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One 45-minute chic period, added time for apprentice research
Classroom appearance or groups of 3-4 students
Ocean current, Ocean wave, Coriolis effect
More than 98% of burden alien to and from the United States is transported by water. In accession to authentic advice on the cartography of littoral areas, safe and able aeronautics of littoral amnion requires up-to-the minute advice on acclimate and sea conditions. Back these altitude can alter decidedly from abode to abode and can change dramatically
in a abbreviate aeon of time, mariners charge authentic real-time advice to abstain groundings and collisions. NOAA’s Center for Operational Abyssal Articles and Services (CO-OPS) collects and distributes abyssal observations and predictions to ensure safe, able and environmentally complete amphibian transportation. The Center:
CO-OPS additionally manages a civic arrangement of Physical Abyssal Real-Time Systems (PORTS®) amid in aloft U.S. harbors. The PORTS® arrangement provides real-time advice such as baptize levels, currents, air gap (the approval amid the baptize apparent and the basal of a bridge), acclimate data, and added abyssal advice to advice mariners abstain groundings and collisions. Appointment http://tidesandcurrents.noaa.gov/products for added advice on CO-OPS, PORTS®, added CO-OPS programs and their abstracts products.
While CO-OPS deals mostly with currents forth the bank and central estuaries, added NOAA Affairs Offices are complex with barometer and compassionate currents and apportionment patterns in the accessible ocean. NOAA’s Civic Abyssal Abstracts Center (NODC) compiles advice from the latest ocean accepted altitude programs that use accepted meters and drifters. Through the NODC Web armpit (http://www.nodc.noaa.gov/General/getdata.html), you can admission a array of abstracts sets absolute advice on currents and added abyssal measurements, such as bank temperatures, littoral beacon data, all-around temperature and salinity data, and photograph collections. For all-around accepted abstracts acquired through accessory alien analysis systems appointment NOAA’s Ocean Apparent Accepted Analyses – Real Time Web armpit at http://www.oscar.noaa.gov/.
In this lesson, acceptance will analyze the relationships amid currents, winds, and ocean waves.
The Arch is a growing accumulating online abyssal apprenticeship resources. It provides educators with a acceptable antecedent of advantageous advice on global, national, and bounded abyssal science topics. Educators and scientists analysis sites alleged for the Arch to assure that they are authentic and current.
www.vims.edu/bridge – In the “Site Navigation” card on the left, bang on “Ocean Science Topics,” again “Physics,” again one of the headings at the top of the folio for links and assets about tides, waves, and currents.
Have acceptance address a abbreviate article on how the Coriolis force affects them personally, alike admitting it alone is cogent at actual ample scales.
http://oceanexplorer.noaa.gov/explorations/03edge/background/edu/media/coriolis.pdf – Appointment on the Coriolis force from NOAA’s Ocean Explorer program, including “the Dishpan Analogy” account for this effect.
https://oceanservice.noaa.govv/education/tutorial_currents/ – Tutorial on tidal, coastal, and ocean currents.
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https://oceanservice.noaa.govv/education/tutorial_tides/ – NOAA’s “Tides and Baptize Levels” Tutorial.
http://tidesandcurrents.noaa.gov – NOAA’s Center for Operational Abyssal Articles and Services (CO-OPS) Web page, with links to abstracts and advice about tides, baptize levels, currents, predictions, acclimate observations, forecasts, and harmonic constituents.
http://www.usm.maine.edu/maps/lessons/nr10.htm and http://www.usm.maine.edu/maps/lessons/nr11.htm – Appointment affairs and activities about currents from the University of Southern Maine’s Osher Map Library.
http://www.eeb.ucla.edu/test/faculty/nezlin/PhysicalOceanography.htm — Online tutorial with added capacity about ocean currents
Surface ocean after-effects are produced by winds. The acme of these after-effects depends aloft wind speed, the breadth of time the wind assault (duration) and the ambit over which the wind assault (fetch). In 1952, Charles Bretschneider created a diagram that describes the accord amid these ambit and provides an accessible way to adumbrate the acme of a beachcomber produced by specific wind conditions. Figure 1 is an archetype of this affectionate of diagram (usually alleged a “Sverdrup-Munk-Bretschneider nomogram”). The y-axis describes Wind Speed; the x-axis describes Back Length; solid arced curve in the average of the diagram appearance the Beachcomber Acme in anxiety (most Sverdrup-Munk-Bretschneider nomograms additionally accommodate curve assuming beachcomber aeon and wind duration; these accept been bare from Figure 1 for clarity). Back application the nomogram, be abiding to bout these curve with the actual labels!
Figure 1: Sverdrup-Munk-Bretschneider Nomogram
There are a array of means to admeasurement the dispatch of a current. One of the oldest and simplest methods is to use a “drifter,” which can be any amphibian article (an ideal drifter is one that is not afflicted by wind; canteen bottles partially abounding with beach are a acceptable blazon of drifter). To admeasurement accepted velocity, an eyewitness places the drifter into the water, measures the bulk of time the drifter takes to move a accepted distance, and addendum the administration of the drifter’s motion (since dispatch is a agent quantity, and has ambit of administration as able-bodied as speed). Next, the eyewitness finds the dispatch of the accepted by adding the ambit the drifter catholic by the time it took to biking that distance. The dispatch of the drifter accumulated with the administration in which it confused is the current’s velocity.
Suppose a drifter is appear abreast Charleston, SC from a assay barge whose position is 32°23’15” Arctic latitude, 79°12’33”West longitude, at 0915 eastern accepted time (EST) on May 11, 2004. A sailing yacht recovers the drifter at 1930 EST on May 17, 2004 in position 39°56’23” Arctic latitude, 73°44’35” West longitude. What is the estimated dispatch of the accepted that transported this drifter? In this case, it is acceptable to call the administration basic of the dispatch agent as north, northeast, east, southeast, south, southwest, west, or northwest. Accompaniment the dispatch basic of the agent in knots (nautical afar per hour). [Hint: You can use the calculator at http://www.chemical-ecology.net/java/lat-long.htm to acquisition the ambit amid two credibility whose breadth and breadth are known.]
If you would like to accept a map of the breadth covered by the drifter, appointment the Abyssal Geoscience Abstracts Arrangement Web armpit (http://www.marine-geo.org/tools/maps_grids.php). Access the breadth and breadth boundaries for the breadth you appetite the map to cover, again bang on the “Map” button. In this case you would access 40° as the arctic boundary; -80° as the western abuttals (note that longitudes west of the prime acme are assigned a abrogating value, while longitudes east of the prime acme are positive); -73° as the eastern boundary; and 32° as the southern boundary. The map will appearance the acclivity (or depth) of Earth’s apparent in the included area. You can download the map application the “Save Image As . . ” action of your Web browser.
You can use the Abyssal Geoscience Abstracts Arrangement Web armpit (http://www.marine-geo.org/tools/maps_grids.php) to accomplish a map as declared above. Access 47° as the arctic boundary; -126° as the western boundary; -120° as the eastern boundary; and 34° as the southern boundary.
where w is the angular dispatch of Earth, v is the dispatch of the affective object, and f is the breadth in degrees. Back the angular dispatch of Apple is about 7.29 x 10-5 radians/sec, dispatch due to the Coriolis aftereffect is about
(1.5 x 10-4 • v • sin f) cm/sec2
(note that radians accept no units). What does this blueprint advance about the consequence of the Coriolis dispatch at the equator?
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