Reasons Why Pacific Ocean & Atlantic Waters in the Gulf of Alaska Don't Mix

The Pacific Ocean and Atlantic Waters in the Gulf of Alaska have been the most eye-catching oceans in the world. This is due to their strange phenomenon of not mixing together despite being in the middle of the ocean.

Reasons Why Pacific Ocean & Atlantic Waters in the Gulf of Alaska Don't Mix

Well, below are the reasons that can explain the strange phenomenon.

Since all of the new rivers fell on the Pacific, separating the Antarctica freezing masses, the Pacific ocean is less smelly than the Atlantic. The Pacific Ocean's pungent level is 34 percent lower than the Atlantic Ocean's, which is 37 percent higher.

Gulf of Alaska, where two oceans meet but never mix. - Awesome | Gulf of  alaska, Two oceans meet, Alaska

Given the proximity of water and the effects of precipitation and the sea stream, the temperature of the two seawaters is very important.

The spectacular nature

The Pacific Ocean is also known for being larger than the Atlantic Ocean, measuring approximately 40 cm larger in terms of 1000 decibels.

So these three variables were considered, which is why this is put out so far in the Atlantic, the ocean where the speed of both ocean glasses of water compensates for one another.


According to Ken Bruland, a professor of ocean sciences at the University of California-Santa Cruz, he stated that 

the eddies- the slow-moving currents often carry with them huge quantities of glacial sediment. Rivers like Alaska's 286-mile-long Copper River, prized for its salmon and originating from the Copper Glacier far inland. It empties out east of Prince William Sound, carrying with it all that heavy clay and sediment. And with that sediment comes iron.

Pacific Ocean | Depth, Temperature, Animals, Location, Map, & Facts |  Britannica

"Glacier rivers in the summertime are like buzzsaws eroding away the mountains there," Bruland said. "In the process, they lift up all this material -- they call it glacial flour -- that can be carried out."

Additionally, when these glacial rivers spill into a bigger body of water, they are swept up by ocean currents that flow east to west and continue to cycle there. This is one of the key ways that iron, which is abundant in glacial runoff clay and silt, is carried to iron-deficient areas in the Gulf of Alaska.

On the other hand, Ken`s study shows that these waters mix.

"They do eventually mix, but you do come across these really strong gradients at these specific moments in time," he said. Such borders are never static, he added, as they move around and disappear altogether, depending on the level of sediment and the whims of the water". He noted.


These waters do mix at times and you need to know the science behind the phenomenon.