Difference between revisions of "Tidal excursion"

From Coastal Wiki
Jump to: navigation, search
(Created page with " {{ Definition| title = Tidal excursion | definition = the average distance travelled by tidal flow between low-water slack tide and high-water slack tide.}} ==Notes== *The...")
 
 
Line 7: Line 7:
 
==Notes==
 
==Notes==
 
*The influence of river runoff on the travelled distance is not included in the tidal excursion.
 
*The influence of river runoff on the travelled distance is not included in the tidal excursion.
* Slack tide is the time at which the tidal current (i.e. the tidal component of the current velocity)  is smallest.
+
* Slack tide is the time at which the tidal current (i.e. the tidal component of the current velocity)  is smallest. Slack tide occurs twice during a tidal cycle. In coastal waters (flow influenced by friction and boundaries), one slack tide occurs closer to low water (low-water slack tide) and another slack tide occurs closer to high water (high-water slack tide).
 
 
  
 +
 
The tidal excursion <math>L</math> is given by the formula
 
The tidal excursion <math>L</math> is given by the formula
  

Latest revision as of 17:00, 24 June 2023


Definition of Tidal excursion:
the average distance travelled by tidal flow between low-water slack tide and high-water slack tide.
This is the common definition for Tidal excursion, other definitions can be discussed in the article


Notes

  • The influence of river runoff on the travelled distance is not included in the tidal excursion.
  • Slack tide is the time at which the tidal current (i.e. the tidal component of the current velocity) is smallest. Slack tide occurs twice during a tidal cycle. In coastal waters (flow influenced by friction and boundaries), one slack tide occurs closer to low water (low-water slack tide) and another slack tide occurs closer to high water (high-water slack tide).


The tidal excursion L is given by the formula

L = \int_{t_{LSW}}^{t_{HSW}} u(X(t),t) \; dt ,

where u(x,t) is the tidal component of the current velocity averaged over the channel cross-section, X(t) is the position of a water parcel moving with velocity u(X(t),t), starting from x=0 at t=t_{LSW} (low-water slack tide, LSW), and arriving at x=L at t=t_{HSW} (high-water slack tide, HSW).

If \quad u(t)=U \sin \omega t ,

meaning that the current velocity does not depend on x and that the tide is sinusoidal with period T=2 \pi / \omega, then

\quad L=2 U / \omega.