Answer:
Surface circulation carries the warm upper waters poleward from the tropics. Heat is disbursed along the way from the waters to the atmosphere. At the poles, the water is further cooled during winter, and sinks to the deep ocean. This is especially true in the North Atlantic and along Antarctica.
Answer:
Stratosphere
Explanation:
Stratosphere. The Stratosphere extends around 31 miles (50 km) down to anywhere from 4 to 12 miles (6 to 20 km) above the Earth's surface. This layer holds 19 percent of the atmosphere's gases but very little water vapor. In this region the temperature increases with height
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Answer:
This depends.
Explanation:
For the puritans and the pilgrims, it was to escape religious peresuction and to build a utopia. For the Dutch and other non-English countries, it was generally to engage in trade to make money, rather than settle down and build a society. For the colonists in virigina who were not puritans, they wanted to make money and also start a new life, and they were generally young men who were risk takers.
Answer:
I believe the best answer is B
Explanation:
Answer:
1. There is less variation in temperature of Aquatic habitats
2. The movement of water up trees results from capillary action.
3. Provides insulation to aquatic habitats
4. Evaporative cooling
Explanation:
1. The specific heat of water is high and is characterized as measure of heat required to result in the rise in temperature of 1 g of a substance by
.
Due to this, water can limit changes in temperature thus there isn't much variation in temperature.
2. Capillary action is the motion of water inside the spaces of a permeable material because of forces of cohesion, adhesion and surface tension.
Thus Cohesion forces results in the motion of water up trees.
3. Water has one most significant property where solid structure is less dense than fluid or liquid form that protects aquatic environments. As water in its solid form is less dense, in this manner ice coasts on the lake's surface that protects the water beneath from solidifying and valuable to aquatic life forms.
4. Heat of vaporization of water is high, which is characterized as the measure of energy expected to transform 1 gram of a liquid substance to a gas at steady temperature.
Along these lines when water particles evaporates, the surface they dissipate from gets cooler, referred to as evaporative cooling.