Sekine conducted shock-wave experiments by using a propellant gun that accelerated a stainless-steel disc into a composite sample simulating the components of meteorites, the ocean, and the atmosphere.
A section of the zonal velocity component in the central part of the ocean is shown in Fig. 5.
Seasonal ice velocity is influenced by several key components of the ice sheet-ocean-climate system, including the subglacial environment, surface melt and runoff, and ice-ocean interaction at the ice front (terminus) [ Joughin et al., 2012; Carr et al., 2013].
Model simulations have linked AMOC variability to climate impacts on decadal timescales [ Knight, 2005; Latif et al., 2004], and observations suggest that the AMOC is a fundamental component of the seasonal ocean-atmosphere heat budget [ Rhines et al., 2008].
Its ocean component calculates the oceanic circulation using an ocean with uniform depth and albedo and no circulation.
Because of the continuity of the Z component across the ocean column, Z at the sea floor is not shown Fig. 11 Modeled X component at a period of 24 h at the sea level.
Because of the continuity of the Z component across the ocean column, Z at the sea floor is not shown Fig. 16 Synthesized Z from a sum of eight tidal constituents (cf. Table 2) at VAL (upper panel) and T12-2 (lower panel) for the year 2011 Fig. 17 Power spectral density (PSD) plots at VAL (Ireland, ground) for the year 2011 and T12-2 (Philippine sea; sea floor) for the year 2007.
It's also major component of the atmosphere, the oceans, and every organic (i.e. carbon-based) life form on the planet.
