Geol 107 Oceanography USC – Flashcards

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who 'invented' oceanography?
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The Egyptians and Mesopotamian cultures were the first to invent oceanography Accumulation of knowledge at the Library of Alexandria, Egypt.
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Eratosthenes
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Determined the circumference of the Earth using geometry (ca 230BC), put it at 40,000km
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Magellan
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First to circumnavigate the world, died before the end
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James Cook
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Voyages of sci. discovery. Outline of Pacific ocean, discovered new zealand, Australia, hawaiian islands. Made the first accurate maps of the ocean using the chronometer to determine longitude. First one with access to accurate sea clock.
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Ben Franklin
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Discovered the golf stream.
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The challenger
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modern expedition that found depths of the ocean, and how deep life could live
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Formation of Earth
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It formed from the accumulation of dust and gases in space, called a nebulae, differentiation occurred.
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Core
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made up of iron and nickel. Extremely hot
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outer core
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dense viscous liquid
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inner core
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solid dense rock, more dense than granite
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mantle
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mainly oxygen, silicon, iron, magnesium. Layer beneath the crust.
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mantle: lithosphere
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uppermost cool and rigid portion of the mantle, strong
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mantle: athenosphere
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below the lithosphere, hot partially melted, weak
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inner/lower mantle:
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hotter than both the lithosphere and athenosphere, but not fast moving because of high pressure, and high density
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crust
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lightweight and brittle, consists of the oceanic crust(basalt), which is much thinner than the continental crust made of granite. Continental crust is thicker and less dense (floats on ocean)
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How was the ocean formed?
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Came from degassing of the crust and mantle rocks, also from comet impacts. Large amounts of 40Ar, product of 40K radioactive decay. Hot vapors from the outgassing rocks and volcanic vents condensed into clouds. Rained for like 20 million years, but it was too hot so it was vaporized into clouds. Clouds finally cooled enough to form droplets and fell to the earth, only to be evaporated again. As time progressed earths surface cooled and the water began to accumulate into basins and seeped into the rocks. Deposited minerals into the rocks and formed the salty oceans.
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How do we know the earth is layered?
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Seismic waves. P and S waves, p can go through liquid core, s cannot.
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How does magnetism happen?
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movement of liquid metal in the molten outer core
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Oceanography
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The scientific study of the Earth's oceans with the goal of understanding its processes and phenomena.
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First Ocean Voyagers
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from Asia • to Papua New Guinea by 60,000 years ago • to Polynesia 4000 BC ? 1000 AD more recently..... • to Hawaii ~450 AD and other remote islands
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Ptolemy
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(An Egyptian?Greek) oriented charts placing N at the top, and dividing deg
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Scientific Knowledge of the Oceans
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• 1925, German Meteor Expedition - First mapped areas of ocean floor using echo sounding • Post?WWII - global maps of ocean floor - military interest in
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Research Knowledge
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• A way of gathering of knowledge that is not individual, but universal. - observable and measurable by multiple humans - i.e. repeatable • Follows a protocol ? the Scientific Method
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Belief Knowledge
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• Knowledge about the world is inherent and unique in each human being. - attained by individual revelation - a personal belief that is not observable by others. • "Feelings" as an example
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What is peer?review?
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• Scientific studies that are published in academic journals go through stringent peer review - Typically by 3 scientists with relevant expertise - Compare Industry reports (profit motive, no review)
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Age of Our Solar System
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• Meteorites date to 4.567 Ga - left over bits from the time of solar system formation
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Origin of Solar System
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• Solar nebula condenses from past exploded star - H is concentrated at the center and condenses enough to form our sun - Solar nebula rotates as it condenses - Protoplanets in
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Formation of the Moon
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• Glancing blow by a Mars?sized object ~4.5 Ga - Re?melted some of both bodies - Involved primarily the mantles (not the cores) of each body • Moon rock chemistry points to this - Imparted more spin and tilt to the earth than would otherwise be expected
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Origin of the Ocean 1: volcanoes
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• Volcanic H2O vapor outgassing from the Earth as it cooled • Current Volcanos emit: - H2O (water), 50?60% - CO2 (carbon dioxide), 24% - SO2 (sulfur dioxide), 13% - "other", 3%
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Origin of the Ocean 2: comets
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• Comets - ice and rock
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Deepest part of the ocean
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11km
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Key Observations from Earthquakes
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• Shallow earthquakes are associated with mid ocean ridges • Deep Earthquakes are only associated with trenches
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abyssal plains
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avg 4km deep, relatively flat, comprised of old, dense ocean floor
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Mid?Ocean ridges
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- Long linear mountain chains - Occur in all oceans - Fractures perpendicular to ridges
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active margins
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margins marked by trenches, subducting zones
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seamounts
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submarine volcanoes also called guyots or atols
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Sediment
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Material that settles to the bottom of a liquid
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Law of Superposition
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Younger material is deposited on top of older material.
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Clastic Sediments
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Clastic: little bits of rock - Terrigenous: material transported from continents ...later in the semester
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Chemical Sediments
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Chemical: minerals precipitated from seawater 1. Abiotic (not shells) 2. Biotic (shells of organisms)
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Abiotic
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Abiotic: chemicallyprecipitated,withoutlife • e.g., manganese nodules
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Biotic
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Biotic: biologically precipitated • i.e., shells of organisms • Foraminifera • Coccothithophores • Diatoms • Radiolarians millions of skeletons make 'oozes' or ocean mud.
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ccd
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snow line, caco3 does not accumulate below this line, because the water is colder, and dissolves CO2 faster, so it does not accumulate there
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ocean sedimentation
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slow in the deep sea, because sediment is easily dissolved by cold water, faster above ccd line
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water molecule
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polar molecule H20, hyrdrogen bonds are weak, but strong enough to result in surface tension
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solution
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two or more components, with uniform molecular properties throughout solvent and solute, water to salt
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solution: solvent
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• Solvent (usually a liquid) is more abundant water is a good solvent
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solution: solute
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• Solute (usually a solid or gas) is the less abundant component
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SALINITY,
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• Salinity is the total quantity of dissolved inorganic solids in water - As salinity increases, freezing point decreases - As salinity increases, evaporation slows - As salinity increases, density increases
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Sensible Heat
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- Heat carried by convection or conduction • temperature changes (it can be sensed) • Your hands heated near a fire. Your hands heated when you hold a wire in fire.
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Latent Heat
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- A loss or gain of heat as water changes state • temp does not change during change of state
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thermal intertia
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tendency to resist change in temperature, water has a high resistance to change in temperature
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Upwelling
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- the vertical movement of water from depth moving up toward the surface.
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Downwelling
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- the vertical movement of water from the surface, moving down (sinking)
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Vertical mixing
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in the ocean is like a conveyor belt • downwelling in one area • upwelling in another • but most of the time it travels sideways
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Density Change Mechanisms: Salinity
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• Add Fresh Water, salinity drops • rain • melting of ice • river (local only, not global) • Evaporate, salinity rises • Form Sea Ice, salinity rises • when seawater freezes, it makes "pure" ice and leaves the salts behind in the sea--left over water is saltier
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North Atlantic Deep Water (NADW)
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• formed in the open North Atlantic by cooling of high salinity water • flows southward underneath the Gulf Stream • salty and cold
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Antarctic Bottom Water (AABW)
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• formed adjacent to Antarctica by increasing salinity of cold water through ice formation • flows northward into all major ocean basins • salty and cold
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Intertropical Convergence Zone (ITCZ)
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• Trade Wind Convergence - Zone of intense rainfall, storms - Migrates north and south with the seasons - Important for low latitude agriculture
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Coriolis Effect Second Order Control on ATM Circ.
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• Fluids in motion are affected by Earth's rotation - Air masses move to the right in the northern hemisphere - Air masses move to the left in the southern hemisphere
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three cells of air flow
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hadley cell ferrel cell polar cell
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ocean v land heat retention
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continents cool and heat faster than ocean, ocean stays relatively the same temperature
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