Oceanic Observations and World Ocean Orgins Ch.1 Flashcards

1
Q

what percentage or earth’s suface is covered by oceans?

A

70.8%

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2
Q

CTD (conductivity-temperature-depth)

A
  • main instrument in oceanography

- measures temp and salinity

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3
Q

The Rosette (w/ CTD+ more sensors+ water sampling)

A
  • deployed off ship usually
  • data fed back to ship along wire in realtime
  • Naskin bottles sample ocean water at selected depths
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4
Q

ARGO Floats

A

A CTD that drifts with ocean currents and comes to the surface regularly to communicate with satellites and transmit data

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5
Q

acoustic doppler current profiler (ADCP)

A

measure velocity in oceanb by pinging sound waves and analyzing the return wave

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6
Q

Air-sea interaction meteorology

A

measure ocean T and S, atomsphdric wind, pressure, radiation nad precipitation; usually on oceanic buoys or research ships but also on land or on sea ice

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7
Q

Nebular hypothesis

A

all bodies in the solar system formed from Nebula

  • Gravity concentrates material at center of clouds (sun)
  • protoplanets form from smaller concentrations of matter (eddies)
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8
Q

Proto-earth

A
  • larger than earth today
  • homogenous composistion
  • H/He atmosphere
  • bombarded by meteorites
  • moon formed from collision with an Mars-sized asteroid
  • desnity stratification
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9
Q

Lithosphere

A

-cool rigid shell
-includes crust and upper mantle
-about 100km thick
forms tectonic plates

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10
Q

orgin of earht’s atmosphere

A
  • initially mostly H and He that was blown out to space by the solar wind-
  • outgassing;occured during drnsidsty stratification as earth colled ; water vapour, carbon dioxide, hydrogen, other gases ALMOST NO OXYGEN
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11
Q

orgin of earth’s oceans

A
  • outgassed water vapour fell as rain
  • the first pernament oceans formed about 4 billion years ago
  • salinity developed from dissolved rock elements
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12
Q

how do we kow the age of earthn

A

radiometric age dating using isotopes

-earth is about 4.6 billion years old

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13
Q

Archean earth System

A
  • 3.8 to 2.5 billion years ago (Ga)
  • atmosphere had hardly any oxygen; eeriest life probably anaerobic
  • UV radiation (no ozone shield); earlist life proabaly underwater
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14
Q

First Autotrophs (Autotroph ia an organism that can produce its own food0

A
  • similar to anaerobic bacteria; survive without O2

- Chermosynthesis; photosynthesis had not evolved

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15
Q

stomatolites

A

biofilms of cyanobacteria capture and bind sediment

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16
Q

kerogen

A
  • concentrated, high-molecular-weight organic compounds occuring in sedimentary rocks
  • precursor to fossil fuels
17
Q

carbonate (most commonly CaCo3)

A
  • the mineral in limestone

- many marine animals form carbonate shells