Exam 1 Flashcards
Continental shelf
Portion of the continent that is slightly submerged, epipelagic (sunlight) & mesopelagic (twilight) zones
Continental slope
Between outer edge of continental shelf and deep ocean floor, bathypelagic (midnight) zone
Continental rise
Wide, gentle incline from deep ocean plane to continental slope, abyssopelagic (abyss) zone
Ocean basin
Contain 3/4 of all water on the planet
Hadal zone
Deepest region of the ocean that lies within the oceanic trenches, named after Greek God Hades
Shore
land along the edge of the sea
Shelf
Edge of continent that lies under the water
Slope
Steeply sloping seafloor that lies between the shelf and oceanic basin
Mid-ocean range
A continuous range of underwater volcanoes
Seamount
Underwater mountains formed by volcanic activity, hotspots for deep sea marine life
Trench
A feature of convergent plate boundaries, deepest parts of the ocean, Mariana Trench
Island
Rise to surface from oceanic basins
Density
the mass per volume of seawater which is a function of salinity, temperature, and pressure/depth
Temperature
Primary parameter determining density expressed in degrees Celcius, bottom of ocean is 4 degrees, temperature of the sunlight zone varies based on location and season, begins to even out at around 70m
isotherms
constant temperature
isohalines
constant salinity
isopycnals
constant density
isobaths
constant depth
Amplitude
The maximum displacement of a particle on the medium from its rest position, from rest to crest
Height
vertical distance between the wave crest and trough
Wave length
Distance in which the wave repeats, period
Shallow water waves
elliptical, condensed vertically
Deep water waves
circular, long waves move faster than short waves
Time domain
For dynamic, real-time problems like control
frequency domain
Response to wave spectrum, resonance of structures
Probability domain
extreme value designs, hurricanes, tsunamis, etc.
Roll
x-axis rotation, tilting from side to side
Pitch
y-axis rotation, rise and fall of bow and stern
Yaw
z-axis rotation, ship spinning
Surge
x-axis translation, waves push ships forward and back
Sway
y-axis translation, swaying from wind or currents
Heave
z-axis translation, “HEAVE” a rope and pully and pulls system upwards
Fetch
Where wind is blowing forming waves
Dispersion
Waves without wind, caused by fetch traveling in the same direction over time
Seas
Waves created in the fetch zone
Ocean swell
Waves in the dispersion zone, shorter waves in the deep ocean, longer waves travel faster than shorter waves
Whitecaps
Wind blowing so strong that the water particles leave the wave
Wind
Pressure differences caused by uneven solar heating across the globe
Currents
Magnitude can vary with depth, direction can vary with depth and time, density of water is 1000x air, 4 degrees celsius at bottom of ocean
Tides
Revolution of celestial bodies and their gravitational pulls
Jackup, jacket, concrete
Fixed, bottom-supported units, shallow water
Tension leg platforms
Floating, moored tension lines
Spars
Floating, deepwater
Ship-based
Floating, period similar to the waves
Seawalls
Large wave resistant wall along shore, in Corpus, designed to withstand the full force of storm waves
Bulkheads
Smaller wave resistant wall along shore, designed to retain shore material under less severe wave conditions
Revements
Slope protection along waterways, protect shorelines and waterways against erosion by currents and small waves
Groins
Structures perpendicular to shore to interrupt littoral or slow down sand losses, prevents erosion, the long lines of rocks along beaches
Sand bypassing
Movement of sand from accreting up drift side to eroding down drift side of harbor
Jetties
Structures used at inlets to stabilize entrance locations
Breakwaters
Large barriers to protect land or water behind them from wave attacks, submerged breakwaters are below water level
Dissipative - active
Pneumatic or hydraulic energy absorbed during normal wave activity released during extreme wave activity
Fetch-limited
Winds blown at a constant rate long enough for wave heights to reach equilibrium at the end of the fetch
Duration-limited
Wave heights are limited by the length of time the wind has been blowing
Hindcasting
Past meteorological data
Nowcasting
current data
Forecasting
Future data