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
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Answer: They are directly caused by the gravitational pull of the Sun.
Explanation:
Water waves are caused by a whole number of factors, they include,
1.) Local winds
2.) Distant wind
3.) Air pressure
4.) Seismic sea wave
The gravitational pull of the sun and moon on the earth also causes waves. Although the sun's gravity also contributes to the waves, but its effects are smaller and serve mostly to vary the heights of high and low tide.
Calcrete or Caliche is a type of sedimentary rock often found in arid and semiarid regions. It is composed of calcium carbonate with bits of gravel, clay and silt. It is found in Australia, Kalahari Desert, Sonoran and Mojave desert. Note that caliche does not form through dissolution and reprecipitation of rainwater. Rather, it forms when water from the ground rise above through capillary action, bringing up minerals from the ground into the surface.
You can try Texas and Pennsylvania
