LOS ANGELES – It’s a warm summer day along the Gulf Coast or southeastern Atlantic Seaboard. You head out to the many beaches and take a dip in the ocean to find it comfortably warm. Water temperatures are in the 70s or even 80s, and you feel like you can spend an entire afternoon in the surf.
Meanwhile, it’s a warm summer day along the Southern California coast. You head out to the many beaches and take a dip in the ocean to find … it’s a bit chilly! Water temperatures are in the mid- to upper 60s. Depending on your heartiness, it’s a much shorter dip in the waters than your East Coast beachgoers before returning to the sand to warm up. It’s why most California surfers will wear a wetsuit.
Both areas feature southern, tropical climates that seem endlessly warm, yet water temperatures are 10 to 20 degrees different. How can that be?
From the late spring into summer, the prevailing weather pattern will feature a ridge of high pressure anchored off the Pacific coast.
The result: A prevailing northerly wind that pushes warm, sun-kissed waters south along the coast. But the spin from Earth’s rotation causes an effect known as the Coriolis force that will bend that south-flowing water out to the west, pulling it away from the coastline.
The process will then pull deeper, much cooler water from the sun-starved depths of the Pacific toward the surface, dropping water temperatures. It’s a process known as “upwelling,” which plays out along the entire U.S. Pacific coast.
Upwelling explains why water temperatures along California, Oregon and Washington beaches are much cooler than similar-latitude beaches in the East.
On the other hand, moving water contributes to warming temperatures along the Gulf and Atlantic coasts.
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In the Gulf of Mexico, warm waters from the Caribbean Sea – much farther south and in an even warmer climate – are fed into the Gulf of Mexico via the Loop Current.
The current will boost water temperatures well into the 80s during the late summer and early autumn, with some offshore buoys even measuring temperatures in the lower 90s.
Meanwhile, on the Atlantic side of the U.S., the Florida and Gulf Stream currents carry warm waters from the Caribbean Sea up north along Florida’s coast and then right around the curve of the southeastern Atlantic coast before turning out to sea around Cape Hatteras, North Carolina.
Average summer water temperatures off the coast of Charleston, South Carolina, are in the lower 80s, about 15 degrees warmer than Los Angeles’ ocean waters despite being at similar latitudes.
These vast differences in water temperatures explain why hurricanes and tropical storms are a yearly danger along the East and Gulf coasts yet are unheard of in the West.
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Tropical systems get their fuel from warm ocean waters that need to be at least 80 degrees to power significant storms. Those conditions are easily reached off the East and Gulf coasts but never reached along the U.S. West Coast. (However, they are reached farther south along Mexico‘s western coastline.)
That said, there have been two recorded instances of tropical systems reaching Southern California over the last two centuries.
As toasty as a swim might be in the East in June or July, water temperatures warm even more as you get into late August and September, even though peak solar heating occurs at the summer solstice in late June.
That’s due to water taking a longer time to heat from the sun. When you turn on a pot of water to boil, the process isn’t instant; it takes a bit of time for the water to absorb the heat.
The same goes for the ocean: It takes longer for ocean waters to warm from increased sunshine than it does for air, though the atmosphere takes some time too.
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The peak heating for summer temperatures is typically in late July but can be four to six weeks later for ocean temperatures.
Suffice to say, if spending hours in warm ocean waters is your dream summer vacation, book a flight to the East instead of the West.