The interactions between the hydrosphere, atmosphere,
lithosphere and people in the study of coastal erosion make this topic
an ideal example of an Earth
System Science study. When looking at an earth system, the interaction
between people and their physical surroundings can become complicated.
The issues associated with coastal erosion and land management include
factors such as the environment, government, and individual needs. Reaching
a balance between these factors is a big challenge.
How are urbanization, societal change and technological advances increasing
or decreasing the damage caused by coastal erosion and catastrophic storms?
The beach-ocean system can be considered to be in a dynamic equilibrium. Sand that is moved off-shore by winter storms, leaving steep narrow beaches and ocean sand bars, is returned to the shore by the gentle waves of summer, creating wide, gently sloping beaches without ocean sand bars. However, the reality is that an equilibrium situation does not exist. Beaches do not qualify as a closed system because sand is regularly being lost from the system.
Coastal erosion occurs when wind, waves and long shore currents move sand from the shore and deposits it somewhere else. The sand can be moved to another beach, to the deeper ocean bottom, into an ocean trench or onto the land side of a dune. The removal of sand from the sand-sharing system results in permanent changes in beach shape and structure.
Forces that are constantly changing beaches combine with forces such as rising sea level and human activity, to create several concerns regarding the shape and future of the shore line on the east coast.
Issues such as erosion control, restoration of beaches and preparation for catastrophic events need to be dealt with by coastal communities. The response to the challenge varies from locality to locality, with local, state and federal governments each having a part in the final action plan that is implemented.
The natural factors that influence the coast are:
FACTOR | EFFECT | TIME SCALE | COMMENTS |
Sediment supply (source and sinks | Accretion/Erosion | Decades to Millennia | Natural supply from inland or shoreface and inner shelf sources cna contribute to shoreline stability or accretion |
Sea Level Rise | Erosion | Centuries to Millennia | Relative sea level rise |
Sea Level Change | Erosion | Months to years | Causes poorly understood |
Storm surge | Erosion | Hours to days | Very critical to erosion magnitude |
Large wave height | Erosion | Hours to months | Individual storms or seasonal effects |
Short wave period | Erosion | Hours to months | Individual storms or seasonal effects |
Waves of small steepness | Accretion | Hours to months | Summer conditions |
Alongshore currents | Accretion, no change,
or erosion |
Hours to millennia | Discontinuities (updrift//downdrift) and nodal points |
Rip currents | Erosion | Hours to months | Narrow seaward-flowing, near-bottom currents may transport significant quantities of sediment during coastal storms. |
Underflow | Erosion | Hours to days | Seaward-flowing, near-bottom currents may transport significant quantities of sediment during coastal storms. |
Inlet presence | Net erosion;high
instability |
Years to centuries | Inlet-adjacent shorelines tend to be unstable because of fluctuations or migrations inlet position; net effect of inlets is erosional owing to sand storage in tidal shoals. |
Overwash | Erosional | Hours to days | High tides and waves cause sand transport over barrier beaches |
Wind | Erosional | Hours to centuries | Sand blown inland from beach |
Subsidence, Compaction | Erosion | Years to millennia | Natural or human-induced withdrawal of subsurface fluids |
Subsidence, Tectonic | Erosion/Accretion | Instantaneous, centuries to millennia | Earthquakes; Elevation or subsidence of plates |
Coastal shorelines differ markedly in physical characterisitics and in vulnerablility to erosion. Erosion rate over time at a given point along the shoreline depends on factors such as:
Studies associated with coastal issues: