Oceanic Observations and World Ocean Orgins Ch.1 Flashcards
what percentage or earth’s suface is covered by oceans?
70.8%
CTD (conductivity-temperature-depth)
- main instrument in oceanography
- measures temp and salinity
The Rosette (w/ CTD+ more sensors+ water sampling)
- deployed off ship usually
- data fed back to ship along wire in realtime
- Naskin bottles sample ocean water at selected depths
ARGO Floats
A CTD that drifts with ocean currents and comes to the surface regularly to communicate with satellites and transmit data
acoustic doppler current profiler (ADCP)
measure velocity in oceanb by pinging sound waves and analyzing the return wave
Air-sea interaction meteorology
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
Nebular hypothesis
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)
Proto-earth
- larger than earth today
- homogenous composistion
- H/He atmosphere
- bombarded by meteorites
- moon formed from collision with an Mars-sized asteroid
- desnity stratification
Lithosphere
-cool rigid shell
-includes crust and upper mantle
-about 100km thick
forms tectonic plates
orgin of earht’s atmosphere
- 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
orgin of earth’s oceans
- outgassed water vapour fell as rain
- the first pernament oceans formed about 4 billion years ago
- salinity developed from dissolved rock elements
how do we kow the age of earthn
radiometric age dating using isotopes
-earth is about 4.6 billion years old
Archean earth System
- 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
First Autotrophs (Autotroph ia an organism that can produce its own food0
- similar to anaerobic bacteria; survive without O2
- Chermosynthesis; photosynthesis had not evolved
stomatolites
biofilms of cyanobacteria capture and bind sediment