Introduction to Ocean Circulation - Geography 163 Wind-driven circulation of major gyres & surface currents Buoyancy-driven circulation linking the major.

Slides:



Advertisements
Similar presentations
Chapter 10. Atmosphere Ocean Interactions Global Winds and Surface Ocean Currents Ocean surface dragged by wind, basins react to high pressure circulation.
Advertisements

Unit 10: Circulation of the World Ocean
Ocean Currents.
Essentials of Oceanography
Ocean Currents
Chapter 7 Ocean Circulation
Ocean Currents
© 2011 Pearson Education, Inc. CHAPTER 7 Ocean Circulation.
Summary from last class… Importance of large-scale ocean circulation –climate, biogeochemistry, marine resources Characteristic “Types” of Ocean Circulation.
Review - Precipitation is caused by the uplift of moist air Air rising along the ITCZ or weather fronts (convergence) Convection caused by intense surface.
Introduction to Ocean Circulation - Geography 163 Wind-driven circulation of major gyres & surface currents Buoyancy-driven circulation linking the major.
The Global Heat Budget Air-sea exchanges of heat (& freshwater) create deep water masses & drive the conveyor belt Heat source into the ocean is solar.
Introduction to Ocean Circulation - Geography 163 Wind-driven circulation of major gyres & surface currents Buoyancy-driven circulation linking the major.
Major currents, gyres, rings, and eddies (basin scale) Winds and wind-driven basin circulation Meanders, rings, eddies and gyres The thermohaline circulation.
Oceanic Circulation Current = a moving mass of water.
Oceans. Vertical ocean temperature profile Plimsoll line.
A Voyage of Discovery Physical oceanography Instructor: Dr. Cheng-Chien LiuCheng-Chien Liu Department of Earth Sciences National Cheng Kung University.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Ocean Currents. Why is Ocean Circulation Important? Transport heat Equator to poles Transport nutrients and organisms Influences weather and climate Influences.
Highways in the Sea (Chapter 9)
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
More Climatic Interactions
© Oxford University Press, All rights reserved. 1 Chapter 6 CHAPTER 6 OCEAN–ATMOSPHERE INTERACTIONS.
6th Grade Earth Science Sutton Middle School
Ocean Currents.
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
Ocean Currents.
DO NOW From what you learned and observed in the density investigation, hypothesize what you think happens in the red areas on the map shown, and why you.
Ocean Circulation Currents. Horizontally Vertically.
CHAPTER 7 Ocean Circulation
Ocean Currents. A penguin walks into a bar and asks the pharmacist for Chapstick. After grabbing the Chapstick, the pharmacist asks the penguin, “How.
Surface Currents Movement of water that flow in the upper part of the ocean’s surface.
Ocean Currents Are masses of ocean water that flow from one place to another. Water masses in motion Surface Currents - wind driven currents move water.
Ocean Circulation.
Ocean Circulation Recall from last lecture that differential heating of the earth, along with the effects of the rotation of the globe cause generally.
Water’s Three States of Matter
Current Weather Introduction to Air-Sea interactions Ekman Transport Sub-tropical and sub-polar gyres Upwelling and downwelling Return Exam I For Next.
Ocean Circulation – Ch Ag Earth Science – Chapter 15.2.
Ocean Currents Please take a copy of the blank ocean currents worksheet on the counter, have a seat, then get out something to take notes on (the back.
Deep Ocean Circulation. Significant vertical movement ▫Accounts for the thorough mixing of deep- water masses.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Lesson 8: Currents Physical Oceanography
What forces cause the ocean to move? Gravitational pull of the Moon and Sun Wind (friction between air and water) Coriolis Effect (spin of Earth) Differences.
Ocean Currents trash islands.
Ocean Response to Global Warming/Global Change William Curry Woods Hole Oceanographic Institution Environmental Defense May 12, 2005 Possible changes in.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
Ocean Current s.  Warm currents flow away from the equator.  Cold currents flow toward the equator. Ocean Currents.
Motion of the Ocean Ch. 9 – Currents. Ocean Currents The steady flow of water in a prevailing direction Basically, an area where most of the water is.
Measuring Deep Currents
Ocean Currents. Mass movement or flow of ocean water Mass movement or flow of ocean water River within the ocean River within the ocean Two types Two.
Ocean Currents Ocean water circulates in currents caused by wind and by density differences Currents are the flow of water between areas of different surface.
Ocean Circulation.
16.1 – Ocean Circulation.
Differential Heating – Specific Heat
Chapter 16.1 Ocean Circulation.
Ocean Circulation 16.1.
Currents and Climate.
Oceanic Influences on Climate
Ocean Currents.
OCEAN CURRENTS.
June 2011 Ocean Currents Ocean water circulates in __________ caused by _____ and by _________ differences Currents are the _____ of __________between.
Ocean Currents: 4 causes
Circulation of the Oceans
Ocean Currents.
Currents and Climate.
Ocean Circulation Currents and Causes.
Ocean Currents.
Currents and Climate.
Convection The transfer of thermal energy by the movement of particles within matter.
Presentation transcript:

Introduction to Ocean Circulation - Geography 163 Wind-driven circulation of major gyres & surface currents Buoyancy-driven circulation linking the major gyres & the global conveyor belt Coastal circulations & land-ocean interactions Build from physical principles (w/out math)

Approach First principles do “work” Build descriptions from first principles Do not bludgeon students with calculus Work with available data sets

Why do we care? Climate –Global heat & water cycles –Weather & weather/climate prediction Global biogeography & biogeochemistry –Species ranges & adaptation to global change –Fossil fuel CO 2 sequestration Marine resources –Renewable (fisheries) –Non-renewable (oil, etc.)

Global Heat Transport How can it be constant?

Global Heat Transport

10 15 W = 1 Petawatt

El Niño

Bigeography

Bigeographical Boundaries

Bigeography

CO 2 Sequestration It’s gotta go somewhere...

CO 2 Sequestration This is where.

Climate & Fish Pacific Decadal Oscillation Warm phase - southern Cool phase - northern We’re now in a cool phase…

Introduction to Ocean Circulation - Geography 163 Wind-driven circulation of major gyres & surface currents Buoyancy-driven circulation linking the major gyres & the global conveyor belt Coastal circulations & land-ocean interactions

Wind-Driven Gyres

Global Ocean Circulation

Global Wind Climate

Conveyor Belt

Net Air-Sea Heat Flux

Coastal Upwelling

July 1992 AVHRR Ch 4

Scales Ocean basins are wide & shallow –Typical scales are 10 4 km across and 5 km deep –“Spit on a basketball” Aspect ratio has important implications –Horizontal velocities are >> vertical velocities –Horizontal property changes are << vertical ones

Hyposgraphic Curve

Atlantic Temperature eWOCE gallery –

Atlantic Salinity

Atlantic Oxygen

Atlantic Phosphate

Summary Importance of large-scale ocean circulation –climate, biogeochemistry, marine resources Characteristic “Types” of Ocean Circulation –Patterns of circulation can be generalized for different regions –Suggests that dynamical processes are the same –Wind-driven, Buoyancy-driven & Coastal Scales - “spit on a basketball”