Episode 12 - "You want to filter out the ducks" Tides

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Apr 10, 2015

Dive into the fascinating world of tides, where gravitational forces of the Sun, Earth, and Moon create mesmerizing patterns. Discover how ocean tides impact commerce and the geological wonders like tidal rhythmites. Unravel the mystery behind tidal measurement techniques, from ancient methods to modern technology. Explore the relationship between the moon's position and Earth's watery rhythms. Plus, engage with creative insights on adapting tools for fieldwork and a quirky physics problem about jumping through the Earth!

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INSIGHT

Tides Shape Earth's Oceans and Geology

Ocean tides result from the gravitational interaction mainly of the Sun-Earth-Moon system.\n- Tides also influence geological sediment layers called tidal rhythmites, highlighting their importance beyond the ocean.

INSIGHT

Understanding Tide Cycles

Tides cycle includes flood tide (rising), high tide, ebb tide (falling), and slack tide (moment of stillness).\n- Tide clocks exist that follow lunar day cycles, showing tides drift about 50 minutes later each day.

INSIGHT

Spring and Neap Tides Explained

Spring tides occur when Earth, Moon, and Sun align, increasing tidal ranges.\n- Neap tides occur at quarter moons when tidal forces partially cancel each other, reducing tidal range.

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Tides pull and deform the surface of the ocean and the surface of the Earth. This week we’ll take a quick tour of tidal forces, address some show feedback, and then talk about a revision on a classic physics problem.

Tides

Tides are a result of gravitational interaction of the Sun-Earth-Moon system, but are of course a factor on many other planets as well.
Gravity is the key to remember and that it varies linearly with mass, but with the inverse square of displacement.

Ocean Tides

The most familiar example is ocean tides. These are important for commerce, safety, and for sedimentary processes.
Sedimentary layers called tidal rythmites
Cool tide visualization from Calculated Images
General cycle is a flood tide raises water levels until high tide. Then an ebb tide takes water back out until low tide is reached. When the tidal stream stops and reverses it is a slack tide.
Generally occur with 24-hour or 12-hour period, can have a complex shape.
Another kind of clock, a tide clock, has been made to show this.
Spring tide has nothing to do with the season.
When planets are aligned, it’s called a syzygy. Word of the week.
A really nice mathematical introduction can be found here.

Tide Gauges

A pole with markings that we read off of
A float and weight on a pulley attached to a paper chart recorder
Pressure gauges or bubbler pressure measurement
Acoustic gauges or radar gauges (time of flight)
There is a whole mess of datums and standards that go into this, but let’s not go there today!
And rocks of course!!

Solid Earth Tide

The same forceings as ocean tides, but we are actually moving the surface of the planet here. Very important for GPS and scientific measurements. Large particle accelerators actually compensate for their deformation.
The largest displacements are around 55 cm!
Needed to explain the Earth’s nutation
Lunar Tidal Heating

Tidal Locking

We can only see one side of the moon because it is tidally locked. It rotates at the same rate that it orbits the Earth.
Checkout the Minute Earth video on tidal locking!

Feedback/Followup

We got an audio suggestion from listener Stacey about Episode 2 (field gear). She suggested attaching your field pencil to a retractable ID clip so you don’t lose it.
John has an update on the Jot Script 2 stylus!

Fun Paper Friday

We’ve all had to solve the classic physics problem of what would happen if you dug a tunnel through the center of the Earth and jumped in. The classic answer has been that you’ll move like a damped oscillator and that your fall will take about 42 minutes. By improving some of the assumptions that are used, that answer has been improved.

Klotz, A. R. (2015). The gravity tunnel in a non-uniform Earth. American Journal of Physics, 83(3), 231–237. doi:10.1119/1.4898780

Show - www.dontpanicgeocast.com - @dontpanicgeo - show@dontpanicgeocast.com

John Leeman - www.johnrleeman.com - @geo_leeman

Shannon Dulin - @ShannonDulin