- We will send in 10–14 business days.
/images/books/13175155/9783639108521.jpg)
- Author: Hyuck Chung
- Publisher: VDM Verlag
- ISBN-10: 3639108523
- ISBN-13: 9783639108521
- Format: 15.2 x 22.9 x 0.8 cm, softcover
- Language: English
- SAVE -10% with code: EXTRA
Mathematical Studies of Wave Propagation in Sea-ice Sea-ice Dynamics (e-book) (used book) | bookbook.eu
Reviews
Description
During the winter months the sea around the coast of Antarctica freezes and form a vast area of ice covered region. The ice sheets found in this area are large and apparently featureless. Therefore a large-scale sea ice sheet has been modeled as a thin elastic plate for small deflection. Partial differential equations are derived to describe vertical deflection of a thin elastic plate coupled with incompressible fluid. The Fourier transform is used to derive the vertical deflection of the ice sheet. A fundamental solution can be expressed by infinite summations of fractional functions at complex roots of the dispersion equation. The Fundamental solution is reduced to a sum of special functions at three roots of a fifth order polynomial when the water depth is infinite. The reflection and transmission of wave energy between two semi-infinite ice sheets joined by a straight-line transition is considered. Analytical formulas for the modal expansion of the waves in the ice sheet are derived using the Wiener-Hopf technique. This monograph should be a good introduction for post-graduate students to the linear hydro-elasticity.
EXTRA 10 % discount with code: EXTRA
The promotion ends in 18d.05:59:30
The discount code is valid when purchasing from 10 €. Discounts do not stack.
- Author: Hyuck Chung
- Publisher: VDM Verlag
- ISBN-10: 3639108523
- ISBN-13: 9783639108521
- Format: 15.2 x 22.9 x 0.8 cm, softcover
- Language: English English
During the winter months the sea around the coast of Antarctica freezes and form a vast area of ice covered region. The ice sheets found in this area are large and apparently featureless. Therefore a large-scale sea ice sheet has been modeled as a thin elastic plate for small deflection. Partial differential equations are derived to describe vertical deflection of a thin elastic plate coupled with incompressible fluid. The Fourier transform is used to derive the vertical deflection of the ice sheet. A fundamental solution can be expressed by infinite summations of fractional functions at complex roots of the dispersion equation. The Fundamental solution is reduced to a sum of special functions at three roots of a fifth order polynomial when the water depth is infinite. The reflection and transmission of wave energy between two semi-infinite ice sheets joined by a straight-line transition is considered. Analytical formulas for the modal expansion of the waves in the ice sheet are derived using the Wiener-Hopf technique. This monograph should be a good introduction for post-graduate students to the linear hydro-elasticity.
Reviews