1 / 48

Oceanography

Oceanography. http://antwrp.gsfc.nasa.gov/apod/image/earth_1_apollo17_big.gif. The Oceans. Ocean Facts: Covers 71% of the earth’s surface Accounts for 97% of the water on earth (rest in land ice, groundwater, lakes & rivers) Average depth ~ 4,000 meters Average temp ~ 4 o C (only 39 o F)

jason
Download Presentation

Oceanography

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Oceanography http://antwrp.gsfc.nasa.gov/apod/image/earth_1_apollo17_big.gif

  2. The Oceans Ocean Facts: • Covers 71% of the earth’s surface • Accounts for 97% of the water on earth (rest in land ice, groundwater, lakes & rivers) • Average depth ~ 4,000 meters • Average temp ~ 4oC (only 39oF) • Average salinity ~ 35‰ = 3.5% (1 meter = 3.3 feet)

  3. The Oceans

  4. Ocean Zones coastal oceanic • Horizontal divisions: • Coastal (neritic) = on/over shelf (shallow) • Oceanic = beyond continental shelf (deep) benthic shelf benthic abyss

  5. Ocean Zones coastal oceanic • Vertical divisions: • Pelagic = open water • Epipelagic (0-200m) • Mesopelagic (200-1000m) • Bathypelagic+ (1000m+) • Benthic = ocean bottom benthic shelf benthic abyss

  6. Continental Margins Continental shelf • As narrow as <1 km (0.6 mi) at active margins (tectonic activity) • As wide as >750 km (470 mi) at passive margins (in middle of plates) • Shallow, typically <200 m (600 ft) • Only 8% of ocean surface, but biologically richest part of ocean

  7. Continental Shelf • Intertidal zone (between high and low tides) – open, exposed • Sandy shores (Atlantic – Cape Cod and south) • Rocky shores (most Pacific, Atlantic – north of Cape Cod)

  8. Continental Shelf • Intertidal zone (between high and low tides) – protected, muddy • Salt marshes (temperate) • Mangrove forests (tropical)

  9. Tides • Tides are affected by both the moon and the sun • Tidal day = 24 hours, 50 minutes

  10. Tides

  11. Continental Shelf • Estuaries - any semi-enclosed coastal area where freshwater and seawater meet and mix

  12. Long Island Sound http://www.epa.gov/region01/eco/lis/facts.html

  13. South Shore Bays http://www.estuary.cog.ny.us/index.html

  14. Peconic Bay http://www.epa.gov/owow/estuaries/programs/studies/pb.gif http://www.peconicestuary.org/CCMP_PDF/Chpt4.habitat.pdf

  15. Continental Shelf • Subtidal zone (always underwater) • Soft-bottom (sand, mud) • Unvegetated • Seagrass beds NOAA

  16. Continental Shelf • Subtidal zone (always underwater) • Hard-bottom • Seaweed, kelp forests • Coral reefs

  17. Continental Margins http://oceanexplorer.noaa.gov/explorations/02hudson/background/mapping/mapping.html http://soundwaves.usgs.gov/2005/01/research.html

  18. Deep-Ocean Basins Deep sea floor features: • Averages ~4000m (13,000 ft, 2.5 mi) http://oceanworld.tamu.edu/resources/ocng_textbook/chapter03/Images/Fig3-6.jpg

  19. Deep Ocean Bottom • Soft bottom (most common): • Abyssal plains • Silt, clay, biogenic oozes (forams, diatoms, radiolarians) http://earthobservatory.nasa.gov/Study/Paleoclimatology_SedimentCores/Images/ocean_detritus.jpg http://www.deepseascape.org/index.php

  20. Deep Ocean Bottom • Hard bottom: • Seamounts • Ridges • Deep coral reefs NOAA http://www.savethehighseas.org/photo_gallery.cfm?Cat=1

  21. Hydrothermal Vents

  22. Hydrothermal Vents • High temperature • High chemical concentrations • High acidity http://www.dfo-mpo.gc.ca/communic/endeavour/photo_e.htm

  23. Hydrothermal Vents • Chemosynthesis – energy from chemicals, not the sun • Chemosynthetic bacteria, archaea: • Outside on rocks • Inside some animals (tube worms, mussels, clams) • An oasis of warmth and food for other animals http://www.teara.govt.nz/NR/rdonlyres/E84896E2-2F7E-4D2A-9D46-366B50558303/87497/p5365dop.jpg http://oregonstate.edu/dept/ncs/photos/grazers.jpg

  24. Cold Seeps • Brine pools: • Gulf of Mexico was shallow sea that dried up in Jurassic period • Thick layer of salts covered with sediment when seawater returned • Salt seeps up through cracks in sediment NOAA

  25. Cold Seeps • Brine pools: • Underwater lakes of super salty water • Methane gases also seep out depth 700 m NOAA

  26. Cold Seeps • Chemosynthetic bacteria in mussels • An oasis of food NOAA http://dx.doi.org/10.1371/journal.pbio.0030102

  27. Water • Water is unique and critical for life • Viscous, thick medium • Slow to heat up & cool down, regulates climate • Exists in 3 states on earth • Maximum density at 4°C, not 0°C (ice floats, insulates) • Universal solvent

  28. Seawater • Seawater is a complex solution of dissolved ions and other dissolved solids and gasses

  29. Salinity • Salinity = the total amount of dissolved salts in water • Average amount = 35 g salt/1000 g seawater = 3.5% = 35‰ (parts per thousand) • Can be 0‰ at river mouths and >40‰ in parts of Red Sea

  30. Salts in Seawater major minor

  31. Temperature Gulf Stream Sargasso Sea California Current

  32. Density • The density of water is a function of its temperature and salinity • Density increases with lower temperature (until 4°C) ← Cold water (max. 1000 at 4°C) ← Warm water (958 at 100°C) ← Solid ice (917 at 0°C) ← Water vapor (1.2) http://upload.wikimedia.org/wikipedia/commons/thumb/8/8a/Density_of_ice_and_water_%28en%29.svg/573px-Density_of_ice_and_water_%28en%29.svg.png

  33. Density • The density of water is a function of its temperature and salinity • Density increases with higher salinity • Cold salty water is the densest of all ← Salty water (1027) ← Fresh water (1000) http://www.marietta.edu/~biol/biomes/physsal.gif

  34. Density, Temperature, and Salinity • 3 stratified layers according to density: • Surface mixed layer (epipelagic) • Mixed by wind and waves • Warmer and less dense • Up to 200m deep • Intermediate transition layer (mesopelagic) • Deep stable layer (bathypelagic & beyond) • Colder and denser • Below 1000m

  35. Density, Temperature, and Salinity 200 - pycnocline halocline

  36. Density, Temperature, and Salinity

  37. Dissolved Gasses • Most gases easily dissolve in seawater, but ocean proportions differ greatly from atmospheric proportions • Carbon dioxide is very soluble (0.039% of atmosphere, 15% of gases in ocean) • Oxygen is not very soluble (much less than in atmosphere) • Unlike solids, gases dissolve better in cold water, so all gas concentrations are higher in the polar waters than the tropics

  38. Dissolved Gasses Highest at surface – mixing with air Oxygen minimum zone - decomposition of organic matter High at bottom – deep water formed at surface

  39. Dissolved Gasses • Hypoxia = low oxygen (<3 mg/l) • Anoxia = no oxygen • Stressful or deadly for marine life http://www.gulfhypoxia.net/overview/images/image005.png http://longislandsoundstudy.net/wp-content/uploads/2010/08/Hypoxia.jpg

  40. Dissolved Gasses • Hypoxia in Long Island Sound every summer http://longislandsoundstudy.net/wp-content/uploads/2010/07/freq-of-hypoxia-2011.jpg

  41. Increased CO2 in air → more in the ocean Increase in H+ ions makes water more acidic, pH 8.2→8.1, expected 7.6-7.8 by 2100 Dissolved Gasses http://theotherco2problem.files.wordpress.com/2009/11/ocean-chemistry.gif

  42. Dissolved Gasses • “Ocean acidification” • Bad for organisms with calcium carbonate shells http://s.ngm.com/2007/11/marine-micro/img/ftr-hdr-acid.jpg http://www.ucar.edu/communications/Final_acidification.pdf

  43. Dissolved Gasses http://3.bp.blogspot.com/-9MpFK0zekqo/T-s8Mzm9qjI/AAAAAAAAB-c/5zsexadUp8A/s1600/oceanacidification.jpg

  44. NOAA Light in the Ocean • Most sunlight does not penetrate very far into the ocean • transparency depends upon suspended matter • deeper in tropics, less in coastal • Blocked by scattering and absorption • Different colors penetrate to different depths

  45. Light in the Ocean

  46. Light in the Ocean Epipelagic = photic zone (bright light, all plants/algae) Mesopelagic = twilight zone (little light, no plants/algae) Bathypelagic = aphotic zone (no light, no plants/algae)

  47. Pressure in the Ocean • Water is heavier than air • Pressure increases with increasing water depth • Sea level = 1 atm. of pressure • In ocean, each 10m of depth (33ft) you add another atm. of pressure

  48. Pressure in the Ocean Before and after travelling to 2000 ft http://www.naturalsciences.org/education/deepsea/images/cups_before_after.jpg

More Related