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Gemma Kelly, Alan Thomson
Evaluating the use of geomagnetic indices for identifying potential damage to power grids Gemma Kelly, Alan Thomson
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GICs Geomagnetically induced currents (GICs) are the main space weather risk to power grids We would like a way to categorise GICs, particularly for the UK, to better identify times when the system is at risk. Ideally we could then provide a forecast with a focus on GICs We generally assume GIC is most closely related to dB/dt – how true is this?
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GIC data Not particularly extensive – relies on a close relationship with Scottish power – they don’t save the data so we have to remember to ask for it in a timely manner Max measured ~40A
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dH/dt and GIC So first assumption look like it holds, GIC follows the dB/dt pretty well. Unfortunately…… March 2012 – Torness GIC data (red) against dH/dt at Eskdalemuir (blue)
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dH/dt and known GIC impacts
Storms in red are identified in Erinmez – or in the case of 2003, engineers at the time reported some effect (noise, heating etc) Erinmez et al., J. Atmos. Sol-Terr. Phys. 2002
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Problem Our earlier GIC data need reprocessing
dB/dt at individual stations is very hard to predict (at the moment) We would like to develop an index to identify when there is a risk of large GIC We start by investigating what existing indices GIC (dB/dt) in the UK relates to.
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NOAA G scales and Kp Widely used and recognised
We use them to forecast and to categorise past activity Based on Kp, the 3-hourly geomagnetic index Commonly used – supply forecasts and post-event analysis in terms of Kp – how useful is that for GIC? NG tell us they aren’t concerned until well into G5 – how good an assumption is that? Is that sensible?
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dH/dt and Kp So Kp 8 predicts events in the red zone – but also a lot of times when dH/dt didn’t get larger than 200 in that period At the moment with our current data we don’t know whether any of the other Kp 8 or 9 events caused lesser effects in the power grid (maybe later on or degradation rather than instant effects)
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Max dH/dt at 24 observatories
dH/dt and Kp 24 observatories with >16 years data Largest dH/dt at Kp = 9o for only 8 of 24 observatories. dH/dt > 1000nT/min was measured at 4 observatories: BRW, ABK, ESK and FCC (all > ±57° geomag latitude) Max dH/dt at 24 observatories Selection of global observatories with at least 16 years of data Important to note that the largest variations in X and Y do not always occur on the same dates. Unsurprisingly a mid-latitude measure of activity not great for near poles
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dH/dt and K Regional K better – in that it at least identifies all events as K=9….but still a large range of dH/dt at K=9
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dH/dt and AE AU AE AO AL 1 minute AE against 1minute dB/dt
AL is westward electrojet AU eastward
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dH/dt and AL Interesting that we only see dH/dt > 600 when AL is small – is this a sign that the auroral oval has moved too far south of the AE stations?
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dH/dt HSD Hourly standard deviation – rolling for last hour
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So how does this help? We can try using some thresholds to see if that helps narrow down times of increased GIC, for example: Kp > 8 AL > -1000 HSD > 100
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Selected data We identify all the storms with dH/dt > 600nT/min
Fewer times identified where there is no large dB/dt at some point during the storm
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Future work = GIC measuring location Reprocess the GIC data we hold and repeat and expand the process with that do the other indices add value to dB/dt? Build regression relationships between GIC and other variables Better proxy than ‘just’ dB/dt Forecasts and validation? Do something similar with NZ data? Comparative study, similar latitudes Investigate whether the dB/dt at Esk is best for UK GIC or whether some combination of data from UK observatories is better
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Quiet High GIC risk Medium risk
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Very simple approach => large number of false alarms
All data Points Accuracy (fraction correct) = correct/total = ( )/ = Predicted Observed No storm Storm 7433 storm 8 False alarm ratio = false alarms/(hits + false alarms) 7433/( ) = Max per day Predicted Observed No storm Storm 10888 66 storm 4
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