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In general, as latitude increases away from the equator towards the poles, temperatures tend to decrease. This is due to a variety of factors, including the angle of sunlight hitting Earth's surface, the length of daylight hours, and the amount of atmosphere sunlight must pass through.
The temperature of the body. As the temperature of the body increases, the wavelength of the radiation emitted decreases, shifting towards shorter wavelengths. This relationship is described by Wien's displacement law.
The temperature of gases in the convection zone increases as they rise towards the top. This is due to the process of convective heat transfer, where hotter gases move upwards and cooler gases move downwards, creating a cycle that leads to temperature increase towards the top of the convection zone.
As latitude increases, the temperature tends to decrease. This is because the amount of solar energy received decreases as you move away from the equator towards the poles. The angle at which sunlight hits the Earth's surface becomes more oblique at higher latitudes, resulting in less direct heating.
28 degrees on surface and gradually decreasing towards depth.
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Temperature and pressure increase due to the weight of the overlying rock layers. The composition of the materials also changes, with denser materials sinking towards the core and less dense materials rising towards the surface. The physical properties of the rocks, such as hardness and density, also change with depth.
False. The temperature increases from the surface of the Earth towards its center. This is due to the heat generated from the Earth's core and the radioactive decay of elements in the Earth's mantle and crust.
Air pressure decreases while temperature increases.
When temperature increases, the frequency of radiation also increases. This is because temperature is directly proportional to the average energy of particles, so they emit higher-energy radiation with higher frequencies. This shift towards higher frequencies is known as thermal radiation or thermal emission.
As you go deeper into the Earth, the temperature and pressure increase. Additionally, you may encounter different layers of the Earth's interior, such as the crust, mantle, outer core, and inner core. The density of materials also tends to increase as you move towards the Earth's center.
In general, as latitude increases away from the equator towards the poles, temperatures tend to decrease. This is due to a variety of factors, including the angle of sunlight hitting Earth's surface, the length of daylight hours, and the amount of atmosphere sunlight must pass through.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
Temperature can affect the wavelength of light by altering the kinetic energy of particles, which in turn can impact the frequency of light waves. Generally, as temperature increases, the average speed of particles also increases, resulting in a shift towards shorter wavelengths for higher temperatures. This phenomenon is known as thermal Doppler broadening.
The temperature of the body. As the temperature of the body increases, the wavelength of the radiation emitted decreases, shifting towards shorter wavelengths. This relationship is described by Wien's displacement law.
The temperature generally increases as you move from the Earth's surface towards the center. The outermost layer, the crust, has variable temperatures. The mantle beneath the crust is solid but can slowly flow, and its temperature increases with depth. The core, consisting of the outer liquid core and the inner solid core, is the hottest layer, with temperatures reaching over 5000 degrees Celsius at the inner core.