<p>Yes, the speed of currents varies with depth.</p>

<p>In the case of shallow, coastal water, the flow is retarted by friction at the seabed, so it is slowest at the seabed and usually has a curve of increasing speed towards the surface.</p>

<p>This curve can theoretically be calculated, but in practice it is very sensitive to things like the material and shape of the seabed, wind and waves near the surface, and so forth, so while estimates can be made from theory, it's usually better to measure it. </p>

<p>Approximations are often made using a "power law" such as </p>

<p><span class="math-container">$u_1 = u_2 \left( \frac{z_2}{z_1} \right)^{\frac{1}{\alpha}}$</span></p>

<p>where <span class="math-container">$u_1$</span> and <span class="math-container">$u_2$</span> are the speeds at distances <span class="math-container">$z_1$</span> and <span class="math-container">$z_2$</span> above the seabed respectively, and <span class="math-container">$\alpha$</span> is an arbitrary value often between 5 and 7.
This figure, from <a href="http://doi.org/10.1016/j.renene.2017.03.096" rel="nofollow noreferrer">Lewis et al. 2017</a> (creative commons licensed), illustrates a number of such theoretical curves with different values of <span class="math-container">$\alpha$</span>.</p>

<p><a href="https://i.sstatic.net/oe5VM.jpg" rel="nofollow noreferrer"><img src="https://i.sstatic.net/oe5VM.jpg" alt="enter image description here"></a></p>

<p>In deeper oceans this mechanism will only apply close to the seabed; however, far more complex systems can come into play, with different water bodies moving in (potentially) different directions. Possibly others with more expertise in ocean dynamics can address that case.</p>

CC BY-SA 4.0
2018-12-04T11:34:53.570Z
2018-12-04T11:34:53.570Z
Semidiurnal Simon
<p>How much speed of surface currents decrease in ocean depth? Approximately? I am wondering if there is any significant gradient within the top 30m ocean layer? Can this be theoretically calculated?</p>

CC BY-SA 4.0
2018-12-03T20:05:39.790Z
"Can this be theoretically calculated?" Sure, depends on what you assume for the boundary conditions and scales involved..
AtmosphericPrisonEscape
CC BY-SA 4.0
2018-12-03T21:45:41.733Z
Are you asking for typical values of such gradients in practice, or the physics for where there is such difference?
JeopardyTempest
<ocean-currents>
Velocity gradient of surface ocean current in dephts
pen
# Velocity gradient of surface ocean current in dephts

(Asked by: username_0 on 2018-12-03)

How much speed of surface currents decrease in ocean depth? Approximately? I am wondering if there is any significant gradient within the top 30m ocean layer? Can this be theoretically calculated?

**Tags:** ocean-currents

> **Comments:**
> **username_1**: "Can this be theoretically calculated?" Sure, depends on what you assume for the boundary conditions and scales involved..  
> **username_2**: Are you asking for typical values of such gradients in practice, or the physics for where there is such difference?  

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## 1 answers

### Answer by username_3 on 2018-12-04. Score: 3

Yes, the speed of currents varies with depth.

In the case of shallow, coastal water, the flow is retarted by friction at the seabed, so it is slowest at the seabed and usually has a curve of increasing speed towards the surface.

This curve can theoretically be calculated, but in practice it is very sensitive to things like the material and shape of the seabed, wind and waves near the surface, and so forth, so while estimates can be made from theory, it's usually better to measure it.

Approximations are often made using a "power law" such as

$u\_1 = u\_2 \left( \frac{z\_2}{z\_1} \right)^{\frac{1}{\alpha}}$

where $u\_1$ and $u\_2$ are the speeds at distances $z\_1$ and $z\_2$ above the seabed respectively, and $\alpha$ is an arbitrary value often between 5 and 7.
This figure, from [Lewis et al. 2017](http://doi.org/10.1016/j.renene.2017.03.096) (creative commons licensed), illustrates a number of such theoretical curves with different values of $\alpha$.

[![enter image description here](https://i.sstatic.net/oe5VM.jpg)](https://i.sstatic.net/oe5VM.jpg)

In deeper oceans this mechanism will only apply close to the seabed; however, far more complex systems can come into play, with different water bodies moving in (potentially) different directions. Possibly others with more expertise in ocean dynamics can address that case.


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