Oceanography Flashcards
Dissolved gasses
Nitrogen, oxygen, and carbon dioxide in seawater
Carbon dioxide and oxygen VERY IMPORTANT
Plants- carbon dioxide w/ sunlight and water: photosynthesis
Photosynthesis releases oxygen into water
Oxygen used to turn food into energy for sea creatures
Sea creatures use gills to take oxygen from water
Salinity
Amount of salt in water/ Measure of amount of dissolved solids in a liquid
Measured in parts per thousand (ppt)
Average salinity of oceans: 34-35 ppt
Thermocline
The middle heat zone of the ocean
There are three heat zones: the surface layer, the main thermocline, and the deep-water layer
Water here gets colder the deeper the ocean
Continental Shelf
The continental shelf goes from the shore to the continental slope, the ‘drop-off’
The continental shelf’s depth can reach 200 meters
The continental shelf is a part of the continental margin of the ocean, which includes the continental shelf, continental slope, and continental rise
The continental margin is more shallow in comparison to the deep-ocean basin
The continental margin is made of continental crust, and the deep-ocean basin is made of oceanic crust
Continental Slope
“The drop-off”
The continental slope goes from the edge of the continental shelf to the flattest part of the ocean
The continental slope can reach 4,000 meters deep
The continental slope is a part of the continental margin, which includes the continental shelf, continental slope, and continental rise
The continental margin is more shallow than the deep-ocean basin
The continental margin is made up of continental crust, and the deep-ocean basin is made of oceanic crust
Ocean trench
Ocean trenches are cracks in the deep-ocean basin formed when one oceanic goes under a continental or oceanic plate
The Mariana Trench is the deepest place in the world, reaching a depth of 10.9 km
How deep a spot on the ocean floor is can be determined using sonar, Sound Navigation and Ranging, when sound is bounced from the bottom of the ocean back to a ship
Mid-ocean ridge
The mid-ocean ridge is a mountain ridge that goes all around the world
It is 80,000 kilometers long
The mid-ocean ridge is formed when tectonic plates separate and let magma through, which cools and causes the ridge to expand, forming the mountains
Abyssal Plain
The abyssal plain is the flat part at the bottom of the deep-ocean basin
The abyssal plain is covered in mud and the remains of marine organisms
It is about 4,000 meters deep
Seamounts
Seamounts are mountains on the bottom of the ocean floor made of volcanic materials
They form when magma goes through the tectonic plates and cools
Seamounts that go above sea level form volcanic islands
Sonar
Sound Navigation and Ranging
Is a way to see how deep the ocean floor is from above water
Based off of how bats use echolocation
The longer it takes for a sound beam to reach the boat again, the deeper the water
Depth= speed of sound in water x half the travel time
Deep zone
The deep zone is the most dense layer of the ocean, and the coldest
There are three layers of density: the surface mixed zone, the pycnocline, and the deep zone
Only in polar regions is the deep zone ever exposed because there is not a pycnocline there
Density of water is determined by pressure, salinity, and temperature
Aphotic zone
The aphotic zone is the darkest layer of the ocean
There is no light, a- no, not; photic- light-related
Also called the midnight zone
Is 90% of the ocean
There are three zones of light in the ocean: euphotic zone, disphotic zone, and aphotic zone
Hydrothermal vent
Forms when seawater meets magma exposed by convergent plate boundaries and ridges
Water is warmed up and can get up to a heat of 700 degrees Celcius!
The water coming out of hydrothermal vents does not boil because of the extreme pressure at the bottom of the ocean
Crest
The top of a wave
Breaks at shore
The crest to the trough is the wave height
The length from crest to crest is the wavelength
The smaller the wave length is the larger the wave height
Trough
The trough is the bottom of a wave
The measurement from the crest to the trough is the wave height
The length from crest to crest is the wavelength
No water is actually being moved side to side, it is actually moving in circles in one spot