Module 9- Oceans and Beaches Oceans and Beaches How do oceans shape our lives? Image Credit: FreeDigitalPhotos.net

Distribution of Water on Earth 97% of all water on Earth is salt water. Only 3% is freshwater, including icebergs, lakes, rivers, and groundwater. Water covers 71% of Earth’s surface. The major oceans in the world are the Pacific (51.6%); the Atlantic (23.6%);Indian (21.2%); Southern and Arctic along with the other seas of the world make up the remaining 3.6% of water on Earth. Image Credit: Nasa.gov

Properties of Ocean Water Ocean water is a mixture of gases and solids dissolved in pure water. There are 85 elements found to exist in ocean water. Salinity describes the amount of dissolved salts in ocean water. It is expressed in parts per thousand, with the average being 35 parts per thousand. The most abundant salt is sodium chloride, NaCl. A liter of seawater will contain about 2.5 teaspoons of this common salt. Image Credit: Photolib.noaa.gov

The most abundant gases in ocean water are nitrogen, carbon dioxide and oxygen. The amount of dissolved gases is affected by two things: 1.Depth – the greater supply of gases at the ocean’s surface is due to the penetration of sunlight. This allows photosynthesis to take place which ensures a large supply of oxygen. Image Credit: Photolib.noaa.gov

2. Temperature of ocean water – warm water holds less dissolved gas than cold water. This means that denser cold water sinks, carrying oxygen to deep areas of the oceans while allowing animals to live there. The warmest layer of the ocean is the surface zone where water is mixed by waves and currents. The thermocline is the zone below the surface where rapid temperature change occurs. The coldest layer is the deep zone with temperatures of around 5 degrees Celsius. Image Credit: PhotoLib.noaa.gov

Motions of the Ocean Waves are the movement of energy through a body of water. Most waves are formed by winds blowing over the surface of the ocean. This transmits energy to the water, forcing it to ripple. Wind causes waves! Image Credit: PhotoLib.noaa.gov

The size of a wave depends on three things: 1.The strength of the wind. 2.The distance the wind blows (called the fetch). 3.The length of the gust (duration).

Waves are divided into several parts. Crest – the highest point of the wave. Through – the valley between two waves. Wavelength – the horizontal distance between the crests or troughs of two consecutive waves. Wave height – a vertical distance between a wave’s crest and the next trough. Wave period – measures the size of the wave in time.

Ocean waves caused by earthquakes are called tsunamis.

Water below the surface moves in streams called currents. These currents are caused by two factors:  wind patterns and  water density. Image Credit: srh.noaa.gov

Surface currents are caused by wind patterns and usually have a depth of several hundred meters. These currents affect climate and weather patterns by warming or cooling the air above the water. Surface currents affect weather. Image Credit: sos.noaa.gov

The Gulf Stream is known as a long-distance current that carries warm water from the southern tip of Florida along the eastern coast of the US. Image Credit: oceanservice.noaa.gov

Currents in the Northern Hemisphere move clockwise (currents correspond to the wind circulation in each hemisphere), while currents in the Southern Hemisphere move counterclockwise. Image Credit: mynasadata.larc.nasa.gov

Surface currents that travel over short distances are called short- distance currents. These currents are usually found at shorelines. Currents moving parallel to the shore are called longshore currents. As these currents move they carry large amounts of sand creating sand bars. A rip current occurs when a current cuts an opening in a sand bar and the currents return to the ocean in a powerful, narrow flow (a type of undertow).

Deep currents are movements of water deep under the surface of the oceans and are caused mainly by differences in water densities. The density (heaviness of the water) is affected by temperature and salinity. Cold water is more dense than warm water. The saltier the water, the more dense. Image Credit: sos.noaa.gov

Deep currents usually flow in opposite directions from surface currents. The movement of deep ocean currents to the surface is called upwelling. This occurs when deep cold currents are forced upward by the ocean floor bring nutrient rich foodstuffs to the surface. This produces rich fishing grounds in areas where upwelling occurs. (Example – Peru, Chile) Image Credit: oceanservice.noaa.gov

El Nino refers to a warm ocean current that typically appears around Christmas time and lasts for several months, but may persist into May or June. The warm current influences storm patterns around the globe. Image Credit: science.nasa.gov

Upwelling ceases to occur when winds die down. Without the nutrient rich waters, many fish and sea creatures die, devastating the fishing industry. Without upwelling, the water becomes much warmer changing weather patterns globally. Image Credit: oceanservice.noaa.gov

Shoreline Formation Shorelines are constantly changing landscapes due to powerful waves constantly eroding rocks and depositing sediments to reshape the land. The following are examples of shoreline formations: Image Credit: nps.gov

1.Sea Cliffs – steep faces of rocks 2. Caves – hollowed out portions of sea cliffs Image Credit: celebrating200years.noaa.gov

3. Sea Stacks – columns of resistant rocks left standing. 4. Sand Bars – an underwater ridge of sand created by longshore currents. Image Credit: photolib.noaa.gov Image Credit: srh.noaa.gov

Beaches – waves deposit large amounts of rock particles to form our beaches. The backshore is the area of the shoreline above the high water or high tide mark. This can contain cliffs or sand dunes or a berm (flat upper beach). The foreshore is the area that is exposed at low tide. It may have a beach scarp (vertical slope produced by wave erosion) and a low tide terrace (broad flat area exposed at low tide). The offshore region extends from the low tide mark seaward beyond the wave breaking zone. It has a shoreface (slope below the low tide mark) and a longshore trough (a depression parallel to the beach between the low tide mark and wave breaking zone). Image CreditL ngs.noaa.gov

Barrier Islands – (nature’s way of straightening out the shore) Elongated bodies of sand bounded on either end by inlets allowing salt and fresh water to flow into and out of the estuary behind the island. (Example – The Outer Banks) Image Credit: learnnc.org

V. North Carolina ’ s Barrier Islands – The Outer Banks A. Barrier islands form in response to four factors: 1.Levels beginning about 10,000 years ago. The sea level was 300 to 400 feet below its present level. The following is an example of sea level creating barrier islands.

a. A straight coast forms during lower sea levels. b. Rising sea levels flood valleys on land and creates a sinuous coast. c. Sand eroded from pre-existing ridges forms spits (sandbar connected to a curving shoreline). d. The spits are breached by storms, separating the islands from the mainland.

2. A large supply of sand – 15,000 years ago the sea level was much lower, waves and winds formed beach ridges (dunes) on the coast of North Carolina. Sea levels rose and broke through the dune forming a lagoon, and the dune is now isolated as an island.

3. A gently sloping coastal plan – North Carolina ’ s coast slopes at.2 feet per mile. The underlying geology of North Carolina consists of sediments dating of Quaternary age (1.8 million years ago to present) with older sediments buried underneath. The deposition of these sediments created a gentle slope conducive to forming barrier islands.

4. Sufficient wave energy to move sand occurred.

The Truth About Shorelines Beach erosion is an expected part of barrier island evolution, especially as sea levels rise. Shoreline erosion is not a problem until someone builds a structure by which to measure it. Shoreline erosion does not create problems for the beach, it simply changes its position. Image Credit: coastalmanagement.noaa.gov

Human activities such as building seawalls, dune construction, building construction, channel dredging, reduce the beaches’ sand supply. This increases the rate of shoreline retreat. Shoreline engineering protects the interests of few people, who are causing the erosion to begin with, and is a high cost to state and federal governments. Image Credit: coastalmanagement.noaa.gov

“You can have buildings, or you can have beaches; in the long run you cannot have both.” The ultimate truth is to avoid the hazards and evaluate the level of risk if choosing to build on a barrier island or coastline. Image Credit: sos.noaa.gov

Image Credit: FreeDigitalPhotos.net The End