The relationship between depth and sunlight is positive. The more sunlight there is, the deeper you can see into the ocean.
pressure of liquid on bottom=density*gravitational force*depth :)
subbduction zones
They both have to do with whether or not people get sunlight or if they don't.
An example of a relationship between abiotic and biotic components in a forest ecosystem is how sunlight (abiotic) affects the growth of plants (biotic). Sunlight is essential for photosynthesis, a process where plants convert sunlight into energy, enabling them to grow and thrive within the ecosystem. This interaction demonstrates the interdependence between the non-living and living components of the forest ecosystem.
The clearest waters are in the South Pacific Gyre. At this place, the sunlight can still be measured at 200-250m depth at maximum. Abyssal plains are at 3000-4000 m depth... so no the sunlight doesn't reach the abyssal plains, it is very far from that!
A relationship that has "depth"?
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The relationship between water depth and pressure is linear. As water depth increases, the pressure exerted by the water also increases. This relationship is described by the hydrostatic pressure formula, which states that pressure is directly proportional to the depth of the fluid and the density of the fluid.
Rainbows are formed by sunlight.
The relationship between underground temperature and depth is that the temperature increases as you go deeper underground. This is because the Earth's core is hot, and heat is transferred from the core to the surface.
pressure of liquid on bottom=density*gravitational force*depth :)
As the depth increases, the density increases also.
subbduction zones
the deeper you go, generally the colder it gets
Please see attached links.
No, the relationship between temperature and depth is primarily influenced by factors such as geothermal heat flux and thermal conductivity of the material, while pressure at depth is mainly dependent on the weight of overlying material. Temperature generally increases with depth due to geothermal heating, while pressure increases with depth due to the weight of the material above.
Sunlight sufficient to power photosynthesis in marine plants penetrates to a depth of approximately (~660 feet). Sunlight decreases from this depth to approximately 900 meters (~3000 feet) where sunlight no longer penetrates. This sunlight-less region is known as the aphotic zone.