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Here is another creative presentation by your slide maker on the topic "OCEAN CURRENTS OF THE WORLD". Hope you like it. If you like it then please, *like*, *Download* and *Share*. By- Slide_maker4u (Abhishek Sharma) *******For presentation Orders, contact me on the Email addresses Written below******** Email- Sharmaabhishek576@gmail.com or Sharmacomputers87@gmail.com *******THANK YOU***************
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Oceans are a vast body of salt water that covers almost three to fourths of the earth's surface. Seas are smaller, found on the margins of the ocean and are partially enclosed by land. Seawater: High density, high heat capacity, colder, salty and slightly compressible (its volume decreases under pressure), thus its density increases with pressure. Why is Ocean Circulation Important? •Similar to winds in the atmosphere, they transfer significant amounts of heat from equatorial areas to the poles and thus play important roles in determining the climates of coastal regions. •The ocean circulation pattern exchanges water of varying characteristics, such as temperature and salinity •ocean currents and atmospheric circulation influence one another. •in addition, they transport nutrients and organisms
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Dubai, often portrayed as a shimmering oasis in the desert, faces its own set of challenges, including the occasional threat of flooding. Despite its reputation for opulence and modernity, the emirate is not immune to the forces of nature. In recent years, Dubai has experienced sporadic but significant floods, testing the resilience of its infrastructure and communities. Among the critical lifelines in this bustling metropolis is the Dubai International Airport, a bustling hub that connects the city to the world. This article explores the intersection of Dubai flood events and the resilience demonstrated by the Dubai International Airport in the face of such challenges.
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Ocean Circulation
1.
2.
3.
4.
Temperature Structure of
Ocean thermocline
5.
Ocean Circulation
6.
7.
8.
Sea Surface Temperature
http://www.ldeo.columbia.edu/dees/ees/climate/slides/sst_march.gif
9.
10.
Temperature-Salinity (density) Diagram
11.
Thermohaline Circulation North
Atlantic Deep Water (NADW 15 million m 3 of near surface water descend into the deep ocean each second.
12.
Thermohaline Circulation -
The Ocean Conveyor
13.
Equatorial to polar
heat transport and water flow
14.
Ocean – Atmosphere
Circulation
15.
UNEQUAL HEATING OF
EARTH BUT – Outgoing solar radiation is not as uneven
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