The Hair Metal Guide to the Ocean

Are you ready to rock?  ROCK THE OCEAN THAT IS! Then bust out your wailing guitar solos, leopard skin leotards, double bass pedals, and aquanet. Welcome to the Hair Metal Guide to the Ocean! Because glam rockers love the ocean.

You may not remember the awesome head and chest hair of Kip Winger, frontman of the surprisingly named band Winger. But he doesn’t care. He just wants you to remember one thing: THERE’S ONLY SEVEN SEAS!*

Kip Winter gets all the ladies with his extensive geographical knowledge.

Kip Winter gets all the ladies with his extensive geographical knowledge.

Our next hair metal phenomena are Tommy LEE WAVES. Just like his relationship with Pamela, these waves are driven by humps, humps and bumps at the bottom of the ocean that is! Lee waves are created when deep currents flow over rough bathymetry, forcing water up and down over these little hills to emit waves that radiate upward into the ocean interior. And just like my beloved internal waves, Lee Waves also break and mix the ocean. In fact, new research suggests that the breaking of lee waves can account for up to one third of the mixing that transforms water masses in the Southern Ocean!

Let the Tommy Lee Waves mix your ocean!
[source: https://sites.google.com/site/nikurashin/research]

You might have met this ocean phenomena in a previous post, stretching to great lengths across the Pacific Ocean is Gene Simmon’s COLD TONGUE. Occurring during La Nina, this ocean organ is a mass of cold water that extends from South America way out into the Pacific. But first, to coax this tongue out you need to turn on the hairdryer, the trade winds. Set on high, these westward winds upwell cold deep water off the South American coast and push it way out into the Pacific, forming the signature cold water streak. But there is always a time and a place for exposing your cold tongue. Once that hairdryer is turned off during normal and El Nino conditions, the winds die down and the cold tongue retreats back to the briney depths.

A scientific comparison of tongues. To the left, the Pacific Cold Tongue (blue). To the right, the Simmons Warm Tongue (pink).

Gene Simmons cold tongue reaches across all your ocean. 

Now it is time for the power ballad, EVERY WAVE HAS IT’S DRIFT. Fluid flow in a wave is oscillatory, pushing water backwards and forwards, up and down, making the lovely loop-de-loops seen below. But at the wave crest, the forward motion is larger than the backward motion in the wave trough causing a net forward transport of water. Just like a love song, the process of pushing water at the top of the wave forward is very slow, causing a slow drift of water in the direction of wave propagation, called Stoke’s Drift  after the dude that invented it.  Please raise a lighter to Poison’s beautiful ode to fluid dynamics.

Fluid parcels lie silently still
at the top of the sea
Although they both float close together
They’ll soon be meters apart inside

Was it some gust of wind or some type of tide?
Did that wave just push you right?
Though it tried not to flip you,
Though it tried,
But I guess that’s why they say

Every wave has its drift
Just like every up has its down
Just like every crest has a deep, deep trough
Every wave has its drift

The loops, they make me WEEP.

And finally, THE EDDIES VAN HALEN. Let their swirls mesmerize you.

These eddies are everywhere!

UPDATE:  I completely forgot Warrant’s ode to undersea exploration, WHERE THE DOWN BOYS GO.  Thank you @DrChrisKellogg.

Warrant: exploring hydrothermal vents, deep-sea corals and the deep ocean in general

Warrant: exploring hydrothermal vents, deep-sea corals and the deep ocean in general

 

* This does depend of your definition of which seas are important, Kip and I chose the largest ones.

Kim Martini (77 Posts)

Kim is a Physical Oceanographer at the Joint Institute for the Study of Atmosphere and Ocean at the University of Washington. She received her Ph.D. from the University of Washington in 2010. Her goal in life is to throw expensive s**t in the ocean. When not at sea, she uses observations from moored, satellite and land-based instruments to understand the pathways that wind and tidal energy take from large (internal tides) to small scales (turbulence).





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