Wiki User
∙ 14y agoIt is this way since the equator is warmer than the subtropical regions. I think warmth burns the salt from the water.
Wiki User
∙ 14y agoSalinity in subtropical regions tends to be higher than at the equator because of the higher rates of evaporation in subtropical regions. As water evaporates, salt is left behind, increasing the overall salinity of the water. In contrast, the equator receives more rainfall, which dilutes the salt content in the water.
The most significant dilution of seawater occurs at the mouths of rivers and streams, where freshwater flowing into the ocean decreases the salinity of the surrounding seawater. Additionally, melting ice caps and glaciers are other sources of dilution in polar regions.
Subtropical water refers to the oceanic water found in regions adjacent to the tropics, characterized by slightly cooler temperatures and different marine life than found in tropical waters. It typically has a temperature range between 18-24 degrees Celsius and occurs at latitudes further away from the equator.
Tropical
Density of seawater is largely a function of two factors: depth, that is, the deeper water is more dense than water at shallower levels; and temperature - water at higher temperatures is less dense than cooler water. Salinity is also a factor, but that's a localized phenomena simply because all the worlds oceans are in fact one large ocean and maintains an average overall salinity.
subtropical high-pressure belts towards the equator and the polar regions. This creates a westerly flow due to the Earth's rotation (Coriolis effect), deflecting the air to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
Salinity in the ocean is highest in regions where evaporation is high and precipitation is low. Density in seawater is determined by both temperature and salinity.
The most significant dilution of seawater occurs at the mouths of rivers and streams, where freshwater flowing into the ocean decreases the salinity of the surrounding seawater. Additionally, melting ice caps and glaciers are other sources of dilution in polar regions.
subtropical regions
The density of seawater increases as salinity increases. This is because salt makes seawater denser by adding mass without significantly increasing volume.
Yes. in fact, they can only survive in subtropical regions.
Surface salinity in polar regions varies seasonally due to the formation and melting of sea ice.
Subtropical water refers to the oceanic water found in regions adjacent to the tropics, characterized by slightly cooler temperatures and different marine life than found in tropical waters. It typically has a temperature range between 18-24 degrees Celsius and occurs at latitudes further away from the equator.
Tropical
Density of seawater is largely a function of two factors: depth, that is, the deeper water is more dense than water at shallower levels; and temperature - water at higher temperatures is less dense than cooler water. Salinity is also a factor, but that's a localized phenomena simply because all the worlds oceans are in fact one large ocean and maintains an average overall salinity.
The salinity of water in polar regions varies seasonally because of the melting of sea ice during warmer months.
In the era of sailing ships, regions of constant winds were much appreciated. They made trade around the world possible.
Trade winds got their name from their historical importance in enabling trade between regions. They blow consistently from the subtropical high pressure zones towards the equator, making them favorable for sailing and early trade routes. These winds helped facilitate trade and exploration in the past, hence the name "trade winds".