Presentation is loading. Please wait.

Presentation is loading. Please wait.

 Susan Howard  Earth & Space Research Basically – why and how the ocean and atmosphere MOVE! www.ametsoc.org There are many scales of motion: From BIG.

Similar presentations


Presentation on theme: " Susan Howard  Earth & Space Research Basically – why and how the ocean and atmosphere MOVE! www.ametsoc.org There are many scales of motion: From BIG."— Presentation transcript:

1  Susan Howard  Earth & Space Research Basically – why and how the ocean and atmosphere MOVE! There are many scales of motion: From BIG to very small Today – I will just cover the basic large scale, GLOBAL circulation.

2 The Ocean and Atmosphere are in CONSTANT motion NASA/Goddard Space Flight Center Scientific Visualization Studio NASA Movie: Perpetual Ocean Model of ocean currents based on data from satellites and other measurements.

3 There are 2 main things that form the Global Ocean and Atmospheric circulation patterns  set up the climate system we know it. Energy from the Sun Rotation of the earth Warming from the sun Sets it in Motion The rotation directs the motion

4 Energy and the Sun The Sun is constantly emitting energy, in the form of “electrogmagnetic radiation”. What is ELECTROMAGNETIC RADIATION? Light Infrared (Heat) Xrays Microwaves Ultraviolet radiation (sunburns!)

5 Solar radiation travels through space and hits the earth and warms it. The Heating of the Earth is Not Even!

6 Short length of day Small angle of incidence/ low intensity Large amounts of Ice cover Noon in Antarctica May 23 rd, 2001 May 23 rd, 2001 UNEVEN HEATING: The daily amount of warming at a point on the Earth depends on 3 things

7 The Heating of the Earth is Not Even! Length of Day - How much sunlight a point receives in a day Angle of Incidence (Intensity) – the angle of the sunlight that reaches the earth Albedo – how much of this light is reflected.

8 Length of Day Earth is tilted with respect to Sun Length of day changes throughout the year Source: Wikipedia NH Summer NH Winter

9 Length of Day Source: Wikipedia

10 Angle of Incidence A beam of light shining straight down is more intense that a beam of light shining at an angle The angle the incoming light makes with respect to the Earth

11 Angle of incidence Wikipedia

12 Intensity of Radiation Varies with Latitude The further you get from equator, the less radiation reaches the earth per area Source:

13 Because the Polar regions receive less radiation, they are cooler. Because they are cooler – ice forms. It reflects the solar radiation What does Sea Ice do? High albedo – high reflection Low albedo – high absorption

14 Ice cover – reflects radiation Radiation reflected Radiation absorbed Warms water So Ice makes the polar regions even cooler!

15 So, because of angle of incidence, length of day, & ice: EquatorEquator PolePole The Equator gets more heat than the Poles... a lot more! WarmerCooler

16 Average Annual Heating by Sun Source: PhysicalGeography.net

17 Average Annual Heating by Sun Source: Wikipedia

18 Ocean temperature movietemperature From NOAA, Based on satellite measurements

19 What does this Uneven Heating do? Hot air and cold air behave differently Hot air rises Cold air will sink. And this causes MOTION

20 Warm air rises Cold air sinks How Wind Forms Low Pressure High Pressure Wind Convection Cell ****Air likes to go from areas of High pressure to Low pressure

21 The GLOBAL Air Circulation is controlled by these convection cells Figure 7.5 in The Atmosphere, 8th edition, Lutgens and Tarbuck, 8th edition, 2001.

22 So, we know: 1)The SUN heats the earth UNEVENLY – And this is going to cause motion. a.The uneven heating causes the rising and sinking of air b.And this rising and sinking causes WIND. c.The sun has set the atmosphere in motion 2) What going to now DIRECT this motion ? ROTATION of the Earth

23 2) Rotation of the Earth it helps DIRECT the circulation. It works at right angles to motion and makes the motion curve Coriolis Force

24 Equator Right in Northern Hemisphere Left in Southern Hemisphere Coriolis Force

25 Global Wind Patterns No Rotation With Rotation

26 Global wind patterns based on Solar heating and Rotation Early Explorers relied on the global wind patterns to sail around the world

27 Summary Movie – Air circulation MovieMovie : Global Atmospheric Circulation By Keith Meldahl, YouTube video

28 Sun’s Heating and Earth’s rotation create wind circulation patterns creates Global Surface Currents in Ocean

29 Wind motion creates Surface Currents in Ocean

30 Map of basic surface currents

31 Wind AND ocean currents

32 Because of uneven heating, just like the Atmosphere, the ocean also has Convection Cells which drives DEEP circulation The Wind drives large scale surface currents but that isn’t all.

33 Basic facts Warm WATER risesCold WATER sinks Warm air rises Cold air sinks

34 Ocean Conveyer Belt

35 Ocean circulation – major currents MovieMovie : GFDL Ocean current move

36 Questions?


Download ppt " Susan Howard  Earth & Space Research Basically – why and how the ocean and atmosphere MOVE! www.ametsoc.org There are many scales of motion: From BIG."

Similar presentations


Ads by Google