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7. Oceanography of an Estuary
Salt Wedge-Draw this in your notes:
Salt Wedge-Description
• Low density FW overrides high density SW
• Can extend far upstream
• Impacted by tides
  – Flood (incoming) – wedge is further upstream
  – Ebb (outgoing) – wedge is less far upstream
  – Because of it, organisms here must deal with
    major salinity fluctuations
Substrate (bottom sediments)
• Rivers:
   – Current is too fast to let sediment drop out
   – Lots of suspended (floating) material
• Estuaries:
   – Wider sides, area where water flows opens up (gets
     wider) so water is slowed down
   – Once flow slows suspended sediments drop out
   – Result: estuaries are usually muddy
• Closer to Oceans:
   – Currents are stronger
   – Smaller particles are washed away leaving larger
     sediments behind
Read:
http://oceanservice.noaa.gov/educati
on/kits/estuaries/media/supp_estuar0
            5a_wedge.html


                    View:
 http://www.youtube.com/watch?v=eeeIgDs4SdY
                     And
http://www.youtube.com/watch?v=4UyocM9bDL4

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7. oceanography of an estuary

  • 1. 7. Oceanography of an Estuary
  • 2. Salt Wedge-Draw this in your notes:
  • 3. Salt Wedge-Description • Low density FW overrides high density SW • Can extend far upstream • Impacted by tides – Flood (incoming) – wedge is further upstream – Ebb (outgoing) – wedge is less far upstream – Because of it, organisms here must deal with major salinity fluctuations
  • 4. Substrate (bottom sediments) • Rivers: – Current is too fast to let sediment drop out – Lots of suspended (floating) material • Estuaries: – Wider sides, area where water flows opens up (gets wider) so water is slowed down – Once flow slows suspended sediments drop out – Result: estuaries are usually muddy • Closer to Oceans: – Currents are stronger – Smaller particles are washed away leaving larger sediments behind
  • 5. Read: http://oceanservice.noaa.gov/educati on/kits/estuaries/media/supp_estuar0 5a_wedge.html View: http://www.youtube.com/watch?v=eeeIgDs4SdY And http://www.youtube.com/watch?v=4UyocM9bDL4