1. Differential warming
2. Transfer of Wind Energy
3. Coriolis Effect
4. Presence of Continents
Thermohaline circulation is also called overturning circulation. It is driven by density. The time scale for thermohaine is 1000 years.
The Dugong is one, it can be found in the tropical waters of indonesia and also in the waters of northern australia and queensland.
Yes, yes I have, it was swimming in the ocean waters, an inverse sandwich for fishermen and sharks alike.
An ocean current is a continuous, directed movement of ocean water generated by the forces acting upon this mean flow, such as breaking waves, wind, Coriolis effect,cabbeling, temperature and salinity differences and tides caused by the gravitational pull of the Moon and the SunFrom Wiki
Upwelling is when the winds cause nutrient rich waters from lower levels of the ocean to replace the surface water. Upwelling's are usually caused by coastal surges or open oceans.
The tropical ocean waters are more saline than colder waters because due to ocean circulation, as seawater moves in horizontal and vertical directions.
Atmospheric forcing, such as wind and temperature changes, can affect ocean circulation by influencing the movement of surface waters and the formation of ocean currents. These forces can drive the mixing of water masses, impact the distribution of heat and nutrients, and play a role in shaping the overall circulation patterns of the ocean.
Wind stress curl is the change in wind direction and speed over a distance. It affects ocean circulation patterns by creating areas of convergence and divergence in the surface waters. This leads to the formation of ocean currents and the redistribution of heat and nutrients throughout the ocean.
The Arctic Ocean plays a crucial role in deep ocean circulation, particularly through the formation of dense water masses like Arctic Bottom Water (ABW) and Greenland Sea Deep Water. These cold, dense waters sink and contribute to the global thermohaline circulation, influencing the Atlantic Meridional Overturning Circulation. Additionally, the inflow of warmer, saltier water from the Atlantic, such as the North Atlantic Current, affects the overall dynamics of deep ocean circulation in the region.
The Pacific Ocean influences the moistest areas of the world, such as the Amazon Rainforest and Southeast Asia, through its ability to transport moisture through atmospheric circulation patterns like the Hadley Cell and the Intertropical Convergence Zone.
a bottle containing a record of the time and place at which it was set adrift in the ocean for supplying when recovered data to aid in determining the circulation of surface waters in the ocean -called also floater
Converging warm winds over warm ocean waters can be the starting point for the formation of hurricanes or tropical cyclones. The warm ocean waters provide the energy needed for the storm to develop and strengthen, while the converging winds help to create the necessary circulation patterns for the storm to intensify.
The shape of ocean basins influences the direction and flow of ocean currents through the Coriolis effect. Density differences in ocean water, caused by temperature and salinity variations, drive vertical mixing and circulation patterns, such as thermohaline circulation, which play a crucial role in redistributing heat and nutrients around the globe.
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Brackish water is a mixture of fresh and salt water. Rivers coming from inland headed to the ocean are fresh, then as they get closer to the salt water influences, the waters are brackish and then salt as you get closer to the ocean.
Tropical ocean waters are more saline than colder waters because tropical waters undergo ocean currents due to the vertical and horizontal movement of seawater.
arctic ocean