Presentation on theme: "Atlantic Ocean Maury Project 2013 CAPT Bill Schulz US Naval Academy"— Presentation transcript:
1 Atlantic Ocean Maury Project 2013 CAPT Bill Schulz US Naval Academy email@example.com
2 Atlantic Ocean Facts The most studied ocean Second-largest of the world’s oceansBorn: about 170,000,000 B.C.Area: ~77 million km2 (~ 6.5 times the area of U.S.)Average depth: 3575 meters (11,072 ft)Volume: 337,000,000 km3 ( 8.9x1019gallons)Average surface salinity: pptHigher than Pacific due to greater evaporationStill growing
3 Atlantic Ocean Basin Mid-Atlantic Ridge Atlantic is in Stage III of Ocean Basin Evolution:A MATURE basinSpreading ~3 cm/yearUSGS - Understanding Plate MotionsMid-Atlantic RidgeStage III
4 Stages of Ocean Basin Evolution I – embryonic (crustal extension, rift; East Africa)II – young (subsidence, spreading; Red Sea)III – mature (spreading; Atlantic)IV – declining (spreading and shrinking; Pacific)V – terminal (shrinking, uplift; Mediterranean)VI – relict scar (Indus Suture)
5 Atlantic Ocean Basin Large ridge/rise system - ~ 70,000 km long Not nearly as seismically active as the PacificYoungest crust down the center, rising and forming the Mid-Atlantic RidgeAge of Oceanic Crust – Millions of Years Before Present
6 Major Surface Currents in the Atlantic UCAR's Windows to the Universe Ocean currents tutorial from RSMASTomczak & Godfrey Regional Oceanography text
8 Motion due to the wind (and Coriolis) affects the vertical structure of the water column (and therefore, temperature, biology, sound, etc….)WesternBoundaryCurrentEasternBoundaryCurrentMost of the poleward transport of warm waters occur along the western boundaries and the sinking of dense surface waters occur in relatively small regions. The upwelling of water occurs basin-wide and is most pronounced in regions with divergent Ekman transport.
9 Atlantic Thermohaline Circulation General Concept (National Climatic Data Center) – Sun’s heat absorbed in tropical ocean carried to the North AtlanticOceanic conveyor belt - the large-scale 3-D flow pattern that results from the sinking of water in the Nordic and Greenland Seas and around Antarctica.
10 Modified from figure courtesy of Dr Modified from figure courtesy of Dr. Steve Hovan, Indiana University of Pennsylvania.
11 Density Distribution Temperature (oC) AABW – Antarctic Bottom Water AAIW – Antarctic Intermediate WaterNADW – North Atlantic Deep WaterUPPER – North Central Atlantic WaterDensity DistributionTemperature (oC)Salinity (PSU)
13 ATLANTIC WATER MASS INPUT: Salt (Mediterranean Sea)Fresh Water (Amazon and Congo Rivers)Sediment (St. Lawrence, Niger, Rhine Rivers)Heat (Caribbean Sea and Gulf of Mexico)Bottom Water (Arctic and Antarctic Seas)
14 Mediterranean Outflow Large evaporation in the Med.Produces dense/salty water, which then sinks. (Levantine Intermediate Water + Mediterranean Deep Water )Water spills over the sill at Gibraltar, As the plume of MOW exits Gibraltar, it moves to the north, then spreads west and southMOW mixes with and settles with the North Atlantic Deep water, and spreads out one thousand km across the basin.
15 (from Tomczak and Godfrey) Temperature at 1000 m depth(from Tomczak and Godfrey)The Mediterranean Sea is connected to the North Atlantic through the narrow Strait of Gibraltar. Flow is into the Mediterranean at the sea surface in the Strait. Within the Mediterranean there is large evaporation and cooling and production of dense water. High salinity water, formed by evaporation in the Meditterean Sea, spills over the sill at Gibraltar, mixes with North Atlantic water, and spreads out one thousand km across the basin. When water is sufficiently cooled, at polar latitudes, by cold atmospheric air, it gets denser and sinks. The vertical sinking motion causes horizontal water motion as surface waters replace the sinking water. This is one example of thermohaline flow. This flows out into the North Atlantic at the bottom of the Strait. The resulting Mediterranean Water (or Mediterranean Outflow or Overflow Water) in the North Atlantic is found at mid-depth and is marked by its salinity maximum both in the vertical and in the horizontal along isopycnals. Vigorous entrainment as it moves down the slope reduces its high salinity and density. It finally equilibrates after mixing at a depth of about 1000 m.
16 The Gulf Stream Current on the western boundary of the Atlantic Ocean Western boundary currents are much narrower and faster than eastern boundary currentsWestern boundary currents move significant amounts of warm waters northward and are important in transporting excess heat from the tropics towards the poles.Eddies form along the meandering Gulf Stream
18 Views of the Gulf Stream “There is a river in the ocean. In the severest droughts it never fails, and in the mightiest floods it never overflows; its banks and its bottom are of cold water, while its current is of warm; the Gulf of Mexico is its fountain, and its mouth is the Arctic Sea. It is the Gulf Stream. There is in the world no other such majestic flow of waters.” - Matthew Fontaine Maury 1855U.S. Coast andGeodetic Survey1860Franklin-Folger 1770NOAA AVHRR 19961770 – Benjamin Franklin had Mount & Page's in London engrave the above chart featuring the Gulf Stream. Copies were sent to the captains of the mail packets at Falmouth, who promptly disregarded it. Franklin also had copies printed in Paris. Since then, it has become the most famous early depiction of the current.1860 – U.S. Coast and Geodetic Survey published this chart based on data gathered by Ben Franklin’s Great-grandson, LT George Bache. LT Bache was engaged in Gulf Stream surveys in 1864, when he was caught in a hurricane off of Cape Hatteras. Bache and many of his shipmates were killed in the storm.1996 – Infrared imagery of Atlantic Ocean sea surface temperatures obtained via AVHRR on NOAA 12 and 14. Image processed by Johns Hopkins Applied Physics Lab.
19 The Loop Current 20 April 2010 Deep Water Horizon NOAA Oil Spill Map Naval Research Lab Gulf of Mexico Currents(Global NRL Layered Ocean Model – NLOM)
20 Air-Ocean Interaction and The Atlantic Ocean Hurricanes2013 expected to be slightly above average (Gray, Colorado State, 2013)18 named storms (avg=12), 9 hurricanes (avg=6.5 avg), 4 major (avg = 2)Atlantic role in Extra-Tropical Cyclones
21 Atlantic HurricanesWarm ocean water (> 78.8 F;26 C) is a main ingredient for formation of HurricanesNASA Earth Observatory - Hurricane TutorialClimatologyNational Hurricane CenterStorm surge (wind piling up water) is biggest damager COMET storm surge tutorialSatellite ImageryOf Past Hurricanes Archive Imagery from CIMSSOf Current Ocean Basins NRL Satellite Homepage, NRL Tropical Cyclone Page
25 Hurricane IsabelSep 2003Extensive flood damage along Chesapeake Bay coastline due to storm surgeUSNA FloodedStorm surges of 3-5 ft above normal tide levels were observed over the central portions of the Chesapeake Bay and 5-6 ft over the southern portion of the Bay in the vicinity of Hampton Roads, Virginia. Surge values of 6-8 ft above normal levels were observed in the upper reaches of the Chesapeake Bay near Annapolis and Baltimore, Maryland and in most of the main stem rivers draining into the Chesapeake Bay. Even higher surges occurred at the heads of the rivers, with values of 8.5 ft above normal levels at the Richmond City locks along the James River in Virginia and nearly 8 ft along the Potomac River in Washington, D.C. Water levels exceeded previous record levels established in the Chesapeake-Potomac Hurricane of 1933 in Washington, D.C., Baltimore and Annapolis.
26 Powerful storm surge and winds from Hurricane Katrina (Aug 2005) rip two floating casinos in Biloxi, MS from their moorings, relocating them across a highway.Other significant damage to structures, landscape and vegetation are also observed.Casino 2Casino 1Biloxi, MS 13 Nov 2001Casino 1Casino 2From: Spaceimaging.comBiloxi, MS 2 Sept 2005
27 Radar Imagery of Landfall of Hurricane Dennis (July 2005) NWS National and Regional Radar Composites
28 Impact of ENSO on ATL Hurricane Season? El Niño (warm equatorial Pacific) leads to fewer ATLANTIC cyclonesLa Niña (cooler equatorial Pacific)favors ATLANTIC cyclone developmentCurrently (26 June 2012) largely neutral, 50% chance of El Niño conditions developing in later half of 2012.ENSO module later in the Project, in the meantime:Climate Prediction Center - ENSO DiscussionNWS JetStream - Weather Impacts of ENSO
29 Winter – Nor’eastersStorms Develop in Southeast and move up the Atlantic coastlineLarge moisture contentPotential for large snowfall amounts from Mid-Atlantic to Northeast U.S.Movement over the Gulf Stream intensifies storm – source of heat/moistureGale/Hurricane force winds and coastal flooding along NE Seaboard
30 History Makers Nor’Easters – Storm of the Century Extra-Tropical / Tropical Storm Interaction - The Perfect Storm
34 Additional On-Line Education Resources Oceans activities from Education WorldCelebrate the Year of the OceanA "Sea" of Resources on the Internet!Tutorials on HurricanesWW2010 Tutorial - HurricanesNASA Earth Science for Kids - "Tropical Twisters"Community Learning Network (CLN) - Hurricane learning and activity resources list
35 On-Line Education Resources, Cont’d Consortium on Oceanographic Activities for Students and Teachers (COAST) - Resource GuideJPL - Resources for OC / MET and Remote Sensing of the OCN/ATMSmithsonian Museum of Natural History – Ocean ExhibitsSmithsonian Ocean Planet - outdatedSmithsonian - Sant Ocean HallList of Oceanography resources from NCSUNWS Tutorial - Thunderstorm Tornado Development