<span>There has been a great deal of discussion about the extent to which climate change could influence thermohaline circulation and its turnover processes in the Atlantic. After all, convection at high latitudes could be weakened by anthropogenic (caused by humans) warming of the atmosphere and the accompanying decrease in surface-water density. Additionally the density will decrease as a result of lower salinity in the North Atlantic. Climate change will probably cause an increase in freshwater input through a number of pathways, which will affect convection and thermohaline circulation. One way would be by an increase in precipitation over both the continents and the ocean. Another would be the increase of freshwater run-off from the melting glaciers to the sea. Furthermore, because less ice forms when it is warmer, the salt concentration in the surface water would not be increased as much by this proces</span>
D. the results of "white only" zoning laws
Answer:
Regions between the Tropic of Cancer and Arctic Circle
Explanation:
If you like my answer than please mark me brainliest thanks
Answer:
Melting is indicated by red arrows, cooling is indicated by blue arrows, and weathering and erosion is indicated by green arrows.
Explanation:
Hope this helps!
Please mark me as Brainlinieast.
Answer: 25.12cm³
Explanation:
First, we need to calculate the volume of the small cone shaped cups of water which will be:
= 1/3πr²h
where,
π = 3.14
r = 3cm
h = 8cm
Volume = 1/3πr²h
= 1/3 × 3.14 × 3² × 8
= 1/3 × 3.14 × 9 × 8
= 75.36cm³
Since Abigail sloshes 2/3 of the water out of a cup before she gets to drink any, this means that there'll be (1 - 2/3) = 1/3 of the water remaining in Abigail‘s cup. Therefore, the volume of the water remaining in Abigail‘s cup will be:
= 1/3 × 75.36
= 25.12cm³
