Answer:
This salinity versus depth profile is typical of the South Atlantic ocean. ... In this profile, salinity at the surface is high (evaporation at this latitude is high) and then salinity decreases until a depth of about 1,000 meters. Salinity then increases again slightly with increasing depth. The ocean around Antarctica has a low salinity of just below 34ppt, and around the Arctic it is down to 30ppt in places.
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Answer:
This salinity versus depth profile is typical of the South Atlantic ocean. ... In this profile, salinity at the surface is high (evaporation at this latitude is high) and then salinity decreases until a depth of about 1,000 meters. Salinity then increases again slightly with increasing depth. The ocean around Antarctica has a low salinity of just below 34ppt, and around the Arctic it is down to 30ppt in places.
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Which of the following must be balanced for a portion of the lithosphere to reach isostatic equilibrium?
A. The buoyant force from the asthenosphere and gravity
B. The densities of the lithosphere and the asthenosphere
C. The isostatic uplift and the crustal rebound
D. The compressive forces of two converging plates
Answer: B
Explanation: The isostatic equilibrium occurs when enormous tectonic plates composed of crustal and upper mantle material are able to float on top of the astenosphere, which in turn is composed of denser rock material. In order for such a thing to be achieved the lithosphere and the astenosphere have to have balanced densities between each other. In other words, the density of the material on top, has to be in balance with the density of the material below it, thus to not have any uplift or sinking occurring between them.
Answer:
The buoyant force from the asthenosphere and gravity
Explanation:
I've seen all these answers on this websites and their all wrong
10. Which tool should be used to measure the amount of water vapor in the air?
A Hygrometer
B) Anemometer
Barometer
D
Thermometer
Answer:
hygrometer
Explanation:
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Answer: The correct answer is Hygrometer
What is the difference between chemical and physical weathering?
Answer: Physical Weathering physically breaks the rock, while Chemical Weathering chemically changes the rock causing it to break.
Explanation: Physical Weathering happens naturally causing the rock to break. An example is roots growing into the concrete causing it to crack. Chemical Weathering on the other hand chemically changes the rock by a chemical reaction. An example is acid rain. Gas or other pollution mixing in with water causing acid rain.
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1. Why do we exist
2. Explain your answer
Pleases explain I need to know the reason 4 existence