I often use temperature as an indicator for different water
sources. Surface water, at least in the top meter or so, can vary from frozen
to almost air temperature in the summer and cools from the surface down in
rivers and lakes. The sea may only reach
about 17degrees if your lucky. However groundwater is often much more stable throughout
the year, and a good rule of thumb is that groundwater, at least in Wales is
about 11°C. Groundwater temperatures can be predicted by using the mean annual
air temp (about 10°C) and adding 2-3°C for every 100m depth, so a groundwater
from about 50m or so depth is likely to be around the 11-12°C mark. So armed
with this – and my new toy – a
FLIR C2 hand held thermal camera - I headed out
to some cliff sections nearby.
Identifying groundwater seepages using thermal cameras is
nothing new (
see these slides from the EPA, 2008) however I am not sure it has
been used for cliff face seepage mapping to identify bryophyte habitat/water
supply –but then I could be wrong!
My aim was to see if the new camera could show temperature
differences on a cliff face and perhaps identify groundwater seepages where
tufa was forming (and bryophytes are living). Would this be any use for mapping
or better understanding these habitats?
Below are my first few attempts, which I thought were worth
sharing. The camera does show areas where groundwater seepage is occurring from
the cliff, which correlate with the tufa and tufa mosses.
There are a few
problems; the camera only records the surface temperature and this will change
as soon as the water seeps out of the cliff and starts to equilibrate with the air temperature. In the summer this will have a
warming effect and a cooling effect in the winter – thus choosing when to do
this needs some thought. Perhaps repeat photography is needed throughout the year. The vegetation itself may alter the temperature as could small areas of shade. It would be useful to measure the water temperature in
situ with a good old thermometer however these cliffs are just too dangerous to
stand underneath.
Since reading
Barrys blog about cow pats I thought that thermal imaging would certainly show up the
temperature of the fresh pats quite nicely, I wonder what they look like in the
winter and for how long they maintain a temperature different to the ambient air temp– are they acting as microclimates for bryophytes?
Happy for comments or suggestions.
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DIGITAL
PHOTOGRAPH: Cliff face groundwater seepage (west of Nash Point) with active
tufa formation – Eucladium verticillatum and Didymondon tophaceus type habitat with lots of Maidenhair fern.
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THERMAL PHOTOGRAPH: Cliff face groundwater seepage (west of
Nash Point) with active tufa formation – Eucladium verticillatum and Didymondon tophaceus type habitat with lots
of Maidenhair fern. The wet area is
highlighted nicely (in the blue-purple colour) and is close to the estimated groundwater temperature of 11OC plus a bit as it was a warm day– although the effect of shade and vegetation on temperature
is not known.
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DIGITAL PHOTOGRAPH: same again some Maidenhair fern with tufa bryophytes |
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THERMAL PHOTOGRAPH: again showing up the groundwater seepage areas quite nicely. The seegage in this picture is warmer than the last, not sure why, could be multiple reasons. It is still however much cooler than the air temp on the day about 20oC. |
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