water mass distribution oeas 604 lecture outline 1)thermohaline circulation 2)spreading pathways in...
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Water Mass DistributionOEAS 604
Lecture Outline
1) Thermohaline Circulation2) Spreading pathways in ocean basins3) T-S diagrams4) Mixing on T-S diagrams
Chapter 9 – KnaussChapter 14 – Talley et al.
Thermohaline Circulation
• Circulation below the wind-driven currents • Flow is determined by density distribution
which is from temperature and salinity • Circulation forced by sinking of cold dense
water at high latitudes • Return flow in upper water column• Referred to a Meridional Overturning
Circulation (MOC)
Water Masses
• Form in certain regions of the ocean
• Advected by ocean currents
• Form frontal regions were meet
• Water mass – a body of water with a common formation history, having its origin in a particular region of the ocean
• Source region – finite volume of ocean where water mass formation takes place
Water Mass Analysis
• Water type - point in n-dimensional parameter space – it is a combination of temperature, salinity, nutrients, oxygen and other tracer values
• Water mass – water formed in certain regions with particular temperature, salinity and other properties
Mixing of water masses
Two-point mixing• Determine the mixture along line between
two source waters • f = fraction of water mass 1, f=1 all from
water mass 1, f = 0 none from water mass 1
• Tmix = fT1 + (1-f)T2
• Smix = fS1 + (1-f)S2
• Know Tmix, Smix, T1, T2, S1, S, so solve for f
Track water masses
Core method
Gives rates ofmixing andtransport direction
Atlantic
Indian
Pacific
T-S distribution for world oceans
North Atlantic and Southern Ocean
NA – open to north, high latitude, limited seasonal sea ice, freshwater sources SO – bounded by continent, seasonal sea ice, no rivers, large polynyas
Atlantic separatedInto basins with littleconnections
Indian Ocean
Blocked to north
Limited connectionto Southern Ocean
Complex bathymetryand limited openingsto the east
Pacific Ocean
Western basinDeeper
Opening to northconstricted byBering Strait
North Atlantic Deep WaterGreenland Sea WaterLabrador Sea WaterMediterranean Sea Water
High salinity, low temp, high oxygen
Antarctic Intermediate WaterLow salinity, high oxygen
Antarctic Bottom WaterHigh salinity, low temperature,average oxygen
Subtropical UnderwaterLow oxygen
Antarctic Bottom WaterPathways
Different varieties along western and eastern sides of basin
Limited across basinexchange
Flow on eastern side blocked by Walvis Ridge
AAIW
NADW
AABW
East-west sectionin South Atlantic
T-S diagrams in East and West Atlantic – NADW, AAIWNorth Atlantic and South Atlantic Central WatersHigh salinity Mediterranean Sea Water
West East
Annual progression of sea ice concentration in 1991, computed from the Special Sensor Microwave Imager (SSM/I) carried on the Defense Meteorological Satellite Program satellites.
Antarctic CircumpolarCurrent
High speedcurrent cores
SubantarcticFront
Polar Front
Southern ACCFront
SubtropicalFront
Track of the Endurance (1914-1916) (from Stone 1914)
Bottom water formation
Spreading and direction of AABW
Intermediate and mode waters form along northern side of Polar and Subantarctic fronts
T-S diagram from Southern Ocean
AASW – Antarctic Surface Water
WW – Winter Water
SSW – Shelf Water
HSSW – High Salinity Shelf Water
ISW – Ice Shelf Water
WS and RS – Bottom WaterCDW - Circumpolar Deep Water
T-S properties ofwater masschange around the Southern Ocean
CDW – cools and freshens
Spreading ofBottom water
Limited exchange
90°E Ridge is abarrier
T-S diagram for Indian OceanAAMW – Australian Mediterranean Water
Spreading ofbottom waterin Pacific Ocean
North-southsection in westernPacific
T-S diagramfrom westernPacific
Next Class
• Ekman Dynamics
• Upwelling
• Chapter 7, Knauss
• Chapter 7, Talley et al.