Euphotic is referring to the sea water layer that receives sunlight for photosynthesis. The euphotic zone biomass percentage reaching the deep ocean floor is only one percent.
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About 50% of the incoming solar radiation reaches the surface of the planet. The rest is reflected or absorbed by the atmosphere & clouds, and a small portion is reflected by the oceans and land.
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About 11% of the total solar radiation that reaches the Moon is reflected back into space. This reflectivity is known as the Moon's albedo, which is relatively low compared to Earth. The majority of the solar radiation is absorbed by the lunar surface, contributing to the Moon's temperature variations.
Approximately 1-2% of the visible light that reaches Earth's producers is converted to chemical energy through photosynthesis. This energy is then used by the producers to fuel their growth and metabolic processes.
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Roughly 70% of the solar energy that reaches the outer atmosphere is absorbed by the Earth's surface. The remaining percentage is reflected back into space by clouds, aerosols, and the Earth's surface.
Approximately 20% of the Sun's energy that reaches the Earth is absorbed by the ozone layer and atmospheric gases. Ozone specifically absorbs a significant portion of ultraviolet (UV) radiation, protecting the surface from harmful effects. The remaining energy is either reflected back into space or absorbed by the Earth's surface.
About 1% of the liquid that reaches the kidneys is filtered and eventually becomes urine. The rest is reabsorbed back into the bloodstream.
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Approximately 1-2% of the solar energy that reaches the Earth's surface is absorbed by corn plants during photosynthesis. This energy is used to convert carbon dioxide and water into glucose and oxygen, enabling growth and development. The efficiency of this process can vary based on factors such as light intensity, temperature, and water availability. Overall, while a small fraction of solar energy is captured, it plays a crucial role in the plant's ability to produce biomass.
The marine life zones that are warm, well-lit, and rich in biodiversity are primarily the neritic zone and the euphotic zone. The neritic zone extends from the shoreline to the edge of the continental shelf, where sunlight penetrates, promoting photosynthesis and supporting a variety of marine organisms. The euphotic zone, which is the upper layer of the ocean, is where sunlight reaches and is home to numerous plants and animals, including phytoplankton, zooplankton, and various fish species. Both zones are critical for marine ecosystems and fisheries.