Titlebook: IUTAM Symposium on Advances in Mathematical Modelling of Atmosphere and Ocean Dynamics; Proceedings of the I P. F. Hodnett Conference proce

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A Dynamical Stabilizer in the Climate System: A Mechanism Suggested by a Simple Model and Supported hanisms such as the ice-albedo feedback and the lower tropospheric water vapour/infrared radiative feedback on sea surface temperature perturbations are known to exist which could, in principle, drive the climate system far from its observed mean state even in the absence of any external forcings. E

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Asymptotic Models and Application to Vortex Dynamicstic expansion of rotating shallow water (RSW) leads to the frontal geostrophic (FG) model which is numerically implemented. Both in FG and in RSW, anticyclones travel westward faster than cyclones. In FG, vortices of both signs show initially a secondary meridional northward drift which we detail. H

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An Air-Ocean Coupled Nowcast/Forecast System for the East Asian Marginal Seasludes the broad shallows of the Sunda Shelf in the south/southwest of SCSi the continental shelf of the Asian landmass in the north, extending from the Gulf of Tonkin to the YES; a deep, elliptical shaped SCS and JES basins, and numerous reef islands and underwater plateaus scattered throughout (Fig