1 Deep Water Formation: Now vs Last Ice Age. 2 Model Predicted Air Temperature Change.

Slides:



Advertisements
Similar presentations
Atmospheric general circulations
Advertisements

Distribution of waters 71% of earth surface is ocean 4:1 in southern hemisphere 1.5:1 in northern hemisphere.
Removal of moisture and heat upwelling 1. Ocean Conveyor Belt.
Deep Ocean Circulation Motion in the Ocean, Part 2, “The Great Conveyor Belt” Jack Barth NASA web site:
The Oceans Nov. 18 Topics Thermohaline circulation –SST; –ocean water masses Wind-driven circulation –Wind-driven upwelling –Surface currents Mundus Subterraneus.
The East Greenland Current (EGC)
1 Surface Circulation Pathways Generally, warm currents move poleward and cool currents move equatorward.
Earth Systems Science Chapter 5 OCEAN CIRCULATION I: SURFACE Winds, surface currents Flow within gyres: convergence, divergence, upwelling, downwelling,
Deep Ocean Circulation
High Latitude Circulation
Thermohaline Circulation Carisa Sousa. Description Defining - terminology –Meridional Overturning Movement –“Overturning” - Pacific and Indian Oceans.
Deep Thermohaline currents
SIO 210 Typical distributions (2 lectures) Fall 2014
Ocean Circulation By: Samantha Hampton In Partnership With: Dr. Zafer Top.
Density Structure of the Ocean. Density Controls Controlled by: 1.) Temperature 2.) Salinity 3.) Pressure Density increases with increasing salinity Density.
Oceanography Ocean Currents
Surface Currents and Deep Currents
Chapter 9.
NADW AABW AAIW Itay Halevy
Antarctic Circumpolar Current
Ocean Currents and Climate. Do the Earth’s Oceans Affect Climate?
Ocean Current Sungwoo & Irving Grade 8G. What is Climate? Climate is the average weather usually taken over a 30-year time period for a particular region.
Topic 14 Density Driven Currents
CIRCULATION OF OCEANS.
Subsurface Currents The Oceans in Motion. Subsurface Currents 1.Mechanics 2.Deep water formation 3.The Importance of the Global Conveyer Belt.
Thermohaline Circulation
Section 1: Ocean Currents
ThermoHaline Circulation
Deep Water Circulation Also known as thermohaline circulation.
Class 27 DEEP CIRCULATION AND WATER MASSES Origin of Atlantic water masses/currentsOrigin of Atlantic water masses/currents –Bottom water –Deep water –Intermediate.
Oceanography Ocean Currents Chapter 24.1 and 24.2.
Deep Currents.
AGU, 2003 image:AGU 2003 How will the Northeast Atlantic and its living resources respond to global climate change? Nordic Seas Greenland Iceland Norway.
Regional Oceanography I
Thermohaline Circulation Lecture Outline 1)What is thermohaline circulation 2)History of understanding 3)Key water masses 4)Formation of deep water 5)Theory.
9.3- Energy transfer in air and water. Heat transfer Heat transfer = the movement of thermal energy from area of higher temp. to area of lower temp. Heat.
Water Mass Distribution OEAS 604 Lecture Outline 1)Thermohaline Circulation 2)Spreading pathways in ocean basins 3)T-S diagrams 4)Mixing on T-S diagrams.
OC3230-Paduan images Copyright © McGraw Hill Chap 7-8: Distributions SPECIAL DATES: MPA meeting…6 Jul R/V Pt Sur Cruise…14 Jul R/V Pt Sur Cruise…25 Jul.
Density Structure Surface Processes Temperature Salinity Pressure.
Ocean Currents.
Deep Ocean Circulation. Significant vertical movement ▫Accounts for the thorough mixing of deep- water masses.
Lesson 8: Currents Physical Oceanography
Music today: Little Mermaid, “Under the Sea” WELCOME OSU MOMS!!
The Conveyer Belt EEn  Ocean circulation travels from the Atlantic Ocean through the Indian & Pacific oceans & back again  Warm water in upper.
Osmosis (Revisited) Video. Density mass per volume of seawater Determined by temperature and salinity Density of seawater increases all the way to its.
Ocean Currents Oceans have a slower, much longer-lasting effect on climate than winds. Ocean currents are basically driven by the sun and the rotation.
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
Deep Ocean Circulation Motion in the Ocean, Part 2, or Who wants to ride the Great Conveyor Belt?
Ocean Circulation. The Layered Ocean The oceans have a well-mixed surface layer of approximately 100 meters(300 feet) Layers of increasing density from.
Temperature and vertical stratification Metabolism: Q10 Preference & tolerance Poikilothermic or ectothermic vs. homeothermic or endothermic Thermocline.
03 Thermohaline Circulation
Density-Driven Downwelling and Thermohaline Circulation
Climate and Ocean Currents
An overview of Climate Oscillations
Essentials of Oceanography
Music today: Little Mermaid, “Under the Sea” WELCOME OSU MOMS!!
Team Members: Veronica Colon, Samy Harmoush, Jose Ramos, Christy Yunn
Global Ocean Conveyor Belt
Circulation of the Oceans
Ocean Motion Vocabulary
1.
Ocean Circulation based on Density: Temperature and Salinity
Surface water circulation
Deep Circulation Changes in density cause ocean currents Cold Warm
OCEANS and CURRENTS.
Deep Ocean Circulation
Deep Ocean Currents.
Interactions between the Oceans and the Atmosphere
The Oceans in Motion Subsurface Currents.
Presentation transcript:

1 Deep Water Formation: Now vs Last Ice Age

2 Model Predicted Air Temperature Change

3 Models Predict a Future Slow Down of Deep Water Formation Rates in N. Atlantic

4 Potential Temperture and Salinity in Atlantic Ocean

5 Formation Regions of Deep and Intermediate Waters

6 Circulation in Region of Antarctic Bottom Water Formation Entrainment Sinking 55ºS 70ºS

7 Distribution of Intermediate Waters ( m)

8 Spread of Mediterranean Water in N. Atlantic (~1000m) Pot Temp Salinity

9 Temperature and Salinity in S. Atlantic (~40ºS)

10 T, S and σ for Deep and Intermediate Waters in Atlantic

11 Pot Temp vs Salinity in Atlantic Ocean Is this site in N. or S. Atlantic?

12 Temperature vs Salinity when there are only two Water Sources

13 Temperature vs Salinity for Three Water Sources

14 T vs S for Components of LNADW LSW= Labrador Sea Water GSW= Greenland Sea Water NSW= Norwegian Sea Water LNADW= Lower NADW Component (GSW) GSW LNADW NSW

15 Effects of Mixing on T and S

16 T vs S in N. Atlantic (~40ºN 30ºW)

17 Theoretical Circulation of the Deep Sea

18 Ocean’s Conveyor Belt Circulation Schematic