SlideShare a Scribd company logo
1 of 20
Energy Transfer: In Atmosphere and In Oceans By: OwaisFarooq Hovo Khachikyan Halim Hakimi  1
Table of Content ,[object Object]
 What is energy transfer
Absorption if the Sun’s energy
Energy Transfer in Atmosphere
Energy Transfer within the Climate System Diagram
Energy transfer in Oceans
Ocean Currents around the World
Citation2
Introduction Most of the Energy on Earth comes from our sun which releases number of different types of radiation. For example Ultraviolet radiation which is a form of invisible high-energy radiation and Infrared radiation which is a form of a invisible lower-energy radiation. The Energy can be transferred in Oceans and In the Atmosphere.… 3
What is Energy Transfer 		You have seen how the weather changes from hot to cold or cold to hot, it gets warmer in summer and etc. The climate transports thermal energy from regions that receive a lot of radiation to regions that receive less radiation, that is transferring energy from place to place. If the Sun’s light worms you in summer, its also energy transfer but in deferent shape. Energy transfer is the transfer of energy from one body into another. 4 	There are two main ways of transferring  the suns Energy around the Earth. One  way is in the Atmosphere and the other is in then oceans. The energy coming from the sun is transferred by convection, conduction and lastly by radiation taking place in the atmosphere and the surface of the Earth.
Absorption of the Sun’s Energy When Solar Energy reaches Earth, It is either reflected or absorbed. Some solar energy is reflected back into outer space by clouds, by particles In the atmosphere and also by Earth's surface which includes oceans. Almost 70% of the solar energy is absorbed by the Earth's atmosphere, water and land. 5
Absorption of the Sun’s Energy    The absorbed solar energy by the Earth's atmosphere, water and land is converted to a thermal energy. A thermal energy is the energy which is associated with the temperature of a substance and changes of state. The Thermal energy causes land and water to become warmer. 6
Absorption of the Sun’s Energy 7 In this following diagram 6% of the energy is reflected by the atmosphere while 20% is reflected by the clouds and 4% is reflected from the Earth’s surface. While 16% is absorbed by the atmosphere and 3% is absorbed by the clouds and 51% is absorbed by land and oceans.
Energy Transfer:  Atmosphere 8
Energy Transfer In Atmosphere 		Almost all the energy comes from Sun. The sun sends to earth 2 kind of radiation, ultraviolet radiation which is invisible  short wavelength, and infrared radiation that is invisible with long wavelength. 		Air at the equator heats up and becomes less dense. Colder denser air drops, pushing the warm air into the atmosphere. The warm air creates an area of low pressure. When the warm air reaches the troposphere, it cools down and drops back down to Earths surface. This movement of warm and cold air is called convection currents. 9
 Convection Currents  	The pattern of convection currents at the equator is repeated at the poles. This is the reason why earth has permanent bands of high and low pressure.      Convection currents are one of the main ways of energy transfer through the atmosphere. This way thermal energy is transported from the equator to the North and South Poles. Air currents that move from high to low pressure are known as winds. Winds blow in the same direction, from the areas of high pressure to areas of low pressure. These prevailing winds move warm air from the equator to the poles. 10
Energy Transfer within the Climate System Diagram 11 Bends of High and Low pressure around the globe creates air currents (winds) that blow from areas of high pressure to areas of low pressure. Winds are named based on the direction they originate from.
Energy Transfer:Oceans 12
Energy Transfer in the Ocean… 		As you know from before, the colder the air is, the more dense it is. This is how the Ocean works too. The water traveling to the North and South poles gets colder and saltier because when the ice is frozen over, it rejects the salt. The low temperatures and the saltiness make the water at the poles more dense. Also, it works the way the air in atmosphere system. Warm water travels to South or North pole, when it gets cold, it comes back to the center of the earth.  13

More Related Content

What's hot

Global air circulation
Global air circulationGlobal air circulation
Global air circulationTsiamo Mokgopa
 
General Circulation of the Atmosphere
General Circulation of the AtmosphereGeneral Circulation of the Atmosphere
General Circulation of the AtmosphereKhalilur Rahman
 
Global energy budget
Global energy budgetGlobal energy budget
Global energy budgetmusadoto
 
3331_Lecture6_GlobalCirculation_F13.pdf
3331_Lecture6_GlobalCirculation_F13.pdf3331_Lecture6_GlobalCirculation_F13.pdf
3331_Lecture6_GlobalCirculation_F13.pdfPeaceMakah1
 
94. Power of the Sun Notes
94. Power of the Sun Notes94. Power of the Sun Notes
94. Power of the Sun Notesmgitterm
 
Earth's energy and seasons
Earth's energy and seasonsEarth's energy and seasons
Earth's energy and seasonsGeronimo Rosario
 
3. ESS Systems and Feedback Notes
3. ESS Systems and Feedback Notes3. ESS Systems and Feedback Notes
3. ESS Systems and Feedback Notesmgitterm
 
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology ChapterAtmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology ChapterKaium Chowdhury
 
Climate and Ocean Currents
Climate and Ocean CurrentsClimate and Ocean Currents
Climate and Ocean Currentsdwinter1
 
Atmospheric circulation
Atmospheric circulationAtmospheric circulation
Atmospheric circulationSarah Zurcaled
 
Ocean Currents 1
Ocean Currents 1Ocean Currents 1
Ocean Currents 1GeoCoops
 
105. Lithospheric Effects on Climate Change
105. Lithospheric Effects on Climate Change105. Lithospheric Effects on Climate Change
105. Lithospheric Effects on Climate Changemgitterm
 
Air sea interaction
Air sea interactionAir sea interaction
Air sea interaction末 Wei
 
Phes ch20 Severe Weather
Phes ch20 Severe WeatherPhes ch20 Severe Weather
Phes ch20 Severe Weatherwindyridge
 
Atmosphere revision booklet 2014 cg malia
Atmosphere revision booklet 2014 cg maliaAtmosphere revision booklet 2014 cg malia
Atmosphere revision booklet 2014 cg maliaMalia Damit
 

What's hot (20)

Global circulation patterns of atmosphere
Global circulation patterns of atmosphereGlobal circulation patterns of atmosphere
Global circulation patterns of atmosphere
 
Global air circulation
Global air circulationGlobal air circulation
Global air circulation
 
General Circulation of the Atmosphere
General Circulation of the AtmosphereGeneral Circulation of the Atmosphere
General Circulation of the Atmosphere
 
Energy budget of earth
Energy budget of earthEnergy budget of earth
Energy budget of earth
 
Global energy budget
Global energy budgetGlobal energy budget
Global energy budget
 
3331_Lecture6_GlobalCirculation_F13.pdf
3331_Lecture6_GlobalCirculation_F13.pdf3331_Lecture6_GlobalCirculation_F13.pdf
3331_Lecture6_GlobalCirculation_F13.pdf
 
Global air circulation
Global air circulation Global air circulation
Global air circulation
 
94. Power of the Sun Notes
94. Power of the Sun Notes94. Power of the Sun Notes
94. Power of the Sun Notes
 
Earth's energy and seasons
Earth's energy and seasonsEarth's energy and seasons
Earth's energy and seasons
 
3. ESS Systems and Feedback Notes
3. ESS Systems and Feedback Notes3. ESS Systems and Feedback Notes
3. ESS Systems and Feedback Notes
 
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology ChapterAtmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
 
Energy budgets
Energy budgetsEnergy budgets
Energy budgets
 
Climate and Ocean Currents
Climate and Ocean CurrentsClimate and Ocean Currents
Climate and Ocean Currents
 
Atmospheric circulation
Atmospheric circulationAtmospheric circulation
Atmospheric circulation
 
Ocean Currents 1
Ocean Currents 1Ocean Currents 1
Ocean Currents 1
 
2 W&C OVERVIEW PPT
2 W&C OVERVIEW PPT 2 W&C OVERVIEW PPT
2 W&C OVERVIEW PPT
 
105. Lithospheric Effects on Climate Change
105. Lithospheric Effects on Climate Change105. Lithospheric Effects on Climate Change
105. Lithospheric Effects on Climate Change
 
Air sea interaction
Air sea interactionAir sea interaction
Air sea interaction
 
Phes ch20 Severe Weather
Phes ch20 Severe WeatherPhes ch20 Severe Weather
Phes ch20 Severe Weather
 
Atmosphere revision booklet 2014 cg malia
Atmosphere revision booklet 2014 cg maliaAtmosphere revision booklet 2014 cg malia
Atmosphere revision booklet 2014 cg malia
 

Similar to Enegy transfer v7

6th Grade Chapter 18 Part 1- atmosphere
6th Grade Chapter 18 Part 1- atmosphere6th Grade Chapter 18 Part 1- atmosphere
6th Grade Chapter 18 Part 1- atmosphereSteven_iannuccilli
 
4.1 -- BIO
4.1 -- BIO4.1 -- BIO
4.1 -- BIOheyylo
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's ClimateOhMiss
 
4.1 Climate
4.1 Climate4.1 Climate
4.1 Climateedraesel
 
ATMOSPHERIC CIRCULATION.pptx
ATMOSPHERIC CIRCULATION.pptxATMOSPHERIC CIRCULATION.pptx
ATMOSPHERIC CIRCULATION.pptxEricJoseph31
 
Weather basics
Weather basicsWeather basics
Weather basicsowenfidler
 
Tropical deforestation, global climate change, ENSO and possible feedback amp...
Tropical deforestation, global climate change, ENSO and possible feedback amp...Tropical deforestation, global climate change, ENSO and possible feedback amp...
Tropical deforestation, global climate change, ENSO and possible feedback amp...Paul Pittman
 
Atmosphere 15
Atmosphere   15Atmosphere   15
Atmosphere 15llaub
 
Monsoon system and Ocean currents around Sri Lanka
Monsoon system and Ocean currents around Sri LankaMonsoon system and Ocean currents around Sri Lanka
Monsoon system and Ocean currents around Sri LankaPrasad Madushanka
 
Higher Atmosphere Revision
Higher Atmosphere RevisionHigher Atmosphere Revision
Higher Atmosphere RevisionOllie Bray
 

Similar to Enegy transfer v7 (20)

Enegy transfer v5
Enegy transfer v5Enegy transfer v5
Enegy transfer v5
 
6th Grade Chapter 18 Part 1- atmosphere
6th Grade Chapter 18 Part 1- atmosphere6th Grade Chapter 18 Part 1- atmosphere
6th Grade Chapter 18 Part 1- atmosphere
 
Chapter 15-atmosphere
Chapter 15-atmosphereChapter 15-atmosphere
Chapter 15-atmosphere
 
4.1 -- BIO
4.1 -- BIO4.1 -- BIO
4.1 -- BIO
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's Climate
 
CLIMATOLOGY CLIMATOLOGY
CLIMATOLOGY CLIMATOLOGYCLIMATOLOGY CLIMATOLOGY
CLIMATOLOGY CLIMATOLOGY
 
Ch 15 ed
Ch 15 edCh 15 ed
Ch 15 ed
 
CLIMATOLOGY
CLIMATOLOGYCLIMATOLOGY
CLIMATOLOGY
 
Weather
WeatherWeather
Weather
 
Chapter 17
Chapter 17Chapter 17
Chapter 17
 
4.1 Climate
4.1 Climate4.1 Climate
4.1 Climate
 
ATMOSPHERIC CIRCULATION.pptx
ATMOSPHERIC CIRCULATION.pptxATMOSPHERIC CIRCULATION.pptx
ATMOSPHERIC CIRCULATION.pptx
 
Chapt15 lecture
Chapt15 lectureChapt15 lecture
Chapt15 lecture
 
Weather basics
Weather basicsWeather basics
Weather basics
 
Climatology
ClimatologyClimatology
Climatology
 
Tropical deforestation, global climate change, ENSO and possible feedback amp...
Tropical deforestation, global climate change, ENSO and possible feedback amp...Tropical deforestation, global climate change, ENSO and possible feedback amp...
Tropical deforestation, global climate change, ENSO and possible feedback amp...
 
Atmosphere 15
Atmosphere   15Atmosphere   15
Atmosphere 15
 
Monsoon system and Ocean currents around Sri Lanka
Monsoon system and Ocean currents around Sri LankaMonsoon system and Ocean currents around Sri Lanka
Monsoon system and Ocean currents around Sri Lanka
 
Higher Atmosphere Revision
Higher Atmosphere RevisionHigher Atmosphere Revision
Higher Atmosphere Revision
 
B10vrv2041
B10vrv2041B10vrv2041
B10vrv2041
 

Enegy transfer v7

  • 1. Energy Transfer: In Atmosphere and In Oceans By: OwaisFarooq Hovo Khachikyan Halim Hakimi 1
  • 2.
  • 3. What is energy transfer
  • 4. Absorption if the Sun’s energy
  • 5. Energy Transfer in Atmosphere
  • 6. Energy Transfer within the Climate System Diagram
  • 10. Introduction Most of the Energy on Earth comes from our sun which releases number of different types of radiation. For example Ultraviolet radiation which is a form of invisible high-energy radiation and Infrared radiation which is a form of a invisible lower-energy radiation. The Energy can be transferred in Oceans and In the Atmosphere.… 3
  • 11. What is Energy Transfer You have seen how the weather changes from hot to cold or cold to hot, it gets warmer in summer and etc. The climate transports thermal energy from regions that receive a lot of radiation to regions that receive less radiation, that is transferring energy from place to place. If the Sun’s light worms you in summer, its also energy transfer but in deferent shape. Energy transfer is the transfer of energy from one body into another. 4 There are two main ways of transferring the suns Energy around the Earth. One way is in the Atmosphere and the other is in then oceans. The energy coming from the sun is transferred by convection, conduction and lastly by radiation taking place in the atmosphere and the surface of the Earth.
  • 12. Absorption of the Sun’s Energy When Solar Energy reaches Earth, It is either reflected or absorbed. Some solar energy is reflected back into outer space by clouds, by particles In the atmosphere and also by Earth's surface which includes oceans. Almost 70% of the solar energy is absorbed by the Earth's atmosphere, water and land. 5
  • 13. Absorption of the Sun’s Energy The absorbed solar energy by the Earth's atmosphere, water and land is converted to a thermal energy. A thermal energy is the energy which is associated with the temperature of a substance and changes of state. The Thermal energy causes land and water to become warmer. 6
  • 14. Absorption of the Sun’s Energy 7 In this following diagram 6% of the energy is reflected by the atmosphere while 20% is reflected by the clouds and 4% is reflected from the Earth’s surface. While 16% is absorbed by the atmosphere and 3% is absorbed by the clouds and 51% is absorbed by land and oceans.
  • 15. Energy Transfer: Atmosphere 8
  • 16. Energy Transfer In Atmosphere Almost all the energy comes from Sun. The sun sends to earth 2 kind of radiation, ultraviolet radiation which is invisible short wavelength, and infrared radiation that is invisible with long wavelength. Air at the equator heats up and becomes less dense. Colder denser air drops, pushing the warm air into the atmosphere. The warm air creates an area of low pressure. When the warm air reaches the troposphere, it cools down and drops back down to Earths surface. This movement of warm and cold air is called convection currents. 9
  • 17. Convection Currents The pattern of convection currents at the equator is repeated at the poles. This is the reason why earth has permanent bands of high and low pressure. Convection currents are one of the main ways of energy transfer through the atmosphere. This way thermal energy is transported from the equator to the North and South Poles. Air currents that move from high to low pressure are known as winds. Winds blow in the same direction, from the areas of high pressure to areas of low pressure. These prevailing winds move warm air from the equator to the poles. 10
  • 18. Energy Transfer within the Climate System Diagram 11 Bends of High and Low pressure around the globe creates air currents (winds) that blow from areas of high pressure to areas of low pressure. Winds are named based on the direction they originate from.
  • 20. Energy Transfer in the Ocean… As you know from before, the colder the air is, the more dense it is. This is how the Ocean works too. The water traveling to the North and South poles gets colder and saltier because when the ice is frozen over, it rejects the salt. The low temperatures and the saltiness make the water at the poles more dense. Also, it works the way the air in atmosphere system. Warm water travels to South or North pole, when it gets cold, it comes back to the center of the earth. 13
  • 21. Climate Zones Warm ocean currents heat the air above them , this warm moist air reaches the land and produces rain. This is how the affect takes place. The Gulf Stream currents give the northwest coast of Europe a warmer climate than it would otherwise have. Cold ocean currents cool the air above them, it cools the land and create desert areas. California and parts of Mexico are cooler and drier because of the cold ocean currents. 14
  • 22. Ocean Currents Ocean currents have a major impact on the climates of nearby land. Ocean currents act like conveyer belts, they move the water and its thermal energy from the equator to the poles and circulate all over the world. Winds also cause ocean currents. Wind are the main cause of the Gulf Stream that transports warm water from the tropics up to the eastern coast of North America and across to Europe. Ocean currents have a strong affect on the climate of the land around them. 15
  • 23. Ocean currents around the World 16 In this following diagrams the Red lines represent the warm ocean currents while the blue lines represent the cold ones.
  • 24. Ocean Currents-Gulf Stream The Ocean Currents act as conveyor belts which moves cold and hot water and at the same time It moves the thermal energy from the equator to the poles. The ocean currents are also caused by winds and one of the examples would be the Gulf Stream. 17
  • 25. Gulf Stream 18 In this following diagram we can see the Gulf Stream which is in bright red colour representing the warm currents while the blue one represents the cold current. The Gulf Stream Is one of the Warm ocean currents and it transports and carries thermal energy
  • 26. Summary - Overview Two types of Energy Transfer:In the oceans and In the Atmosphere Air and Ocean currents are the main ways that energy is transported around the earth Ocean currents affect the climate of their surrounding nearby land. Convection currents transport warm and cold winds all over the Earth Gulf Stream is a very large ocean current which has changed the climate of many places. Video:http://www.brightstorm.com/science/physics/heat-transfer-and-change-of-phase/thermal-energy-transfer 19
  • 27. Citations "All About Frozen Ground: How Does It Form?" National Snow and Ice Data Center (NSIDC). Web. 10 Jan. 2011. <http://nsidc.org/frozenground/how_fg_forms.html>. "Introduction to the Atmosphere: Background Material." UCAR | Understanding Atmosphere, Earth, and Sun | Home. Web. 9 Jan. 2011. <http://www.ucar.edu/learn/1_1_1.htm>. Adam-Carr, Christine, and Martin Gabber. "Energy Transfer: Oceans and Atmosphere." Science Perspectives 10. Toronto: Nelson Education, 2010. 326+. Print. "Thermal Energy Transfer - Free Science Videos by Brightstorm." Free Homework Help Videos from Brightstorm - Math, Science, Test Prep - Brightstorm. Web. 18 Jan. 2011. <http://www.brightstorm.com/science/physics/heat-transfer-and-change-of-phase/thermal-energy-transfer>. "Temperature of the Gulf Stream : Image of the Day." NASA Earth Observatory : Home. Web. 13 Jan. 2011. <http://earthobservatory.nasa.gov/IOTD/view.php?id=681>. 20