Convection currents
The temperature in the zone beneath the thermocline remains relatively stable as it experiences minimal mixing with the warmer water above and the cooler water below. This results in a sharp temperature gradient between the layers above and below the thermocline.
This movement is an example of convection. As the mantle is heated from below, warmer, less dense material rises toward the crust, while cooler, denser material sinks back down. This convection process drives plate tectonics and influences the movement of Earth's lithosphere.
Convective motion is typically observed in fluids, where warmer, less dense material rises and cooler, denser material sinks. This can occur in various arrangements, such as in a liquid heated from below or in a gas exposed to a temperature gradient. Additionally, convective motion may occur in Earth's mantle due to the heat flow from the core.
Two examples of microclimates are a street in a city that is warmer than the surrounding areas due to the heat-absorbing properties of concrete and a hillside that experiences cooler temperatures than the valley below due to elevation changes and the flow of cold air.
Cold air is denser than warm air, so it sinks below the warm air, displacing it upwards. This process is called convection, where the warmer air expands and rises as the colder air contracts and sinks.
The circular motion of heating in fluids is caused by convection currents. When a fluid is heated from below, it expands, becomes less dense, and rises. This rising fluid displaces cooler, denser fluid which then descends, creating a circular motion.
because the sun hits the equator more therefore, the equator is warmer
Heat. As the air expands (as it's heated), it rises and causes air to flow upward.
The hand placed below the tray of ice would feel cooler. This is because heat transfer occurs from a warmer object (your hand) to a cooler object (the ice), so the hand in contact with the ice will experience a greater cooling sensation.
For the most part, liquid water expands when heated, and so does pretty much every material. Water's volumetric expansion is a few hundred parts per million per degree Celsius. The interesting thing about water, though, is that if it's below 4°C it expands as it gets colder, i.e. it has a negative volumetric expansion coefficient.
The density of liquid water is fairly constant across the range of temperatures. Liquid water is most dense at 4°C. At temperatures below that, water will expand slightly. When water freezes to form ice, it expands. Water vapor (steam) expands when heated.
We call the flow of thermal energy from warmer matter to cooler matter heat transfer, and we study this in thermodynamics. A link can be found below to check facts and learn more.
Front of trans, just below the cooler lines.Front of trans, just below the cooler lines.
It is on the front of the transmission case, below the cooler hoses.It is on the front of the transmission case, below the cooler hoses.
During summer, the sun heats the surface of the pond more quickly than the deeper layers due to direct sunlight exposure. This results in the surface water feeling warmer. Conversely, the deeper layers of the pond remain cooler as they are not in direct contact with the sun's heat, creating a temperature difference between the surface and the bottom.
The basement is underground so the sun's heat does not reach it, but probably its just that above ground is warmer rather than below ground is cooler.
Almost always warmer at the surface.