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the movement of the tide out to sea; “the tide was on the ebb”; “the ebb tide” |
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The incoming or rising tide; the period between low water and the succeeding high water |
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A measure of the turnover time for fresh water in an estuary. |
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What are Jamaica Bay Resources? |
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•Recreational resource •Wildlife preserve •Part of the Atlantic flyway •Rich in habitat •Important to fisheries |
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In the early day of Jamaica Bay what was the bay like? |
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*its was used for Rereaction -Rockaway Beach&fishing shanties *Processing -oil, fertilizer& fish wastse *Refuse disposal -Barren Island -Pennsylvania Ave. landfill -Fountain Ave. landfill -Edgemere landfill *Fertilizer production -dead hourses and other another |
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means low oxygen and is primarily a problem for estuaries and coastal waters. Hypoxic waters have dissolved oxygen concentrations of less than 2-3 ppm. Hypoxia can be caused by a variety of factors, including excess nutrients, primarily nitrogen and phosphorus, and waterbody stratification due to saline or temperature gradients |
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What about eutrophication? |
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promote algal growth. As dead algae decompose, oxygen is consumed in the process, resulting in low levels of oxygen in the water.” - Mississippi River Basin |
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What are the 2 species of sea grass in Jamaica Bay? |
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*Spartina alternaflora -Interior of bay *Phrapmites austraslis -Fringes of bay
**20% of bay is wetlands |
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*Altered circulation-induced stratification *Elimination of shellfish harvesting *Restrictions on swimming *Restrictions on recreation *Alteration to topography *Loss of wetwetlands *Loss of eel grass *Eutrophication *Alterations in drainage *Reduction of faunal diversity *Hardened shorelines *Dredged channels *Health advisories for striped bass, bluefish, American eel, blue crabs. |
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How do you study what you can not see? |
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*Submersibles *Remotely Operated Vehicles (ROVs) *Autonomous Benthic Explorer (ABE) *Satellite Altimetry *Tracks |
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-Manned submersibles capable of horizontal and vertical travel Alvin-Woods Hole Oceanographic Institute ~4,500 meters |
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Remotely Operated Vehicles (ROVs) |
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unmanned, piloted from onboard a ship ~6,000 meters |
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Autonomous Benthic Explorer (ABE) |
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unmanned, untethered vehicle ~6,000 meters |
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using satellites, can measure the height of this bulge |
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as these satellites pass over the Earth they are continuously recording data - data from4.5 years of GeoSat measurements have been coded and converted |
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Echo from within sediments |
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seismics or subbottoms reflection |
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What factors control development Coastlines? |
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-Geological Setting *provides exiting sufaces for processes to shape -Sea Level *moves position of the shoreline across the continental shelf -Waves *long-shore transport, shorelineline straightening -Tides *directs sediment onshore/offshore |
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What do geologists want to know about the ocean bottom? |
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-Depth -Sediments (composition, thickness, history) -Rocks below sediments (age, composition) -Processes controlling the above |
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- Echo sounding - Multibeam system - Satellite altimetry *Backscatter *Coring *Submersibles(but these can cover only only tiny area) |
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Sounds bounces off layers in sediment to show structure |
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Wegener identified several lines of evidence to support the idea that the continents had drifted |
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Evidence for continental drift |
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*Matching mountain ranges across oceans *Glacial ages and climate evidence *Distribution of fossils such as -Mesosaurus and Lystrosaurus |
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Why did people not believe Alfred Wegener and continental drift? |
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*Wegener did not provide a plausible mechanism to explain how the continents could have drifted apart *Most Earth scientists rejected continental drift because it was -Too far-fetched -Contrary to the laws of physics |
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1. Continents “_____” ______ than _____ crust as made of _______ rock |
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float, higher
Ocean, lighter |
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Ridge crest “_________” oceanic crust forming ________ _____ |
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splitting, mid-ocean ridge |
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3. When ocean crust meets continent, is forced under creating ______ and _________ |
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A passive margin is the transition between oceanic and continental crust which is not an active plate margin -Very stable setting |
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In plate tectonics, a convergent boundary also known as a destructive plate boundary (because of subduction) -Very unstable setting |
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Where are active and passive margins? |
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Passive margin- eastern North America
Active margin- western Central America -convergent margin |
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interaction of river discharge &coastal processes |
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What kinds of coasts are there? |
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Is the location of a coast fixed?
How do you shape the coast? |
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it depends on the volume of ocean basin (amount of water in the ocean)
-Shape depends on: uplift/subsidence, erosion, sediment transport |
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larger zone affected by processes occurring in this boundry includes-marshes, dunes, cliffs, sand bars troughs |
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point at which the ocean meets the land example: sandy beach |
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"young" coast dominated by terrestrial influences -Altered by erosion (non-wave), sediment deposition, volcanism, tectonics -Land erosion coasts are frequently formed when a river valley floods (drowned valleys) -Chesapeake Bay, Hudson River valley -Also get this with glacial fjords |
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older coasts significantly altered by wave & other ocean processes
-significantly altered by wave, current, & tidal action -a variety of features, the most common being a beach |
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Erosional coasts (4 points) |
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-Steep cliffs created as waves undercut rocks (caves, blow-holes, etc). *Harder rock more resistant to erosion. -Initially coasts are irregular but straighten with time -At times of low sea level, rivers may have cut valleys. As these flood during higher sea-level,can make harbors, fjords, estuaries *Formed by erosion. -Volcanism can create coasts, often with steep cliffs |
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a zone of loose particles (boulders, cobble, pebbles, gravel, sand, silt) that covers all or part of a shore. Particles are contantly moving. |
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vegetation, sea cliff, dune, seawall |
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where sediment movement onshore/offshore ceases (about 10 m below sea level at low tide) |
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Longshore drift consists of the transport of sediments (generally sand but may also consist of coarser sediments such as gravels) |
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Sediment being carried along shore settles out as water reaches end of barrier and slows |
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sand spit closes off a bay by attaching to headland adjacent to bay |
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4 Services Coasts Provide |
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1)Protection -storm protection (marshs, barrier islands) 2)Provisions -fish, shellfish, transportation (goods&waste) 3)Recreaction -boating, swimming, fishing etc. 4)Function Regulating -nutrient recycling, (O2 rich water) |
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Major Ions in Seawater (6) |
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1.Na+ 4.Ca+ 2.Cl- 5.K+ 3.SO4-2 6.Mg2+ |
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from Crest(A) to Crest (B) |
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the lowest point in a wave |
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the highest point in a wave |
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how many waves pass point A or point Beach second |
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the time required for wave crest at point A to reach point B |
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of an individual water molecule at water surface |
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graptivy=g depth=h Shallow Water Waves (speed) |
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distance the wind blows over a body of water that has a force effect |
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what is the freezeing point of... 1.Freshwater 2.Saltwater |
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What is CTD/Condtivity Temp Depth used for? |
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What are the 3 types of Detlas? |
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-River dominated deltas (Mississippi) -Wave dominated deltas (San Francisco) -Tide dominated deltas (Ganges) |
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List 3 ways to stop erosion |
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-gronies -sea wall -beach nutrishment |
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Conservative vs. Non-coservative |
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Conservative vs. Non-coservative CFCs Nutrients 3He Dissolved O2 |
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_______________________ | CaCO3 | || | || Dissolved | \ / | V |......................lysocline | |_______________Carbate Compensation Depth (No CaCO3)
Explain this... |
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Carbate Compensation Depth the Depth at which there would be no more CaCO3 (like a snow capped moutain) |
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Terrestrial vs Marine Environments (4points) |
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1. Seawater is much denser then air -organisms floats 2.Seawater strongly absorbs light -most of the light is gone below 100m 3.Gravity -because of bouyancy organisms do not have to invest as much energy 4.O2 can be limiting in marine environments |
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occur when the sun and moon are directly in line with the earth and their gravitational pulls reinforce |
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A tide that occurs when the difference between high and low tide is least; the lowest level of high tide. Neap tide comes twice a month, in the first and third quarters of the moon. |
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A tide in which there is only one high water and one low water each lunar day |
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A tide having two high waters and two low waters during a tidal day. |
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amount of element in the ocean / rate at which the element is added to or removed from the ocean |
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closest to long island = North America |
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The upper layer of a body of water receiving light and thus where photosynthesis is possible |
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Malthus -famine -war -disease |
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- varies as a function of latitude - deflectionis to the light in northern hemisphere |
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- 45* angle - wind force - friction - upwelling/downwelling |
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A form of motion found in the near-surface layer of lakes and oceans under windy |
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norwegean/oceanographer/peace prize |
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-Mixing -photosynthesis -Adection |
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1. Fringing Reef 2. Barrier Reef 3. Atolls |
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