it gets cold and freezes
The salinity of the water increases. Nova net
When ocean water reaches the poles, it cools down and becomes denser, causing it to sink to deeper parts of the ocean. This cold, dense water then starts to circulate and move towards lower latitudes, influencing global ocean currents and climate patterns. Additionally, the melting of ice at the poles adds freshwater to the ocean, impacting salinity levels and ocean circulation dynamics.
Mamadas!!!
The water melts
According to the conveyor belt model of ocean circulation, when water reaches the poles, it cools and becomes denser, leading it to sink. This cold, dense water then contributes to deep ocean currents, playing a crucial role in global thermohaline circulation. As it sinks, it helps drive the movement of warmer surface waters toward the poles, maintaining the balance of oceanic circulation.
it becomes water vapour in the atmosphere.
It is a solid
The majority of the water freezes because water is the only molecule that doesnt sink...so the water becomes ice
Water in the atmosphere stays there as water vapor, or it condenses and falls as rain, snow, hail, etc.
Water in the atmosphere stays there as water vapor, or it condenses and falls as rain, snow, hail, etc.
Water reaches its boiling point of 212 degrees Fahrenheit at standard atmospheric pressure. At this temperature water transitions from liquid to vapor, forming steam.
The energy that reaches the equator is more intense than the energy that strikes poles