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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#1
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Thanks very much Stephen (and Will for pi!). I will have a go at this, as I
reckon I have a 20% underread compared to a manual guage here. Phil |
#2
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Can I add just a small word of caution here. First, I wouldn't
recommend anyone altering the screw settings on their Davis rain gauge unless they're really convinced that it is misreading significantly and have completely ruled out other possible explanations. Often an apparent miscalibration has another explanation, eg the gauge increment is not correctly set on console or software or the reference rainfall readings are not properly comparable, which can be for a variety of reasons.And in practice it's pretty difficult to return the screw heights exactly to their factory settings once altered if you subsequently decide that the error wasn't as great as you initially thought and you didn't keep an accurate record of any changes that were made. In general the VP2 gauges do record reasonably accurately though like all less costly TBRs will inherently tend to under-record slightly and will typically be mounted at eg 4ft height rather than at ground level, so exaggerating this tendency a little. That said, I suspect that there was a particular batch of VP1 gauges that were mis-calibrated at the factory and this is primarily where the reports of 20% under-recording come from. Finally, I agree - the drip method is a good way of checking the calibration - volume figures for the Davis gauges can be found on our website towards the bottom of the page at: http://www.weatherstations.co.uk/vp_faqt2.stm (NB Apologies - this page is now a few years old and really needs updating soon but the figures are still all correct AFAIK) Don't underestimate the care and patience that's needed to run the drip method reliably - although it's reasonably straightforward to do, things like measuring (or weighing) the total volume of water accurately, not exceeding the suggested drip rate etc all need attention. Unless you're meticulous with the method, it's still not easy to get a precision on repeat calibration runs of better than 4-5%. John Dann www.weatherstations.co.uk |
#3
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In message , Phil Layton
writes Thanks very much Stephen (and Will for pi!). I will have a go at this, as I reckon I have a 20% underread compared to a manual guage here. Phil Repeated thanks to all, particularly Stephen Burt and John Dann. In tests, it took about 40 mins for 500ml to run through my improvised feed and the result? Well, calculations said that 500ml should translate into 23.64mm and the average of two runs was 23.1mm - close enough for my peace of mind. That still leaves me wondering at the 20% anomaly - the other gauge (1m away and 0.6m lower) checked out as accurate too. Can that separation cause such a large disparity? Anyway, it all goes to prove that John Dann's advice about not twiddling anything until error is proven! -- Chris |
#4
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Just one correction to my own message...
Well, calculations said that 500ml should translate into 23.64mm That should read 23.38mm -- Chris |
#5
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![]() "Zak" wrote in message ... In message , Phil Layton writes Thanks very much Stephen (and Will for pi!). I will have a go at this, as I reckon I have a 20% underread compared to a manual guage here. Phil Repeated thanks to all, particularly Stephen Burt and John Dann. In tests, it took about 40 mins for 500ml to run through my improvised feed and the result? Well, calculations said that 500ml should translate into 23.64mm and the average of two runs was 23.1mm - close enough for my peace of mind. That still leaves me wondering at the 20% anomaly - the other gauge (1m away and 0.6m lower) checked out as accurate too. Can that separation cause such a large disparity? Hi Zak. In a word - yes!!! If you look back through British Rainfall at the beginning of the 20th Century when folk were trying to decide on best gauge design and site, it was quickly concluded that elevated gauges would under-read due to air currents deflecting rain and greater exposure to wind generally. I have exactly the same problem as you my Davis reads 20% lower than my rain gauge 2m away and just over 1m lower. Cheers, Will -- |
#6
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![]() The strange choice of an elevated design of these Davis AWS gauges will lead to under-reading owing to wind eddying effects, as Will correctly points out. The difference between this type of gauge and a standard adjacent checkgauge (rim at 30 cm) will vary significantly with both site and weather conditions, so a windy wet day in an exposed site will lead to greater losses than a day's rain with light winds - the differences could then be expected to vary from almost nil to perhaps 30% or more, and adjusting the tip capacity may not be the right answer. Sheltered sites may see much smaller differences between these gauges and a standard checkgauge - but of course both may be under-recording if the site is seriously under-exposed, particularly to the main rain- bearing winds. I'd suggest before tinkering with the calibration settings themselves: 1. Maintain a standard five-inch checkgauge in a reasonable exposure to provide the benchmark against which to judge the accuracy of the tipping-bucket readings. They're not expensive, perhaps £150 for a new one, less second-hand (check on e-bay): it'll last 50 years with a bit of care. Don't forget the measuring cylinder too. 2. Do the drip test as outline in my earlier post. If this comes out OK, and 5% is probably the limit of accuracy without laboratory equipment, look elsewhere for the reasons for any under-reading. 3. If your exposure is limited, check the readings from your checkgauge with that of a local gauge in a standard location. Readings can vary significantly over short distances in hilly locations, and in showery situations, so compare over weeks and months rather than days. There's enough COL sites in the major population areas to get an idea of the true fall in your locality, or ask for help on this site. If you feel your readings show a previously unsuspected dry spot in your neighbourhood, check against large-scale average annual rainfall maps. If your percentage of average over 3-6 months is significantly different from nearby gauges, your gauge is under-reading, probably owing to sheltered exposure. 4. If the checkgauge readings look OK, the calibration test is OK and you're still under-reading on your TBR, it's your exposure - most likely the height that's causing the problem. Use the elevated gauge readings only for time/intensity readings and use the checkgauge as the absolute values, or if you want automatic gauge readings to agree more closely, disconnect the elevated gauge and plug in a standalone 0.2 mm unit instead - mounted on the ground. HTH. Stephen Burt Stratfield Mortimer |
#7
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And just to emphasise the points Stephen made about the effect of wind eddies.
My site is well exposed but is often windy and the rain is often dense and fine (many droplets swirling around). Here is a comparison for annual rainfall of Davis AWS (1.4m above ground) versus manual 5" check gauge on the ground in short grass. 2005 AWS 1263 mm Gauge 1406 mm (9% deficit with AWS) 2006 AWS 1333 mm Gauge 1544 mm (14% deficit with AWS) I'll have to live with that, using the manual gauge for the definitive record and the AWS for recording interesting rainfall event timings etc. Will (Haytor, Devon, 1017 feet asl) -- |
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