[M-IS15] Geophysical fluid dynamics-Transfield approach to geoscience

Sun. May 20, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Keita Iga(Atmosphere and Ocean Research Institute, The University of Tokyo), Shigeo Yoshida(Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University), Takatoshi Yanagisawa(海洋研究開発機構　地球深部ダイナミクス研究分野, 共同), Hidenori AIKI(Nagoya University)

This session on geophysical fluid dynamics is open to discussions and researches on fluid phenomena in whatever fields of earth and planetary sciences, e.g., motions in the earth and planetary interior, oceans, atmospheres, volcanoes, and the ionosphere, conducted with whatever methods. Talks intending to stimulate exchange of ideas among multiple fields of researches or those identifying concepts that are commonly applicable to wide range of geophysical fluids are especially welcome.

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[MIS15-P01] On penetration of compositional convection into a thermally stable stratified layer

*Shin-ichi Takehiro¹, Youhei SASAKI² (1.Research Institute for Mathematical Sciences, Kyoto University, 2.Department of Mathematics, Kyoto University)

[MIS15-P02] Theoretical consideration of the excitation of atmospheric Lamb waves by tsunamis

*Kensuke Nakajima¹ (1.Department of Earth and Planetary Sciences,Flculty of Sciences,Kyushu University)

[MIS15-P03] The life-cycle analysis of wave energy in the global atmosphere and ocean for understanding the mechanism of tropical climate variations

*Hidenori AIKI^1,2 (1.Institute for Space-Earth Environmental Research, Nagoya Univ., 2.Application Laboratory, JAMSTEC)

[MIS15-P04] Axisymmetric flow in a cylindrical tank with a rotating bottom: comparison between fast and slow cases

*Keita Iga¹ (1.Atmosphere and Ocean Research Institute, The University of Tokyo)

Presenter supplemental information

[MIS15-P05] Is there mantle convection? A paradigm that can not be demonstrated.
In Multi Impact Hypothesis, it is possible to unifyly describe multiple current situations only once,
It can be verified all results using abduction

*Akira Taneko¹ (1.SEED SCIENCE Lab.)

Session information

[M-IS15] Geophysical fluid dynamics-Transfield approach to geoscience

[MIS15-P01] On penetration of compositional convection into a thermally stable stratified layer

[MIS15-P02] Theoretical consideration of the excitation of atmospheric Lamb waves by tsunamis

[MIS15-P03] The life-cycle analysis of wave energy in the global atmosphere and ocean for understanding the mechanism of tropical climate variations

[MIS15-P04] Axisymmetric flow in a cylindrical tank with a rotating bottom: comparison between fast and slow cases

[MIS15-P05] Is there mantle convection? A paradigm that can not be demonstrated.
In Multi Impact Hypothesis, it is possible to unifyly describe multiple current situations only once,
It can be verified all results using abduction

Authentication

Session information

[M-IS15] Geophysical fluid dynamics-Transfield approach to geoscience

[MIS15-P01] On penetration of compositional convection into a thermally stable stratified layer

[MIS15-P02] Theoretical consideration of the excitation of atmospheric Lamb waves by tsunamis

[MIS15-P03] The life-cycle analysis of wave energy in the global atmosphere and ocean for understanding the mechanism of tropical climate variations

[MIS15-P04] Axisymmetric flow in a cylindrical tank with a rotating bottom: comparison between fast and slow cases

[MIS15-P05] Is there mantle convection? A paradigm that can not be demonstrated.In Multi Impact Hypothesis, it is possible to unifyly describe multiple current situations only once,It can be verified all results using abduction

Authentication

[MIS15-P05] Is there mantle convection? A paradigm that can not be demonstrated.
In Multi Impact Hypothesis, it is possible to unifyly describe multiple current situations only once,
It can be verified all results using abduction