Out of order response,
sea slug said:
Does this delay have anything to do with tidal bulges and despinning of the moon?
I'm dealing with this first (I'll get to the delay later) because this question represents a bit of an oversimplification on the part of the educational system. In a sense, there is no such thing as a tidal bulge, at least not in the sense taught in schools. There
would be a tidal bulge
if the Earth wasn't rotating and if Earth had no land and was instead covered by a very deep ocean. There are several reasons why this simple model is just too simple:
- Eurasia+Africa+Australia and North+South America, that block the flow of this tidal bulge.
- The oceans aren't deep enough to sustain a surface wave moving at 460 km/hr. Such a wave would require an ocean depth of 22 km or more.
- The sub-lunar point moves at 460 km/hr (at the equator) because the Earth is rotating. This means the Coriolis effect comes into play. Even if the continents were gone and the ocean was 22 km deep, there still wouldn't be a tidal bulge of the simple sort depicted in schools and across the 'net.
The animated gif provided by granpa (previous post) shows a better model of the tides based on modern remote sensing data and the not so modern Laplace's Tidal Equations. Can you see the tidal bulge in that image? What you see is a set of gyres rotating around various amphidromic points. The image below depicts the M
2 tidal (the principal lunar semidiurnal component of the tides) amphidromic systems. Click on the image for an enlarged version.
http://www.aviso.oceanobs.com/uploads/pics/200010_m2_amp_pha_fes99_sm.gif
So what about the tidal bulges? They appear as residual components if you look at things from the perspective of a frame in which the Earth and Moon are fixed and average out ocean heights over time and over latitude -- and they are small, about 3 or 4 centimeters high.
Now to answer your question in full.
sea slug said:
Hi,
I'm an old biologist/naturalist who loves to go tidepooling, so this is not a homework question. Why do the lowest tides follow the full moon by a few days? For example, the "super" full moon of yesterday March 19, will pull the lowest tides (here in Maine) on
Monday and Tuesday March 21 & 22.
Saturday March 19th 4:46 am -1.3 5:11 pm -1.5
Sunday March 20th 5:37 am -1.9 5:59 pm -1.6 (talk about spring tides! ha ha)
Monday March 21st 6:28 am -2.1 6:48 pm -1.5
Tuesday March 22nd 7:19 am -2.0 7:38 pm -1.0
Wednesday March 23 8:13 am -1.6
Does this delay have anything to do with tidal bulges and despinning of the moon?
Thanks!
Lynn
This has nothing to do with the tidal bulges and the despinning of the moon. There are multiple frequency components to the tides due to the tides being caused by the Moon and the Sun and by interactions between the tides, the depths of the oceans, and the geography of the coasts. The best way to describe the tides for a given location is to perform a Fourier analysis of the historical observations the tides at that location. The result of this analysis will attribute the tides at the location as amplitudes and phases the various components of the tide (principal lunar semidiurnal (12.42 hour period), lunisolar diurnal (22.93 hours), principal solar semidiurnal (12 hours), principal lunar diurnal (25.82 hours), etc.). This attribution is strictly empirical and applies only to the given location. It is however extremely accurate in terms of predictability.
Those amphidromic systems can get quite complex. For example, it is always high tide somewhere in the North Sea due to the presence of three amphidromic points in the North Sea / English Channel.