wat
yes
Deep ocean currents typically have greater salinity compared to surface currents. This is primarily due to factors such as evaporation in warmer regions and the formation of sea ice, which increases the concentration of salts in the water. Additionally, deep currents are often sourced from colder, saltier water masses that have sunk and are less affected by precipitation and runoff that can dilute surface salinity.
Well, honey, a surface current is like the diva strutting her stuff on the runway - it's the flashy, visible movement of water caused by things like wind and tides. On the other hand, a deep current is more like the mysterious loner lurking in the shadows - it's the slow, hidden flow of water deep below the surface, driven by differences in temperature and salinity. So, in a nutshell, surface currents are the show-offs, while deep currents are the silent movers and shakers of the ocean.
Deep ocean currents are in the depths of the oceans. Surface current are at the surface, not deep down. Deep ocean currents bring vitamins and nutrients to the shore, surface currents do not. Deep ocean currents are caused by salinity and temperature differences. Surface currents are cause by the force and impact of the wind.
Deep ocean currents are in the depths of the oceans. Surface current are at the surface, not deep down. Deep ocean currents bring vitamins and nutrients to the shore, surface currents do not. Deep ocean currents are caused by salinity and temperature differences. Surface currents are cause by the force and impact of the wind.
wat
negatvily
A deep current forms when water masses sink and flow horizontally along the ocean floor due to differences in temperature and salinity. This creates a slow-moving, deep-sea current that can transport large amounts of water and nutrients over long distances in the ocean.
a surface current
Salinity (how much salt) of the water and low temperatures
A thermohaline current is affected by differences in water temperature and salinity. These differences drive the circulation of deep ocean waters around the globe, transporting heat and nutrients to different regions and influencing climate patterns.
3