History of Oceanography
History of Oceanography
Herodotus’s map of the world ~ 450 B.C. (ancient Greek)
Ptolemy’s map of the world ~ 150 A.D. (Roman)
Post-Roman World
Roman Empire collapses
Western knowledge of Greek and Roman world largely dies with the Roman Empire in Middle Ages - “Dark Ages”
Middle Ages - Arabs become maritime traders using knowledge of Greeks and Romans
Trade with India and southeast Asia for silks and spices
Sold for huge profits, making them rich
European buyers
Become accomplished celestial navigators
Developed powerful army from riches and triumphed many areas
European monarchs decide to pioneer the trade routes and goods themselves
Age of Discovery (1487-1522)
Could be retitled: Revenge of the Europeans/Revenge of the Monarchs
Sailed in large groups to try to obtain great riches for the European monarchs
Western European monarchs seek trade routes and riches
Columbus - essentially built Spanish empire
Balboa
Magellan
Spanish became rich, English and Dutch became accomplished pirates
England Becomes Ruler of the Seas
England defeats Spanish Armada in 1588
Spain lost its navy
English knows that in order to project power in the world and maintain world trade, they need to understand the oceans
Advances in Scientific Understanding
Kepler (1571-1630): planetary motion
moon’s connection to the tides
Galileo (1564-1642): mass and acceleration
allowed us to study air and water motion
Newton (1642-1721): unifying law of gravity, later used to explain tides
Challenger
England’s effort to understand the world’s ocean
Floating laboratory
Largely a sailing vessel
Built floating labs
Pulled nets behind it to study the ocean life
Discovered new living organisms basically every time they pulled up the net
Used an anchor and a cable to measure the depth of different areas of the ocean
Deepest water they found was ~11,000m deep (called the Challenger Deep) → Mariana Trench!
Made ~300 of these around the world
Depth varied widely
Voyage of the Meteor (1925-1927)
German ship
Period between the World Wars
First use of SONAR
SOund NAvigation Ranging
Two-Way Travel Time: the time it takes the sound wave to hit the sea floor and return to the ship
Distance/time = velocity
distance = velocity * time
ex: 60 = v * 6
v = 10 ft/s
2 depth = v t
depth = v * t/2
ex: d (2 seconds) = 10 ft/s * 2s/2
d = 10 ft
ex: d (4 seconds) = 10 ft/s * 4s/2
d = 20 ft
Inconsistent velocity
Speed of sound is not constant
Function of the “stuff” it goes through
Higher the density of a material, the faster a sound wave can move through it
Water pressure doesn’t have much to do with density
Water density in the oceans is NOT consistent
Soundwaves speed up as they get deeper in the ocean
3 Star Concept:
CORK CONCEPT: high density things want to sink, low density things want to float
Glomar Challenger (1968-83)
Scientific drill rig
Drilled holes into the sea floor to recover sea cores
If you know what the sea floor is made of, you can figure out how it’s made
Age of the seafloor is important because it goes towards the validity of the plate tectonics theory
Important because they are repositories that help us understand global climate change
Franklin Folger Map
Studied ship logs and floated along with the currents and recorded navigational hazards
Gulf Stream: takes water out of the Gulf of Mexico