Return to site

Factors To Control Oceanic Salinity By Best Online tuition Classes

· online tuition class,online tuition,online tuitions,tuition classes,tuition online

The oceanic salinity is a different form of C that depends upon the factors like precipitation influx of the river evaporation and prevailing wind. The best online tuition classes in this article will make you understand the sea waves and ocean currents. The waves are the oscillatory movements that produce winds and manifest into the sea surface. 

broken image

Over the waves are important agents in coastal regions. They are known as various landforms with gulf, capes, Cliff, and bays. Let us understand the movement of ocean currents properly.

Movements of waves by best online tuition classes

The tsunami which hit on 26 December 2004 was the South East Asia which causes heavy damage in the region. The tsunami and seismic waves are caused by volcanic eruptions and earthquakes.  The Indonesian Tsunami Islands of CBSE of Sumatra and Java. Most of the people got injured and killed.

The ocean currents are a continuous directed movement. It generates forces that break waves Coriolis Effect and temperature. The senator difference in the gravitational pull of the sun and moon circulate into clockwise direction. However Northern hemisphere and in the anticlockwise direction, the ocean currents are not the same. 

The best online tuition classes explain that the ocean current is a continuous movement. And are dependent upon two factors

  • Warm current

Yeah, the current flows from lower to higher altitudes and is further known as warm currents.

  • Cold currents

Here, the ocean currents flow from higher latitude to lower latitude and are known as cold currents.

Warm currents are dependent on North equatorial current and North Pacific drift. Not equatorial current flows West water from the Western coast of Mexico to the Philippines. The online class tuition explains that the Kuroshio Current is an extension of not agree told current towards the north. The North Pacific drift is current it extends from Northward to the Pacific drift. 

The current of the South Pacific Ocean is known as the East Australian current. It is also known as a great barrier current. It flows towards the east coast from the equator to the pole. The South equatorial current originates from South East trade and flows westward. The counter equatorial current flows exactly on the equator from west to east. It is the equatorial South current.

  • Cold currents are known as equator that flows in Peru. The west wind drift flows from Tasmania to Chile. America in 40 degrees to 50 degrees South latitude flows under the influence of westerlies. 

The north equatorial current is between the equator and 10 degrees north. Florida is near Florida which is called the US coast. Antilles current flows to the east and follows in other islands. The Gulf Stream flow from the United States coast towards Europe under the influence of Bristol events. However the North Atlantic drift known as gulfstream bifurcates into two called West wind drift and cal current which is called. West wind drift is also called. The second one is not Atlantic drift, which is warm.

The cold current originates from Labrador Current. It originating in Gulf Stream and Newfoundland. New fondant is a famous fishing zone. It is basically known as the Grand Bank. The Grand Bank originated from Greenland and Iceland. Later on it merges with North Atlantic drift. Do you know that the online tuition classes provide you a practical video example of different currents slowly? Cal current flows along the Western coast between Madeira Cape and Verde. 

The currency of the South Atlantic is Warm Current

The South equatorial current flows between equator and 10 degree latitude. It flows in the east coast of Brazil from equator to the pole.

Hollywood, the currents of the Indian Ocean are the most important for all of us.

North equatorial current flows from east to west. It reaches the east coast of Africa and turns southward. It crosses the equator and becomes a Mozambique Current.

South east monsoon drift is along the coast of India. Somalia current flows in the south boundary current that runs along the side of Somalia and Oman. It is similar to the Gulf Stream in the Atlantic Ocean. West Australian current flows in the West coast of Australia. It flows from pole to equator. However there is no counter equatorial current. This Asiatic monsoon influences the current of the north Indian Ocean. For example, it is known as the current of the South Indian Ocean which influences the atmosphere in anticyclonic circulation.

 However this blog will definitely help you in understanding the different ocean currents. West wind drift, Guinea current, Venezuela current and falak land current are the 4 most important currents. They all flow from the coast of Africa then Brazilian then South to North and finally south east coast respectively.The above blog will help you to understand the different oceanic current.