OCEANS
Hypsometric Curve
EUSTATIC SEALEVEL CONTROLS
LOCAL SEALEVEL CONTROLS Subsidence Tectonism (mtn building) Isostatic adjustment
GROUP PRS Why is sealevel in Sitka falling? Mountain building B. Distance to equator C. Glacial melting D. Mid-ocean spreading E. Local subsidence
Greenland ice melts = 5 m rise
What impact would a .5-1 m sealevel rise have on the US? Given that we may not know how much it will rise for another 20-30 years, what if anything, do we do now?
OCEANS TIDES
Spring Tides Neap Tides
PRS If the moon was twice as far away the tides would be A. Larger B. Smaller C. No change
Tides affected by shoreline shape
Tides affected by latitude
PRS If the Bay of Fundy was on the equator how would the highest tides be affected? A. Higher B. Lower C. No change
WAVES
Generated by wind speed, duration, fetch Wavebase = ½ wavelength
Shore profile is dynamic equilibrium
Wave Refraction waves bend toward slower medium
Wave energy focused on headlands = erosion Wave energy dispersed in bays = deposition
Wave refraction generates longshore current
Creates Spits Alligator point
PRS Which way is the longshore current flowing? To the North B. To the South C. To the East D. to the West E. Can’t tell
Barrier Islands How formed? Cutoff Spit Drowned Dunes Exposed Sand Bar
PRS Overwash causes barrier islands to move in which direction? Toward shore B. Toward the ocean C. Parallel to the coast
Coastal Engineering Seawalls
Beach Armor – Rip-Rap
Groins, jetties
Which way is the longshore current flowing? PRS Which way is the longshore current flowing? A. To the North B. To the South C. To the East D to the West E. Can’t tell
Beach Nourishment
GROUP PRS Why has the southern part of the island migrated onshore? Change of wave direction Development on southern island Rise in sealevel Inlet jetties Change in longshore current
Rip Currents
Convection
ITCZ = Inter Tropical Convergence Zone - Low pressure Rising air cools and rains
Note the pronounced shift in the ITCZ over India. What causes this?
PRS The shift is caused by Plate tectonics B. Eccentricity in earth’s orbit C. Atmospheric CO2 D. Asia E. Human interference
Coriolis effect
Convection cells and zonal wind flow