INCREASE in temperature.This tremendous ability to store and release heat over long periods of time gives the ocean a central role in stabilizing Earth’s climate system.The main source of ocean heat is sunlight.Additionally, clouds, water vapor, and greenhouse gases emit heat that they have absorbed, and some of that heat energy enters the ocean.Waves, tides, and currents constantly mix the ocean, moving heat from warmer to cooler latitudes and to deeper levels.Heat absorbed by the ocean is moved from one place to another, but it doesn’t disappear.The heat energy eventually re-enters the rest of the Earth system by melting ice shelves, evaporating water, or directly reheating the atmosphere.Thus, heat energy in the ocean can warm the planet for decades after it was absorbed.If the ocean ABSORBS more heat than it RELEASES, its heat content increases.Knowing how much heat energy the ocean absorbs and releases is essential for understanding and modeling global climate.Therefore, A and B only true here.Kinetic energy:Moving objects are capable of causing a change, or, put differently, of doing work.Energy means the ability to do work, so all moving things have energy by virtue of their motion. This type of energy is called kinetic energy. A speeding bullet, a walking person, and electromagnetic RADIATION like a light all have kinetic energy.Another example of kinetic energy is the energy associated with the constant, random bouncing of atoms or molecules.This is also called thermal energy – the greater the thermal energy, the greater the kinetic energy of atomic motion, and vice versa.The AVERAGE thermal energy of a group of molecules is what we call temperature, and when thermal energy is being transferred between two objects, it’s known as heat.