The product's price decreases.
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The Norwegian Current creates marine climate type.
Explanation:
There are several ocean currents in the Atlantic Ocean. Some of them are warm ocean currents (surface currents), while some are cold (deep currents). The warm ones develop around the Equator and move toward the higher latitudes, while the cold ones develop in the higher latitudes and move toward the Equator.
The Norwegian Current is part of the warm ocean currents in the Atlantic. This ocean current is an extension of the North Atlantic Drift, which is an extension of the Gulf Stream, which is an extension of the Florida Current, which is an extension of the Antilles Current, which is an extension of the North Atlantic Current, thus creating a curved, interconnected extensions of one another. This ocean current brings in warm and humid weather conditions. It makes the western coast of the Scandinavian Peninsula much warmer that it should be according to its latitude, and brings in solid amounts of precipitation.
Some other ocean currents in the Atlantic Ocean are:
- Counter Equatorial Current
- Labrador Current
- East Greenland Current
Learn more about deep ocean currents brainly.com/question/12168401
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Answer:
the earth rotates about it's axis,just as a top spins around it's spindle.the earth rotates from the north pole to the south pole.it takes 24hours for the earth to make one complete rotation.
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The Ural Mountains and the Caucasus Mountains.
Answer: Convective
Explanation:
Convective Lifting is arguably the most common form of lifting and involves the heating of the Earth's surface such that surface water gets evapotranspirated from the ground and plants.
As the clouds rise, they encounter cooler temperatures and thus cool down and condense into clouds. Higher temperatures mean higher convection.
The Amazon lies on the Equator which receives the most direct sunlight so the surface gets heated a lot. Water therefore collects faster and condenses more over the Amazon which leads to more precipitation over the Rainforest.
