Oceanography Class: Chapter 10 Summary
Introduction
- Topic: Beaches, shoreline processes, and the coastal ocean.
- Coastal areas are busy with increasing human populations due to the mild climate, seafood availability, and transportation.
- 50% of the world's population lives along the coastlines.
- Coastal oceans are rich with marine life; 95% of fish caught are within 200 miles of the shore.
Definitions of Coastal Regions
- Shore: Zone between the lowest tide level and the highest elevation affected by storms.
- Coast: Extends inland where ocean-related features are found.
- Coastline: Boundary between the shore and the coast.
Zones in Coastal Areas
- Backshore: Above high tide line.
- Foreshore: Between high and low tide lines.
- Shoreline: Migrates with tides.
- Nearshore: Extends from low tide line to low tide breaker line.
- Offshore: Beyond low tide breakers.
- Beach: Deposit of wave-worked sediment.
- Wave-cut benches: Flat areas formed by wave action.
Beach Composition and Dynamics
- Composed of local rocks and biological material.
- Movement: Perpendicular and parallel to the shore.
- Swash: Water rushing up the beach.
- Backwash: Water draining back to the ocean.
- Seasonal variations affect beach width and sand deposition.
Longshore Transport
- Movement of sand along the beach by longshore currents.
- Influenced by wave direction and refraction.
- Affects sediment distribution along the coastline.
Types of Shores
- Erosional Shores: Have well-developed cliffs and are tectonically active.
- Depositional Shores: Feature barrier islands, sand dunes, and are subsiding.
Coastal Features
- Headlands, Sea Arches, Sea Stacks: Found on erosional shores.
- Barrier Islands, Lagoons, Spits: Found on depositional shores.
Human Impact and Coastal Management
- Hard stabilization structures: Groins, jetties, breakwaters, sea walls.
- Alternatives: Beach replenishment, relocation, construction restrictions.
Coastal Waters
- Close to land, vary in salinity and temperature due to runoff and evaporation.
Salinity
- Affected by freshwater runoff and evaporation.
- Results in haloclines or isohaline conditions.
Temperature
- Varies with latitude and season, can be isothermal.
Estuaries
- Vertically Mixed, Slightly Stratified, Highly Stratified, Salt Wedge: Types of mixing in estuaries.
- Important for marine life nurseries but threatened by human activities.
Wetlands
- Salt Marshes: From 30° to 65° latitudes.
- Mangroves: Found below 30° latitude.
- Serve as nurseries, protect inland from erosion, and filter pollutants.
- Over 50% of US wetlands lost, but conservation efforts are ongoing.
Sea Level Changes
- Affected by tectonic activity and climate changes.
- Past sea level changes due to glacial cycles.
Coastal Processes and Human Impact
- Rising sea levels impacting coastal areas.
- Human construction affecting natural coastal processes.
Conclusion: Understanding coastal processes is crucial for managing and protecting these dynamic environments from human impact and natural changes.