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The second innermost layer of the sun is the radiative zone. This layer is where energy generated in the sun's core is conveyed through radiation as the photons bounce between atoms until they reach the convective zone.
The layer surrounding the core of the sun is the radiative zone. This zone is responsible for transferring energy produced in the core to the outer layers of the sun through the process of radiation.
The Sun won't reach the Earth any time soon.The sunlight takes 8 minutes to reach the Earth.The Sun won't reach the Earth any time soon.The sunlight takes 8 minutes to reach the Earth.The Sun won't reach the Earth any time soon.The sunlight takes 8 minutes to reach the Earth.The Sun won't reach the Earth any time soon.The sunlight takes 8 minutes to reach the Earth.
The Sun's radiative zone is the region in its interior where energy produced by nuclear fusion in the core is gradually transported outwards through radiation. It is characterized by tightly packed gas and intense heat, with energy being emitted in the form of photons that bounce and travel slowly through the dense material of the zone. This process can take thousands to millions of years for a photon produced in the core to reach the outer layers of the Sun.
The radioactive zone in the Sun is the region where nuclear fusion occurs, specifically the conversion of hydrogen into helium. This process releases energy in the form of light and heat, which ultimately powers the Sun and allows it to shine.
The second innermost layer of the sun is the radiative zone. This layer is where energy generated in the sun's core is conveyed through radiation as the photons bounce between atoms until they reach the convective zone.
At the top of the ocean, or Sunlit, It is warmer because the top of the ocean the sun is closer then it is to the twilight,dark,abyss, and trenches zone. At the bottom of the ocean, or Trenches, It is colder because the sun can not reach that low in the ocean better then it can the Sunlit zone.
The sun can't reach the thermocline layer to heat that depth of water
Sunlight can reach through all the zones of the ocean, including the epipelagic (sunlight zone), mesopelagic, bathypelagic, abyssopelagic, and hadalpelagic zones. The intensity of sunlight decreases with depth, so the amount of light available for photosynthesis decreases below the epipelagic zone.
the regions are, in order from surface to center: the surface, which is 10,000 degrees F. then there is the convection zone, then the radiation zone. Finally, we reach the core which is 27,000,000 degrees F.
No, the aphotic zone in a marine biome is the deep, dark layer where sunlight cannot penetrate. This zone lies below the photic zone, where sunlight can reach and support photosynthesis.
Aphotic zone.
The convection zone of the sun surrounds the radiative zone, which is the region where energy generated by nuclear fusion in the core is transported outwards through the slow process of radiative diffusion. In the convection zone, energy is transported by the movement of hot plasma, creating convection currents.
The polar zones, located near the North and South Poles, receive the least amount of sunlight due to their extreme latitudes and the tilt of the Earth's axis. This results in long periods of darkness during winter months.
Your question is unintelligible. There is no "radioactive zone" defined as part of the Sun.
in the sun light zone
The radiative zone in the sun can reach temperatures of several million degrees Celsius. Energy from nuclear fusion reactions in the core is transported through this region via photons before reaching the convective zone.