1663245087 modified "2023-09-27" @default.
- W1663245087 title "A Layered Wave Equation Model for Thermally Stratified Flow" @default.
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- W1663245087 doi "https://doi.org/10.1016/s0167-5648(08)70356-3" @default.
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