Ocean currents ppt cscope

28
Ocean Current s

description

 

Transcript of Ocean currents ppt cscope

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Warm  currents  flow  away  from  the  equator.      

Cold  currents  flow  toward  the  equator.    

Ocean  Currents  

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Sun  Wind  Coriolis  Gravity    

Factors  Influencing  Currents  

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Energy  from  the  Sun  heats  the  water.  Warm  water  is  less  dense  that  cold  water.  Warm  water  rises,  and  cold  water  sinks.  As  warm  water  rises,  cold  water  moves  it  to  replace  it.  

 

Sun  

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Just  as  wind  moves  from  high  pressure  to  low  pressure  areas,  so  does  the  water.  Winds  blow  across  the  surface  of  the  water,  causing  friction.  The  water  piles  up  because  the  surface  currents  flow  slower  than  the  winds.  

   

Wind  

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As  water  piles  up  and  flows  from  high  pressure  to  low  pressure,  gravity  will  pull  down  on  the  water.  This  forms  vertical  columns  or  mounds  of  water.  The  Coriolis  Effect  causes  the  water  to  curve.  

Gravity  

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Causes  water  to  move  to  the  right  in  the  Northern  Hemisphere    

Causes  water  to  move  to  the  left  in  the  Southern  Hemisphere  

The  Coriolis  Effect  

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The  Coriolis  Effect  

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M  Up  to  maximum  depth  of  400  m  Surface  ocean  currents  are  caused  by  the  surface  wind  patterns.    

Surface  Currents  

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Vertical  columns    or  mounds  of  water  at  the  surface  and  flow  around  them  Produce  enormous  circular  currents    Five  major  locations:  

North  Pacific  -­‐  clockwise  South  Pacific  -­‐  counterclockwise  Indian  Ocean  -­‐  counterclockwise  South  Atlantic  -­‐  counterclockwise  North  Atlantic  -­‐  clockwise    

Gyres  

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A  strong  surface  current  Begins  at  the  tip  of  Florida  Flows  up  the  eastern  coastline  of  the  U.S.    Crosses  the  Atlantic  Ocean  Causes  warmer  climate  in  NW  Europe  

Gulf  Stream  

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Surface  waters  blow  to  the  right  of  the  wind.    

As  less  dense,  surface  water  moves  off  shore,  cold,  deep,  denser  waters  come  to  the  surface  to  replace  them.    

Upwelling  

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 Differences  in  density  cause  them  to  move.  Differences  in  density  are  related  to  temperature  and  salinity.  At  high  latitudes,  they  sink  deep  into  the  ocean  basins.  Temperatures  are  so  cold,  they  cause  the  density  to  increase.  

Deep  Water  Currents  

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How  are  ocean  currents  produced?    

Reflective  Question  

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Abnormally  high  surface  ocean  temperatures  off  the  coast  of  South  America    Causes  unusual  weather  patterns  across  

       the  globe    

 

El  Nino  

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Starts  because  the  easterly  trade  winds  weaken  and  allow  the  warm  waters  in  the  Western  Pacific  to  move  east  toward  South  America  This  changes  where  the  convection  current  occurs.  Causing  rain  where  it  usually  doesn't  occur  and  drought  where  it  usually  rains    

El  Nino  

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Abnormally  low  surface  ocean  temperatures  off  the  coast  of  South  America    Causes  unusual  weather  patterns  across  

       the  globe    

La  Nina  

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Ocean  currents  move  more  slowly  than  winds.  Oceans  hold  more  heat  than  the  atmosphere  and  land.  Cold  currents  will  cause  nearby  coastlines  to  be  cooler.  Warm  currents  will  cause  nearby  coastlines  to  be  warmer.  

 

Where  do  the  cold  currents  come  from?  The  warm  currents?  

 

 

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Predictable  Patterns    How  do  these  currents  affect  the  climate  of  

the  coastline?  

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How  do  our  oceans  impact  climate?  

Reflection  Questions