During convection, heat transfer happens through the movement of fluid (liquid or gas) due to temperature differences. As the fluid near a heat source gets warmed up, it becomes less dense and rises, while cooler fluid sinks to replace it. This creates a continuous circulation pattern that helps to equalize temperatures within the fluid.
Convection occurs in fluids such as liquids and gases, unlike conduction, which occurs in solids. During convection, the heated particles in the fluid become less dense and rise, while cooler particles sink, creating a circular motion that transfers heat.
convection
nondijunction
Heat transfer in gases is called convection. It is the process by which heat is transferred through the movement of fluid (gas or liquid) particles. Convection occurs when hot air rises and cold air sinks, creating circulation and transferring heat in the process.
light independent
Crossing over is a process that occurs during meiosis.
convection
convection occurs in fluids such as water and air
convection occurs in fluids such as water and air
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It refers to a region in which convection occurs.
The thermal energy transfer that occurs by the motion of fluid in liquid or gas is known as convection. This process involves the transfer of heat by the movement of a fluid due to density differences created by temperature variations. Convection is a key mechanism for distributing heat in fluids.
Convection occurs in fluids such as liquids and gases, unlike conduction, which occurs in solids. During convection, the heated particles in the fluid become less dense and rise, while cooler particles sink, creating a circular motion that transfers heat.
Convection is the transfer of heat through the movement of fluids (liquids or gases). This occurs as hot fluids rise and cold fluids sink, creating a continuous flow of heat transfer. Convection is an important process in the Earth's atmosphere, oceans, and interior.
When convection occurs in the air, winds are formed.
The heat transfer method that occurs in the Earth's mantle is called convection. In this process, heat is transferred through the movement of molten rock material within the mantle, creating convection currents that drive plate tectonics and other geological phenomena.