Question

explain how ocean current influence temperature of a place with examples ​

Answer 1

Answer:

Ocean currents act as conveyer belts of warm and cold water, sending heat toward the polar regions and helping tropical areas cool off, thus influencing both weather and climate. ... One way that the world's ocean affects weather and climate is by playing an important role in keeping our planet warm.

Answer 2

Following are the affects of the ocean current on the temperature of the place.

Explanation:

• Ocean curriculum works as a hot and cold water carrier belt, send heat to polar areas and helps in cooling tropical areas, thus influence both weather and climate. Land area also absorbs some sunlight, and helps in maintaining the heat of the environment, which otherwise spreads in space after sunset.
• The cold ocean stream flows towards equatorial areas from polar. During this process, polar regions flows with the iceberg stream. This, in return, has become a threat to sea routes, where the continuous movement of the ships is.
• This speed is caused by sea streams that are not always stable. Water rotates in water and as soon as the waves of sea water come on the edge, the speed of water changes due to the size of the beach, which changes streams in sea water.
• Ocean currents are horizontal continuous flow from one place to another from a place of water. The hot air and cold air is met by meeting cold and hot streams. Hot air from cold air will become hot air, resulting in dense fog, resulting in cooling down from her dew point.
• Ocean currents is used to define any more or less permanent or continuous, guided speed of sea water flowing in one of the oceans of the Earth. These are arising from the powers working on water such as roaming, air, temperature and salinity and the gravity of the moon. Ocean currencies may flow up to thousands of kilometers and affect the direction and power of their depth, coastline and other sections.
• When the sea water is frozen, then the sea becomes ice, the salt remains behind, which is the surrounding seawater saline and dense. Dense-cool-salt water is immersed in the sea level. To change the drowning water, the superficial water flows, which is cold and saline in turn, which is sufficient to drown.