wind.
Advection fog results when moist air moved across a cold surface. When moving across a cold surface, the air is cooled to its dew point.
Different temperatures make currents, the wind could cool down or heat up the surface water.
A sea breeze occurs when cool air moves from the beach toward the ocean at night.
No, hurricanes do not cool the ocean. Instead, they can actually warm the ocean due to the mixing of warm surface waters with cooler waters below.
Advection fog forms when moist air moves horizontally over a colder surface, causing the air to cool and reach its dew point, leading to the condensation of water vapor into fog.
This process is called advection cooling. As the warm, moist air moves over the cold surface, it loses heat to the cooler surface, causing the air to cool and potentially leading to the formation of fog or low clouds.
Warm air moves from a beach toward the ocean by convection.
sea breaze
Maritime polar air forms over the North Pacific Ocean due to the combination of cool ocean temperatures and moist air. As air moves over the relatively warmer ocean surface, it picks up moisture, leading to the development of clouds and precipitation. This air mass is characterized by its cool and damp conditions, which can influence weather patterns as it moves inland, often bringing cooler temperatures and increased humidity to coastal regions.
This process is known as onshore flow. As the cool ocean air moves over the warmer land, it cools the land surface, leading to lower temperatures in coastal areas. Onshore flow can bring fog, mist, and lower humidity levels to the affected regions.
Because you are getting hot and the blood in your body moves closer to the surface to cool down.
Ocean surface temperatures generally decrease from the Northern Pacific Ocean southward to Antarctica. In the Northern Pacific, warmer waters are influenced by the North Pacific Current and the Kuroshio Current, which bring warmer temperatures. As one moves southward, particularly past the equator, the waters cool significantly due to the influence of the cold Humboldt Current along the western coast of South America and the Southern Ocean's circumpolar currents. By the time you reach Antarctica, the surface temperatures are among the coldest in the world, often near freezing.