The average temperature on the surface of Europa (as in one of Saturn's moons) is around -260 degrees Fahrenheit.
The thermocline is the layer of seawater that changes temperature rapidly with depth. In this layer, the temperature decreases quickly as you move from the warmer surface waters to the colder deeper waters.
Temperature inversion
The outermost layer of the sun's surface is called the photosphere. This is the visible surface of the sun that emits light and heat. It has an average temperature of about 5,500 degrees Celsius.
The atmosphere is the thin layer of air that surrounds the Earth and helps regulate its temperature by trapping heat from the sun. This layer acts like a blanket to protect the Earth's surface from extreme temperature fluctuations.
In the thermocline region, the temperature of ocean water decreases rapidly with depth due to the barrier between the warm surface layer and the cold deep layer. This abrupt change in temperature creates a distinct layer of transition between the warmer surface water and the colder deep water.
Temperature inversion
The layer of water where temperature drops sharply is called the thermocline. This is a zone of rapid temperature change in the ocean that separates the warm surface water from the colder deep water.
Layers in Earth's atmosphere are primarily separated based on temperature variations caused by differences in altitude and composition. The troposphere is the layer closest to the Earth's surface, where temperature generally decreases with altitude. Above that is the stratosphere, where temperature begins to increase due to the presence of the ozone layer.
the layer above the earth is the troposphere
The mesosphere is the layer of the atmosphere that protects the Earth's surface from most meteoroids. Meteoroids burn up in this layer due to the high temperature caused by the friction with the air molecules.
As distance from the Earth's surface increases, the temperature of the stratosphere generally increases. This warming occurs because the stratosphere contains the ozone layer, which absorbs ultraviolet (UV) radiation from the sun, leading to an increase in temperature with altitude. In contrast, the troposphere, which is the layer below the stratosphere, experiences a decrease in temperature with altitude.
it will increase (get hotter).