I am not to sure but I think that it sinks...
colder than at the equator due to the angle of sunlight hitting the poles, causing denser air to sink and accumulate. This results in high atmospheric pressure and lower temperatures.
yeah cold water is denser than room temperature (warm) water.
Sunspots are darker because they are cooler than the surrounding area.
For a tectonic plate to subduct, it typically requires a temperature and density differential where the subducting plate is colder and denser than the surrounding mantle. Generally, this occurs at convergent plate boundaries where an oceanic plate, which is usually denser and cooler, collides with a less dense continental plate. As the colder, denser oceanic plate descends into the mantle, it creates conditions favorable for subduction, often influenced by the temperature gradient associated with increasing depth.
the sun's rays strike the water at a angle at the poles APEX
colder than at the equator due to the angle of sunlight hitting the poles, causing denser air to sink and accumulate. This results in high atmospheric pressure and lower temperatures.
They are colder and darker than the other areas
yeah cold water is denser than room temperature (warm) water.
Yes, because it is closer to the poles
Denser water sinks.
Because cold air is denser than warm air.
Sunspots are darker because they are cooler than the surrounding area.
The poles are colder than other regions because sunlight hits them at a more oblique angle, spreading out the energy over a larger area and making it less intense. This results in lower temperatures at the poles compared to regions closer to the equator.
Temperature decreases with altitude
It depends. If the river is in the mountains or near the Poles than it's probably colder but if the ocean is like the arctic ocean or something like that then that's probably colder
For a tectonic plate to subduct, it typically requires a temperature and density differential where the subducting plate is colder and denser than the surrounding mantle. Generally, this occurs at convergent plate boundaries where an oceanic plate, which is usually denser and cooler, collides with a less dense continental plate. As the colder, denser oceanic plate descends into the mantle, it creates conditions favorable for subduction, often influenced by the temperature gradient associated with increasing depth.
Colder air is denser than warmer air