Oceanography, Oceanography in Telugu, ap dsc latest news today, TS DSC, AP DSC, kings dsc, APPSC
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Oceanography, Oceanography in Telugu, ap
Oceanography, Oceanography in Telugu, ap dsc latest news today, TS DSC, AP DSC, kings dsc, APPSC
#Oceanography #Oceanography in Telugu #ap dsc latest news today #TS DSC #AP DSC #kings dsc #APPSC
హాయ్ నా పేరు సోమరాజు. ఏ పి డి ఎస్ సి కంటెంట్ ఎక్ష్ప్లైన్ చేయడానికి ఈ వీడియో లు చేస్తున్నాను. డి ఎస్సి ఖచ్చితంగా సాధించాలి అనేవారి కోసం ఈ వీడియోలు పక్కా ప్రణాళికతో తయారు చేయడం జరుగుతుంది. టెక్స్ట్ బుక్ నే ప్రామాణికం చేసుకొని ప్రతి పాయింట్ లైన్ టు లైన్ టచ్ చేసి అకాడెమి లెవెల్ లో ఒక్క పాయింట్ కుడా మిస్ కాకుండా ఈ వీడియో లు రూపొందించడం జరుగుతుంది. ఈ విడియోలు నచ్చితే లైక్ చేసి సబ్స్క్రయిబ్ చేసుకోండి. అనుదినము మీ ప్రిపరేషన్ లో నా వంతు సహాయంగా అందిస్తుంటాను.చుడండి టెక్స్ట్ బుక్ పాయింట్స్ ని సింపుల్ గా డివైడ్ చేసి మైండ్ మ్యాపింగ్ ద్వారా మీకు బోధించడం జరుగుతుంది. ఒక్కసారి ఈ విడియో చూస్తూ నోట్స్ ప్రిపేర చేసుకొని టెక్స్ట్ బుక్ టెక్స్ట్ బుక్ చుస్తే మికే అర్ధమౌతుంది యెంత పక్కాగా వుందో!
Oceanography is the science of oceans, as the name implies.
Oceanography encompasses all studies conducted on or connected to oceans, from history to current climatic variations; chemistry to biological processes to products; origin to destruction; pollution to conservation.
It is a branch of science that examines the physical, ecological, geomorphic, and dynamic properties of oceans.
Reliefs of the Ocean Basis
Water covers around a third of the earth's surface.
Oceans, Inland Seas, Small Enclosed Seas, Bays, and other hydrosphere features are separated into Oceans, Inland Seas, Small Enclosed Seas, Bays, and other hydrosphere features based on their size and location.
Pacific Ocean, Atlantic Ocean, Indian Ocean, and the Arctic Ocean are the world's four primary oceans.
The ocean floor, which is the 'land' beneath the oceans' waves, has complex and varied features similar to those seen on land.
Tectonic, volcanic, erosional, and depositional processes, as well as their interactions, all contribute to the formation of ocean relief.
There are four relief zones on the ocean floor:
Continental Shelf
Continental Slope
Deep-Sea Plain and
Oceanic deep or trench.
Temperature and Density of Ocean Water
Massive meteorology, which deals with the portion of the atmosphere that overspreads the huge water masses, is concerned with the study of ocean temperatures.
One of the most important responsibilities of oceanographers has been to determine the temperature of the sea and to accurately measure it, as this aids in the determination of the motions of enormous amounts of ocean water.
The density of a substance is defined as its mass per unit volume expressed in grams per cubic centimeter.
The term density is commonly used to refer to specific gravity, which is defined as the ratio of density to that of distilled water at a certain temperature and pressure.
At 4 degrees Celsius, pure water has a maximum density of one unit, however, the density of the sea varies depending on the salinity content.
Pure water's density is only determined by temperature and pressure.
Seawater, on the other hand, is affected by temperature, pressure, and salinity.
The effect of salt on density and freezing point is depicted in this diagram.
Salinity
The entire amount of solid material in a kilogram of seawater, expressed in parts per thousand, is referred to as salinity.
The average salinity of saltwater is 3.5 percent, which is measured in parts per thousand.
Winds caused by variations in air pressure cause salinity to fluctuate.
The strong winds that blow throughout the year transport much of the warm and saline water from the western shore of the land in the lower middle latitudes to the eastern shore in the higher latitudes, causing salinity distribution to alter.
The nature of the atmosphere, i.e. the difference between precipitation and evaporation, determines salinity changes.
Movement of Ocean Water
Movement of Ocean Water
The water in the ocean is never still. Diverse forms of ocean water flows exist as a result of different physical qualities such as temperature, salinity, density, and so on. External influences such as the sun, moon, and winds influence the movement of ocean water.
The major movements of ocean waters can be divided into three categories. They are as follows:
Waves
Tides
Ocean Currents
Ocean currents and waves are horizontal motions of ocean waters, whereas the tide is a vertical flow of ocean water.
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#Oceanography #Oceanography in Telugu #ap dsc latest news today #TS DSC #AP DSC #kings dsc #APPSC
హాయ్ నా పేరు సోమరాజు. ఏ పి డి ఎస్ సి కంటెంట్ ఎక్ష్ప్లైన్ చేయడానికి ఈ వీడియో లు చేస్తున్నాను. డి ఎస్సి ఖచ్చితంగా సాధించాలి అనేవారి కోసం ఈ వీడియోలు పక్కా ప్రణాళికతో తయారు చేయడం జరుగుతుంది. టెక్స్ట్ బుక్ నే ప్రామాణికం చేసుకొని ప్రతి పాయింట్ లైన్ టు లైన్ టచ్ చేసి అకాడెమి లెవెల్ లో ఒక్క పాయింట్ కుడా మిస్ కాకుండా ఈ వీడియో లు రూపొందించడం జరుగుతుంది. ఈ విడియోలు నచ్చితే లైక్ చేసి సబ్స్క్రయిబ్ చేసుకోండి. అనుదినము మీ ప్రిపరేషన్ లో నా వంతు సహాయంగా అందిస్తుంటాను.చుడండి టెక్స్ట్ బుక్ పాయింట్స్ ని సింపుల్ గా డివైడ్ చేసి మైండ్ మ్యాపింగ్ ద్వారా మీకు బోధించడం జరుగుతుంది. ఒక్కసారి ఈ విడియో చూస్తూ నోట్స్ ప్రిపేర చేసుకొని టెక్స్ట్ బుక్ టెక్స్ట్ బుక్ చుస్తే మికే అర్ధమౌతుంది యెంత పక్కాగా వుందో!
Oceanography is the science of oceans, as the name implies.
Oceanography encompasses all studies conducted on or connected to oceans, from history to current climatic variations; chemistry to biological processes to products; origin to destruction; pollution to conservation.
It is a branch of science that examines the physical, ecological, geomorphic, and dynamic properties of oceans.
Reliefs of the Ocean Basis
Water covers around a third of the earth's surface.
Oceans, Inland Seas, Small Enclosed Seas, Bays, and other hydrosphere features are separated into Oceans, Inland Seas, Small Enclosed Seas, Bays, and other hydrosphere features based on their size and location.
Pacific Ocean, Atlantic Ocean, Indian Ocean, and the Arctic Ocean are the world's four primary oceans.
The ocean floor, which is the 'land' beneath the oceans' waves, has complex and varied features similar to those seen on land.
Tectonic, volcanic, erosional, and depositional processes, as well as their interactions, all contribute to the formation of ocean relief.
There are four relief zones on the ocean floor:
Continental Shelf
Continental Slope
Deep-Sea Plain and
Oceanic deep or trench.
Temperature and Density of Ocean Water
Massive meteorology, which deals with the portion of the atmosphere that overspreads the huge water masses, is concerned with the study of ocean temperatures.
One of the most important responsibilities of oceanographers has been to determine the temperature of the sea and to accurately measure it, as this aids in the determination of the motions of enormous amounts of ocean water.
The density of a substance is defined as its mass per unit volume expressed in grams per cubic centimeter.
The term density is commonly used to refer to specific gravity, which is defined as the ratio of density to that of distilled water at a certain temperature and pressure.
At 4 degrees Celsius, pure water has a maximum density of one unit, however, the density of the sea varies depending on the salinity content.
Pure water's density is only determined by temperature and pressure.
Seawater, on the other hand, is affected by temperature, pressure, and salinity.
The effect of salt on density and freezing point is depicted in this diagram.
Salinity
The entire amount of solid material in a kilogram of seawater, expressed in parts per thousand, is referred to as salinity.
The average salinity of saltwater is 3.5 percent, which is measured in parts per thousand.
Winds caused by variations in air pressure cause salinity to fluctuate.
The strong winds that blow throughout the year transport much of the warm and saline water from the western shore of the land in the lower middle latitudes to the eastern shore in the higher latitudes, causing salinity distribution to alter.
The nature of the atmosphere, i.e. the difference between precipitation and evaporation, determines salinity changes.
Movement of Ocean Water
Movement of Ocean Water
The water in the ocean is never still. Diverse forms of ocean water flows exist as a result of different physical qualities such as temperature, salinity, density, and so on. External influences such as the sun, moon, and winds influence the movement of ocean water.
The major movements of ocean waters can be divided into three categories. They are as follows:
Waves
Tides
Ocean Currents
Ocean currents and waves are horizontal motions of ocean waters, whereas the tide is a vertical flow of ocean water.
download free Video intro & logos templates from renderforest.com
https://www.renderforest.com/
Copyright Notice:-
Please feel free to leave me a notice if You find this upload inappropriate.
Contact me personally if You are against an upload which You may have rights to the Images (or) music,
instead of contacting YouTube about a Copyright Infringement....Thank You..!"
if you found this video Helpful give it a like.
If you know someone who needs to see it, share it.
Leave a comment below with your thoughts or any queries regarding any technology..
Thank you for watching..!!
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