Only about 2-5 percent. Because the huge broad-leaf canopies absorb most of the light. As a result the vegetation on the floor of tropical rain forests tends to be vegetation adapted to low levels of light (bromeliads, dotter vines, fungi, lichens).
1% - gradpoint
The ground floor of the rainforest is called the forest floor. It is the lowest layer of the rainforest where little sunlight reaches, resulting in limited plant growth.
The tropical rainforest biome is so abundant and thick that almost no sunlight reaches the soil due to the dense canopy formed by tall trees, vines, and other vegetation. This results in a dark and humid understory where only shade-tolerant plants can grow.
Little sunlight reaches the ground in a tropical rainforest due to the dense canopy layer formed by the overlapping branches and leaves of tall trees. This canopy layer blocks much of the sunlight from penetrating through to the forest floor. Additionally, the high levels of humidity and moisture in a tropical rainforest can also scatter and absorb sunlight, further reducing the amount that reaches the ground. As a result, the lower levels of the rainforest receive minimal sunlight, leading to dimmer conditions compared to the upper canopy levels.
it depends on the place but they absorb around 25 to 75 percent
there are so much abiotic elements in the tropical rainforest i will list all of them 1soil 2temperature 3is sunlight i will not saw all of them because that is to much my name is amanda springfield
Well 0% percentage of it is because TP eats and with his cheese as for the cheese problem, you cant stop that he likes cheese
About half the amount of sunlight reaches the surface of Mars compared to Earth, due to its greater distance from the Sun. The thin atmosphere on Mars also scatters and absorbs some of the sunlight before it reaches the surface.
8 seconds
Lots!
plentiful
Sunlight reaches the surface of the Earth at all points where there is daylight. The distribution of sunlight on Earth varies throughout the day due to the rotation of the Earth on its axis.