surface
the air in the atmosphere and the waters in our oceans circulate in known patterns in an effort to redistribute the energy. In the atmosphere, we end up with the prevailing wind bands in both hemispheres. In the oceans, we end up with both surface and deep water currents. It is the surface currents that have a marked effect on climate.
Vertically
Coastal Surface waters in all major oceans.
Deep ocean currents and surface currents do meet, but mixing is limited. The waters stratify based on temperatures and salinity. The higher the salinity, the heavier the water.
Surface currents involve warm water that flows in different directions and different speeds that stay close to the top of the oceans. They originate in tropical waters and flow in circular motions from all the major gyres of the world ocean.
The differing densities of water create a consistent movement between the various thermal layers. As water is cooled, it actually expands, so it rises, and as it is warmed it sinks.
ocean fronts
Yes
Surface ocean currents are mainly wind-driven and occur in all of the world's oceans. Examples of large surface currents that move across vast expanses of ocean are the Gulf Stream, the North Atlantic Current, the California Current, the Atlantic South Equatorial Current, and the Westwind Drift. Associated with surface currents are counter-surface and underlying currents. Surface ocean currents are deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere due to the Coriolis effect. The Coriolis effect holds that because the Earth is spinning, surface waters move in a clockwise direction in the Northern Hemisphere and in a counterclockwise direction in the Southern Hemisphere. The currents eventually come into contact with the continents which deflect them, creating giant oceanic current circles known as gyres. Vertical and ocean-bottom currents are mainly driven by density differences caused by changes in temperature and salinity. Originating in polar regions, cold, salty waters sink to the ocean bottom and move toward the opposite poles where they again surface. Vertical upwelling currents can also be caused by winds "blowing off" a coastline. The displaced waters are then replaced by underlying bottom waters. Currents are important to marine life as they help to move food and nutrients, making them available for photosynthesis, metabolic requirements and/or consumption.
Nutrients are in deeper (colder) waters while light is in surface waters.
Sunlight warms the waters on the ocean surface. Some heat energy is transferred to cooler waters through convection.
The Portuguese man-of-war prefers the warm waters of the Pacific, Indian, and Atlantic oceans, but are found in all oceans. They live on the ocean surface. The Portuguese man-of-war cannot propel itself, but is moved along by currents, tides, and waves.