How warm ocean currents are beneficial in the coastal areas?
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- Sea flows impact the temperature of the locale they travel through. Warm flows increment the temperature of the coasts along which they move. Sea breezes that blow over warm flows get warmed thusly and ingest dampness.
- At that point they convey the glow and dampness to neighboring seaside regions. For instance, the North Atlantic Drift, conveying warm tropical waters northwards, expands temperatures along the bank of north-western Europe and assists with keeping ports along these coasts open (i.e., not solidified) all through the year.
- On the other hand, winds that blow over cool flows become cold and dry. Along the western banks of most land masses, these dry, cold breezes have prompted the advancement of deserts like the Atacama (South America) and the Namib (Africa) deserts.
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