Explanation:
Plants absorb water from the soil through their roots.
Some of the water is used for photosynthesis and most of this water evaporates into the air through transpiration.
Liquid water is often absorbed by plants. Their roots penetrates deep into the earth in search of water. Different root morphology are known in plants to maximize the absorption of water.
Plants use just a little of the water for its metabolic life processes. An example is photosynthesis.
The remaining is returned back into the atmosphere by evaporation through transpiration.
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Biogeochemical cycle brainly.com/question/4217448
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Answer:
<u>Relative dating </u> determines the order of layers of rock based on their relationship to one another .
Explanation:
Relative dating -
The method to determine the relative order of the past events , without finding the absolute ages .
The actual numerical dates of the rocks are not provided by this method .
Even the order of the series of the past is determined by this method , not when the event occurred .
The preferred method in paleontology is done by relative dating by biostratigraphy , and is very accurate .
The entire United States and the rest of the world serve as the hinterland for all of the following cities except Tucson.
Answer:
- Interaction with land
- Conctact with colder water
- Strong vertical wind shear
Explanation:
- The interaction with land: a hurricane needs evaporation from the ocean surface to survive, when it touches land the hurricane is separated from its energy source since the air masses over the ocean are drier, less moisture is carried into the storm and air is cooled and then sinks disrupting hurricane's circulation.
- Getting in contact with colder water: when a hurricane moves northward out of the tropical ocean into mid-latitudes, it begins to get in contact with colder water, this makes it lose the warm water source, less moisture is evaporated into the atmosphere to supply clouds and this weakens the storm.
- Strong vertical wind shear: a change in wind direction or speed with height can enhance the mixing of drier environmental air into the storm eyewall leading to a column of cool air that rapidly sinks into the grounds, this inhibits the intensification of the hurricane. This kind of wind shear can be generated by fast upper-tropospheric winds.
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