Episode 12 - "You want to filter out the ducks" Tides
Don't Panic Geocast
English - April 10, 2015 10:00 - 1 hour - 58 MB - ★★★★★ - 45 ratingsNatural Sciences Science Technology computing geology geophysics geoscience physics science talk technology Homepage Download Apple Podcasts Google Podcasts Overcast Castro Pocket Casts RSS feed
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.
Contact us:
Show - www.dontpanicgeocast.com - @dontpanicgeo - [email protected]
John Leeman - www.johnrleeman.com - @geo_leeman
Shannon Dulin - @ShannonDulin
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.
Contact us:
Show - www.dontpanicgeocast.com - @dontpanicgeo - [email protected]
John Leeman - www.johnrleeman.com - @geo_leeman
Shannon Dulin - @ShannonDulin