SlideShare a Scribd company logo
1 of 16
Download to read offline
How Our Oceans Move
and Why We Care...
Benicat, Sabrina, Kijana, Bella
Counselors: Maria and Aisha
Intro: Mechanical Engineering
Mechanical
Engineering
“Classical”
engineering
Quantum
Mechanics
Fluid
Mechanics
Computational
Fluid Dynamics
Study of
classical
engineering
Studying
Newton’s
Law
Physics-
looks at
particle
movement
Air, water;
study of any
gas/ liquids
Solving
equations of
fluid mechanics
on a computer
Ocean Modeling
Why do we need to understand how the Ocean Moves?
weather
climate
natural disasters:
***we LOVE Earth***
hurricanes, tsunamis, tornadoes, earthquakes,
volcanoes, sinkholes, droughts, heat, waves,
wildfires, floods, blizzards, avalanches
Ocean Circulation
- Stratification
- Rotation of the Earth
- Wind
- Continental Boundaries
These factors cause
-Small Scale Ocean Phenomena
-Medium Scale Ocean Phenomena
-Large Scale Ocean Phenomena
Small Scale Phenomena
- Micro-turbulence
-Gravity
-Tides
Observation Day
Density & Stratification
Density is a characteristic property of a
substance
Density = mass / volume
rho = m / v
Global Winds
∗ Coriolis Force
∗ Gulf Stream
Westerlies:
∗ Lie between the Northern
and Southern Hemisphere
∗ Blows from west to east
along the equator
∗ Highly variable and
unsteady winds
∗ Part of hurricanes,
tsunamis, monsoons, etc.
Frequent changes to the
weather:
∗ Mid-latitude storms
∗ Wintertime changes
Trade:
∗Travels from east to west
∗ Lie on both sides of the
equator which:
∗ Gives out steady wind flow
∗ Ocean waves are very
steady around these areas
∗ Sail and fishing boats
depend on the airflow to get
to nearby coastal areas
safely
Thermohaline
Circulation
-Large Scale Ocean Phenomena
-Deep and shallow currents create the well known "Great
Ocean Conveyor Belt"
-Regulates our climate
-The movement of large quantities of water allow for the
transportation of nutrients and heat
-It is the overall circulation of the ocean, if it shuts down
everything would collapse
The Experiment
-Lab simulation of the differences in water temperature
-The lab was conducted by placing ice packs on one end of
the dish and placing a lamp on the on the other end.
-The water had to stand for 20-30 minutes and then colored
dye was added.
-The warm water(red/equator) rose above the colder
water(blue/North Pole)
Western Boundary Currents
Causes
1. Wind
2. Rotation of the earth
3. Continental boundaries
Hypothesis
The Western Boundaries Currents (WBCs) need all the three factors to develop
the circulation pattern observed by satellites.
Methods
-Set up laboratory scale experiment that mimic Western Boundary Currents
-Set up computational experiments that mimic Western Boundary Currents
Lab Experiment
Materials
-Big plastic tank
(continental
boundaries)
- Water (ocean)
- Slope (spherical
rotation)
- Two little pillars
- Fans (winds)
- Red and blue dye
- Turntable (rotation of
earth)
- Camera
Procedure
-Set up the two little pillars
-Put in the slope
-Fill the tank with water
-Adjust the fans (North and South side of
the box) SP=West ;NP=East (to mimic
the winds)
-Set up the camera
-Begin the counterclockwise rotation of
the tank, like the Earth
-Let it spin for 20-30 minutes
-When ready, add the red & blue dyes
(red = southwest & blue = northeast )
Trials
Trial A - All factors
Trial B - No wind (no fans)
Trial C - No spherical
rotation (no slope)
Trial D - No rotation of Earth
(no rotation of tank)
Observations
Computational Experiment :MATLAB
The 5 Factors
1. Local Changes
2. Convection
3. Coriolis
4. Wind
5. Diffusion/ smoothing/ disappearing effect
Trials
Case 1 = All Terms
Case 2 = No Convection
Case 3 = No Coriolis
Case 4 = No Wind
Case 5 = No Diffusion
Experiment
- Using a coding program MATLAB we were able to view different
simulations on the computer
- Equations used in mechanical engineering are long and complex
that they can easily be solved using a software such as MATLAB
- The equation we plugged in was the Barotropic Vorticity Equation
- Vorticity: a measure of how much the fluid spins
- We were able to make videos of how the western boundary
currents look from satellites
Look at video
Why do we care?
-Melting of ice caps slows thermohaline
circulation causing extreme climate change
-The ocean’s temperature increase and
sea level rise will cause severe hurricanes
Thank You
Professor Reckinger, REU Researchers, and Counselors

More Related Content

What's hot

Simulation Tool for GNSS Ocean Surface Reflections
Simulation Tool for GNSS Ocean Surface ReflectionsSimulation Tool for GNSS Ocean Surface Reflections
Simulation Tool for GNSS Ocean Surface ReflectionsTibor Durgonics
 
Effective Discharge Nooksack Watershed
Effective Discharge Nooksack WatershedEffective Discharge Nooksack Watershed
Effective Discharge Nooksack WatershedLeif Embertson
 
3.3 Climate data and projections
3.3 Climate data and projections3.3 Climate data and projections
3.3 Climate data and projectionsNAP Events
 
Emma Hutchinson SESUR poster
Emma Hutchinson SESUR posterEmma Hutchinson SESUR poster
Emma Hutchinson SESUR posterEmma Hutchinson
 
Climate Modelling, Predictions and Projections
Climate Modelling, Predictions and ProjectionsClimate Modelling, Predictions and Projections
Climate Modelling, Predictions and Projectionsipcc-media
 
Climate Change
Climate ChangeClimate Change
Climate ChangeTom Moritz
 
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814Peter Burgess
 
Publication_Draft_09Aug
Publication_Draft_09AugPublication_Draft_09Aug
Publication_Draft_09AugKevin Schmidt
 
Modeling Past and Future Climate
Modeling Past and Future ClimateModeling Past and Future Climate
Modeling Past and Future ClimateAndreas Schmittner
 

What's hot (20)

Simulation Tool for GNSS Ocean Surface Reflections
Simulation Tool for GNSS Ocean Surface ReflectionsSimulation Tool for GNSS Ocean Surface Reflections
Simulation Tool for GNSS Ocean Surface Reflections
 
Effective Discharge Nooksack Watershed
Effective Discharge Nooksack WatershedEffective Discharge Nooksack Watershed
Effective Discharge Nooksack Watershed
 
3.3 Climate data and projections
3.3 Climate data and projections3.3 Climate data and projections
3.3 Climate data and projections
 
Emma Hutchinson SESUR poster
Emma Hutchinson SESUR posterEmma Hutchinson SESUR poster
Emma Hutchinson SESUR poster
 
NASA Science
NASA ScienceNASA Science
NASA Science
 
Climate Modelling, Predictions and Projections
Climate Modelling, Predictions and ProjectionsClimate Modelling, Predictions and Projections
Climate Modelling, Predictions and Projections
 
Climate Change
Climate ChangeClimate Change
Climate Change
 
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814
RISK p3-14 CLIMATE CHANGE ... Hansen et al predictions 2015 150814
 
Earthscope4D.pptx
Earthscope4D.pptxEarthscope4D.pptx
Earthscope4D.pptx
 
Environmental modelliing
Environmental modelliingEnvironmental modelliing
Environmental modelliing
 
Publication_Draft_09Aug
Publication_Draft_09AugPublication_Draft_09Aug
Publication_Draft_09Aug
 
AAS National Conference 2008: Robert Lin
AAS National Conference 2008: Robert LinAAS National Conference 2008: Robert Lin
AAS National Conference 2008: Robert Lin
 
Great Lakes Ice Forecasts and Climate Research
Great Lakes Ice Forecasts and Climate ResearchGreat Lakes Ice Forecasts and Climate Research
Great Lakes Ice Forecasts and Climate Research
 
Solar variability terrestrial climate
Solar variability terrestrial climateSolar variability terrestrial climate
Solar variability terrestrial climate
 
Climate Models
Climate ModelsClimate Models
Climate Models
 
Simone Fatichi
Simone FatichiSimone Fatichi
Simone Fatichi
 
Modeling Past and Future Climate
Modeling Past and Future ClimateModeling Past and Future Climate
Modeling Past and Future Climate
 
Climate and climate modelling
Climate and climate modellingClimate and climate modelling
Climate and climate modelling
 
9 precipitations - rainfall
9   precipitations - rainfall9   precipitations - rainfall
9 precipitations - rainfall
 
NY
NYNY
NY
 

Similar to Oceans Currents

Burntwood 2013 - Why climate models are the greatest feat of modern science, ...
Burntwood 2013 - Why climate models are the greatest feat of modern science, ...Burntwood 2013 - Why climate models are the greatest feat of modern science, ...
Burntwood 2013 - Why climate models are the greatest feat of modern science, ...IES / IAQM
 
Ch 1esnew
Ch 1esnewCh 1esnew
Ch 1esnewbasdsci
 
Butterfly Satellite Mission Overview
Butterfly Satellite Mission OverviewButterfly Satellite Mission Overview
Butterfly Satellite Mission OverviewChelle Gentemann
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2Sarah Ramanathan
 
Atmosphere science 7 quarter 4 .........
Atmosphere science 7 quarter 4 .........Atmosphere science 7 quarter 4 .........
Atmosphere science 7 quarter 4 .........LeaCamillePacle
 
EARTH SCIENCE LAYERS OF THE Atmosphere.ppt
EARTH SCIENCE LAYERS OF THE Atmosphere.pptEARTH SCIENCE LAYERS OF THE Atmosphere.ppt
EARTH SCIENCE LAYERS OF THE Atmosphere.pptAngelle Pantig
 
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docxrhetttrevannion
 
Long term & short term effects of climate
Long term & short term effects of climateLong term & short term effects of climate
Long term & short term effects of climateSarah Ramanathan
 
1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.pptgrssieee
 
1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.pptgrssieee
 
Greenhouse effect, GHG, Global warming and climate change.ppt.pptx
Greenhouse effect, GHG, Global warming and climate change.ppt.pptxGreenhouse effect, GHG, Global warming and climate change.ppt.pptx
Greenhouse effect, GHG, Global warming and climate change.ppt.pptxAnjalMahat
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2Sarah Ramanathan
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2Sarah Ramanathan
 

Similar to Oceans Currents (20)

Burntwood 2013 - Why climate models are the greatest feat of modern science, ...
Burntwood 2013 - Why climate models are the greatest feat of modern science, ...Burntwood 2013 - Why climate models are the greatest feat of modern science, ...
Burntwood 2013 - Why climate models are the greatest feat of modern science, ...
 
Ch 1esnew
Ch 1esnewCh 1esnew
Ch 1esnew
 
Butterfly Satellite Mission Overview
Butterfly Satellite Mission OverviewButterfly Satellite Mission Overview
Butterfly Satellite Mission Overview
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 
Atmosphere.ppt
Atmosphere.pptAtmosphere.ppt
Atmosphere.ppt
 
Atmosphere.ppt
Atmosphere.pptAtmosphere.ppt
Atmosphere.ppt
 
Atmosphere science 7 quarter 4 .........
Atmosphere science 7 quarter 4 .........Atmosphere science 7 quarter 4 .........
Atmosphere science 7 quarter 4 .........
 
EARTH SCIENCE LAYERS OF THE Atmosphere.ppt
EARTH SCIENCE LAYERS OF THE Atmosphere.pptEARTH SCIENCE LAYERS OF THE Atmosphere.ppt
EARTH SCIENCE LAYERS OF THE Atmosphere.ppt
 
Final Paper
Final PaperFinal Paper
Final Paper
 
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx
36127 Topic SCI 207 Our Dependence upon the EnvironmentNumber.docx
 
Climate
ClimateClimate
Climate
 
Moon formation processes
Moon formation processesMoon formation processes
Moon formation processes
 
Long term & short term effects of climate
Long term & short term effects of climateLong term & short term effects of climate
Long term & short term effects of climate
 
lectures2.ppt
lectures2.pptlectures2.ppt
lectures2.ppt
 
1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt
 
1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt1_Buck - Wavemil Steps IGARSS-11.ppt
1_Buck - Wavemil Steps IGARSS-11.ppt
 
Greenhouse effect, GHG, Global warming and climate change.ppt.pptx
Greenhouse effect, GHG, Global warming and climate change.ppt.pptxGreenhouse effect, GHG, Global warming and climate change.ppt.pptx
Greenhouse effect, GHG, Global warming and climate change.ppt.pptx
 
Climate
ClimateClimate
Climate
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 

Oceans Currents

  • 1. How Our Oceans Move and Why We Care... Benicat, Sabrina, Kijana, Bella Counselors: Maria and Aisha
  • 2. Intro: Mechanical Engineering Mechanical Engineering “Classical” engineering Quantum Mechanics Fluid Mechanics Computational Fluid Dynamics Study of classical engineering Studying Newton’s Law Physics- looks at particle movement Air, water; study of any gas/ liquids Solving equations of fluid mechanics on a computer Ocean Modeling
  • 3. Why do we need to understand how the Ocean Moves? weather climate natural disasters: ***we LOVE Earth*** hurricanes, tsunamis, tornadoes, earthquakes, volcanoes, sinkholes, droughts, heat, waves, wildfires, floods, blizzards, avalanches
  • 4. Ocean Circulation - Stratification - Rotation of the Earth - Wind - Continental Boundaries These factors cause -Small Scale Ocean Phenomena -Medium Scale Ocean Phenomena -Large Scale Ocean Phenomena
  • 5. Small Scale Phenomena - Micro-turbulence -Gravity -Tides
  • 7. Density & Stratification Density is a characteristic property of a substance Density = mass / volume rho = m / v
  • 8. Global Winds ∗ Coriolis Force ∗ Gulf Stream Westerlies: ∗ Lie between the Northern and Southern Hemisphere ∗ Blows from west to east along the equator ∗ Highly variable and unsteady winds ∗ Part of hurricanes, tsunamis, monsoons, etc. Frequent changes to the weather: ∗ Mid-latitude storms ∗ Wintertime changes Trade: ∗Travels from east to west ∗ Lie on both sides of the equator which: ∗ Gives out steady wind flow ∗ Ocean waves are very steady around these areas ∗ Sail and fishing boats depend on the airflow to get to nearby coastal areas safely
  • 9. Thermohaline Circulation -Large Scale Ocean Phenomena -Deep and shallow currents create the well known "Great Ocean Conveyor Belt" -Regulates our climate -The movement of large quantities of water allow for the transportation of nutrients and heat -It is the overall circulation of the ocean, if it shuts down everything would collapse
  • 10. The Experiment -Lab simulation of the differences in water temperature -The lab was conducted by placing ice packs on one end of the dish and placing a lamp on the on the other end. -The water had to stand for 20-30 minutes and then colored dye was added. -The warm water(red/equator) rose above the colder water(blue/North Pole)
  • 11. Western Boundary Currents Causes 1. Wind 2. Rotation of the earth 3. Continental boundaries Hypothesis The Western Boundaries Currents (WBCs) need all the three factors to develop the circulation pattern observed by satellites. Methods -Set up laboratory scale experiment that mimic Western Boundary Currents -Set up computational experiments that mimic Western Boundary Currents
  • 12. Lab Experiment Materials -Big plastic tank (continental boundaries) - Water (ocean) - Slope (spherical rotation) - Two little pillars - Fans (winds) - Red and blue dye - Turntable (rotation of earth) - Camera Procedure -Set up the two little pillars -Put in the slope -Fill the tank with water -Adjust the fans (North and South side of the box) SP=West ;NP=East (to mimic the winds) -Set up the camera -Begin the counterclockwise rotation of the tank, like the Earth -Let it spin for 20-30 minutes -When ready, add the red & blue dyes (red = southwest & blue = northeast ) Trials Trial A - All factors Trial B - No wind (no fans) Trial C - No spherical rotation (no slope) Trial D - No rotation of Earth (no rotation of tank)
  • 14. Computational Experiment :MATLAB The 5 Factors 1. Local Changes 2. Convection 3. Coriolis 4. Wind 5. Diffusion/ smoothing/ disappearing effect Trials Case 1 = All Terms Case 2 = No Convection Case 3 = No Coriolis Case 4 = No Wind Case 5 = No Diffusion Experiment - Using a coding program MATLAB we were able to view different simulations on the computer - Equations used in mechanical engineering are long and complex that they can easily be solved using a software such as MATLAB - The equation we plugged in was the Barotropic Vorticity Equation - Vorticity: a measure of how much the fluid spins - We were able to make videos of how the western boundary currents look from satellites Look at video
  • 15. Why do we care? -Melting of ice caps slows thermohaline circulation causing extreme climate change -The ocean’s temperature increase and sea level rise will cause severe hurricanes
  • 16. Thank You Professor Reckinger, REU Researchers, and Counselors