<p>I'm posting this as an answer rather than a comment to expand a bit on the excellent answer from Isopycnal Oscillation and note some minor differences I observed.</p>

<p>I had actually looked for temperature and temperature anomaly differences in the middle of the eddies and didn't see them prior to posting the question so it didn't look like upwelling at first. Here is an image from 2015-10-12 That shows some interesting features.</p>

<p>The areas of positive and negative anomalies actually include several eddies. This is particularly noticeable in the red/yellow areas which seem to be strengthening - there were more groups of blue a few days ago and little yellow. So it appears the vertical motion covers a larger area than individual mesoscale eddies. Is that correct?</p>

<p>The other thing to notice is that the yellow - high positive anomaly is aligned with the high surface current around the eddies, not in the centre. I'm not sure why that is, but seems to indicate that the eddy currents are being driven by the temperature/flow differences between them.  </p>

<p><a href="https://i.sstatic.net/90XNx.jpg" rel="nofollow noreferrer"><img src="https://i.sstatic.net/90XNx.jpg" alt="Tasman Sea Temperature Anomaly and Currents"></a> </p>

CC BY-SA 3.0
2015-10-12T02:36:09.153Z
2015-10-12T02:36:09.153Z
haresfur
<p>Great question. These features are mesoscale Eddies and they are akin to hurricanes in the atmosphere. They are the ocean’s high or low pressure systems and are the result of instabilities. The cyclonic eddy (counterclockwise direction in the northern hemisphere) is called a cold-core eddy and the anti-cyclonic eddy is called a warm-core eddy.</p>

<p><a href="https://i.sstatic.net/kri9D.gif" rel="noreferrer"><img src="https://i.sstatic.net/kri9D.gif" alt="enter image description here"></a></p>

<p>Unlike destructive hurricanes, ocean eddies are important physical processes for the transport of heat and particulate matter. They stir up the ocean drawing up nutrients from the lower depths and fertilizing waters as they propagate. They are important for the transport of marine organisms in the offshore direction and support phytoplankton and zooplankton production.</p>

<p>In the Tasman sea, this region is known as 'Eddy Avenue' which speaks to their ubiquity and persistence. In Everett (2012) they identified 30 thousand eddies in a period of $15$ years.</p>

<blockquote>
  <p>... at a density of 61 cyclonic and 63 anticyclonic eddies per $10,000$
  km$^2$. On any given day there are 16.8 cyclonic and 17.8 anticyclonic
  eddies within the Tasman Sea. Tasman Sea eddies are typically smaller
  than the global average ($82$ km radii compared with $86$ km), have a
  faster rotational speed ($23$ cm s$^{-1}$ compared with $15–16$ cm
  s$^{-1}$) and have a larger Sea Level Anomaly($10$ cm compared with
  $6–7$ cm) (Table 1).</p>
</blockquote>

<p>Generation:</p>

<blockquote>
  <p>“When the current separates from the coast, it gets complicated. It
  starts to wobble; it meanders. Rather than going in a relatively
  straight path like the Gulf Stream in the North Atlantic, it walks
  like a drunk man.” Not only does the EAC wobble, it U-turns. [...] The EAC is a bit  anomalous.” About two-thirds of the current retroflects back up into
  the eastern Pacific, breaking up the EAC further. “It really is a
  current of eddies.” Such instabilities saturate Eddy Avenue with
  eddies.</p>
</blockquote>

<p>As far as the El-Niño connection, I can only speculate. But generally, El-Niño will give rise to positive SST anomalies. The figure below shows recent positive SST anomalies which are relatively strong near the coast. Because ocean temperatures are higher ocean eddies can increase in size and strength. </p>

<p><a href="https://i.sstatic.net/2ZryR.png" rel="noreferrer"><img src="https://i.sstatic.net/2ZryR.png" alt="enter image description here"></a></p>

<p><strong>References</strong></p>

<p><a href="http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.363.5897&amp;rep=rep1&amp;type=pdf" rel="noreferrer">Everett, J. D., M. E. Baird, P. R. Oke, and I. M. Suthers. 2012. An avenue of eddies: Quantifying the biophysical properties of mesoscale eddies in the Tasman Sea. Geophysical Research Letters 39, L16608, doi:10.1029/2012GL053091.</a></p>

CC BY-SA 3.0
2015-10-09T18:27:46.127Z
2015-10-09T19:34:58.450Z
2015-10-09T19:34:58.450Z
Isopycnal Oscillation
<p>I was looking at the model ocean current maps from <a href="http://earth.nullschool.net/#current/ocean/surface/currents/overlay=sea_surface_temp/orthographic=153.77,-31.32,2274" rel="noreferrer">earth :: a global map of wind, weather, and ocean conditions</a> for 2015-10-07 00:00 UTC and there are a lot of odd-looking 'whirlpool' areas off the eastern coast of Australia. Anyone know the explanation? Is this a common occurrence? Is it related to the strong El Niño?</p>

<p><a href="https://i.sstatic.net/qAeJc.jpg" rel="noreferrer"><img src="https://i.sstatic.net/qAeJc.jpg" alt="Ocean currents off Australia"></a></p>

<ocean><oceanography><ocean-currents><enso><pacific>
What causes these odd-looking currents in the Tasman Sea?
haresfur
# What causes these odd-looking currents in the Tasman Sea?

(Asked by: username_0 on 2015-10-09)

I was looking at the model ocean current maps from [earth :: a global map of wind, weather, and ocean conditions](http://earth.nullschool.net/#current/ocean/surface/currents/overlay=sea_surface_temp/orthographic=153.77,-31.32,2274) for 2015-10-07 00:00 UTC and there are a lot of odd-looking 'whirlpool' areas off the eastern coast of Australia. Anyone know the explanation? Is this a common occurrence? Is it related to the strong El Niño?

[![Ocean currents off Australia](https://i.sstatic.net/qAeJc.jpg)](https://i.sstatic.net/qAeJc.jpg)

**Tags:** ocean, oceanography, ocean-currents, enso, pacific


---

## 2 answers

### Answer by username_1 on 2015-10-09. Score: 10 | Accepted answer

Great question. These features are mesoscale Eddies and they are akin to hurricanes in the atmosphere. They are the ocean’s high or low pressure systems and are the result of instabilities. The cyclonic eddy (counterclockwise direction in the northern hemisphere) is called a cold-core eddy and the anti-cyclonic eddy is called a warm-core eddy.

[![enter image description here](https://i.sstatic.net/kri9D.gif)](https://i.sstatic.net/kri9D.gif)

Unlike destructive hurricanes, ocean eddies are important physical processes for the transport of heat and particulate matter. They stir up the ocean drawing up nutrients from the lower depths and fertilizing waters as they propagate. They are important for the transport of marine organisms in the offshore direction and support phytoplankton and zooplankton production.

In the Tasman sea, this region is known as 'Eddy Avenue' which speaks to their ubiquity and persistence. In Everett (2012) they identified 30 thousand eddies in a period of $15$ years.

> ... at a density of 61 cyclonic and 63 anticyclonic eddies per $10,000$
> km$^2$. On any given day there are 16.8 cyclonic and 17.8 anticyclonic
> eddies within the Tasman Sea. Tasman Sea eddies are typically smaller
> than the global average ($82$ km radii compared with $86$ km), have a
> faster rotational speed ($23$ cm s$^{-1}$ compared with $15–16$ cm
> s$^{-1}$) and have a larger Sea Level Anomaly($10$ cm compared with
> $6–7$ cm) (Table 1).

Generation:

> “When the current separates from the coast, it gets complicated. It
> starts to wobble; it meanders. Rather than going in a relatively
> straight path like the Gulf Stream in the North Atlantic, it walks
> like a drunk man.” Not only does the EAC wobble, it U-turns. [...] The EAC is a bit anomalous.” About two-thirds of the current retroflects back up into
> the eastern Pacific, breaking up the EAC further. “It really is a
> current of eddies.” Such instabilities saturate Eddy Avenue with
> eddies.

As far as the El-Niño connection, I can only speculate. But generally, El-Niño will give rise to positive SST anomalies. The figure below shows recent positive SST anomalies which are relatively strong near the coast. Because ocean temperatures are higher ocean eddies can increase in size and strength.

[![enter image description here](https://i.sstatic.net/2ZryR.png)](https://i.sstatic.net/2ZryR.png)

**References**

[Everett, J. D., M. E. Baird, P. R. Oke, and I. M. Suthers. 2012. An avenue of eddies: Quantifying the biophysical properties of mesoscale eddies in the Tasman Sea. Geophysical Research Letters 39, L16608, doi:10.1029/2012GL053091.](http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.363.5897&rep=rep1&type=pdf)


---

### Answer by username_0 on 2015-10-12. Score: 4

I'm posting this as an answer rather than a comment to expand a bit on the excellent answer from username_1 username_1 and note some minor differences I observed.

I had actually looked for temperature and temperature anomaly differences in the middle of the eddies and didn't see them prior to posting the question so it didn't look like upwelling at first. Here is an image from 2015-10-12 That shows some interesting features.

The areas of positive and negative anomalies actually include several eddies. This is particularly noticeable in the red/yellow areas which seem to be strengthening - there were more groups of blue a few days ago and little yellow. So it appears the vertical motion covers a larger area than individual mesoscale eddies. Is that correct?

The other thing to notice is that the yellow - high positive anomaly is aligned with the high surface current around the eddies, not in the centre. I'm not sure why that is, but seems to indicate that the eddy currents are being driven by the temperature/flow differences between them.

[![Tasman Sea Temperature Anomaly and Currents](https://i.sstatic.net/90XNx.jpg)](https://i.sstatic.net/90XNx.jpg)


---

