Hello,

is it possible to share the code how you calculated NZavg in the weewx? Did
you extend aggregation type with xtypes?

Thanks for reply :)

st 29. 3. 2023 v 22:37 odesílatel 'Peter Fletcher' via weewx-development <
[email protected]> napsal:

> It certainly does depend on what you want to do with the numbers.
>
> Like you, I have solar panels, and, also like you, I monitor them
> separately from my weewx installation. If all you want to do is keep a
> check on total (potential) energy influx, then 24-hour averaging and using
> the sort of calculation you suggest, will work perfectly well, though it
> won't take account of the fact that solar panels are generally tilted and
> face in a specific direction (ideally between SE and SW), while most
> standard weather station radiation sensors are designed to be pretty much
> equally sensitive to radiation coming from anywhere in the sky. OTOH, if
> you want to get total energy from daytime-only averages, you just need to
> make sure that you have counted how many samples you have, so you haven't
> really lost any information. My problem with simple 24-hr averaging is that
> if you want to know 'how bright it was' on a past date, and you use simple
> averaging, winter days won't get a fair shake, because, even if the sun was
> shining out of a clear sky all day, there will be a lot more zeroes
> contributing to the average and the average radiation number will be
> disproportionately lower than I feel it 'should be'. I suppose that the
> question I am asking and answering is: "What was the average radiation
> level *during the day*?". I know it was zero at night!
>
> For UV, I think you are right about showing minutes per day above a
> specified level (or perhaps two different ones) being more useful than any
> sort of average, though here, too I think there is an argument for
> averaging (if that is what you are going to do) only during the day.
>
> On Tuesday, March 28, 2023 at 3:43:26 AM UTC-4 Cameron D wrote:
>
>> The obvious question is what you need to do with the numbers.
>> I have solar panels and I log the values separately so I don't use weewx
>> for that - I got the weather station partly to help understand my PV
>> output.  The important long-term values to me are total energy over the
>> day/month/etc.  So, if I was needing to use weewx values of max or mean to
>> plot how things were going then I suppose I would go for the 24-hour
>> average.  The summation of W/m2 over the day scales to the total energy
>> generated - assuming your time interval is fixed and every value is
>> recorded. So for a 5 minute interval, multiply the W/m2 value by 300 will
>> give you J/m2.
>> In the same way, because you should have a fixed number of samples per
>> day, the 24-hour average also scales to total energy.  However, if you only
>> use daylight or non-zero values then you are adding another variable and it
>> carries less meaning - if total energy is important to you.
>>
>> As for UV, since I live in skin cancer central, I would be mainly
>> interested in the high values.  Any average would be pretty useless to me,
>> unless it is, for example, an average between 9:00 and 15:00 (or 3 hours
>> either side of solar zenith.)  A better long-term value might be minutes
>> per day above index 10, 11 or 12.
>> I was not even sure an arithmetic mean of a UV index was valid, but
>> having had a quick look at the derivation of the index, I think it is OK.
>>
>> On Tuesday, 28 March 2023 at 12:37:18 am UTC+10 Peter Fletcher wrote:
>>
>>> I'm trying to start a discussion - not an argument! The fact that no-one
>>> has come up with a way of displaying historic radiation readings that a
>>> consensus of weather experts thinks is better than a simple average
>>> strongly suggests either that no-one thinks that the issue is that
>>> important, or that there is no one right answer - probably a bit of both.
>>> You can and should use whatever approach is most meaningful for you. In
>>> fairness, however, your temperature analogy really does not fly - maximum
>>> daily temperatures correlate much better with mean temperatures that is
>>> true for radiation values, but max temps are independently more 'important'
>>> than max radiation values. This is, of course, partly because it is very
>>> rare for a max temp to be a single isolated value in the way a max
>>> radiation reading may frequently be.
>>>
>>> I have switched my annual charts of both UV and Solar Radiation to show
>>> 'daytime averages', as previously described. I have attached images of both
>>> pairs of charts - 'old' uses simple averaging; 'new' uses daytime
>>> averaging. The maximum values are substantially higher in the latter, but
>>> the overall patterns are not hugely different. The higher maxima 'feel'
>>> better to me, but I certainly would not go to the wall for 'my' way of
>>> doing things.
>>> On Sunday, March 26, 2023 at 11:33:09 PM UTC-4 [email protected]
>>> wrote:
>>>
>>>> Where I live, with the hardware I use, in my understanding, it is
>>>> useful: in addition to the information how much energy from solar radiation
>>>> your location got over the day, you can tell if was clear at least for some
>>>> time that day, or not. So if you say "where I live, fairly high spikes on
>>>> otherwise cloudy days are common, and days with light to moderate cloud
>>>> cover with significantly lower maxima are also fairly common" that's just
>>>> the point: that's the extra information you get. The fact that you know
>>>> that because you live there is proven with data and if your station is on
>>>> the internet, everyone can know.
>>>> What would you reply to me, if I said: "I not convinced daily maxima
>>>> are particularly useful for temperature. At least where I live, fairly high
>>>> maxima on otherwise pretty cold days are common, and days with moderate
>>>> averages, and maxima not significantly above average, are also fairly
>>>> common"?  Probably you'd say: "That's different", which is true, because
>>>> radiation changes are very like to be more radical than temerature changes
>>>> often, but it is not so much different one might think.
>>>>
>>>> Peter Fletcher schrieb am Sonntag, 26. März 2023 um 22:32:13 UTC+2:
>>>>
>>>>> I'm not convinced that daily maxima are particularly useful for solar
>>>>> radiation. At least where I live, fairly high spikes on otherwise cloudy
>>>>> days are common, and days with light to moderate cloud cover with
>>>>> significantly lower maxima are also fairly common. Simple averages are, at
>>>>> least, somewhat meaningful, and I don't think showing the daily maxima 
>>>>> adds
>>>>> anything to them. Only counting as maxima values that are sustained for
>>>>> more than a specified time might make them more so.
>>>>>
>>>>> On Tuesday, March 21, 2023 at 1:16:48 AM UTC-4 [email protected]
>>>>> wrote:
>>>>>
>>>>>> For myself, I found that for a yearly chart, using a bar chart with
>>>>>> the daily averages, and a crosshair to display the daily maximum, a
>>>>>> comprehensive way to display solar readings.
>>>>>>
>>>>>> Peter Fletcher schrieb am Donnerstag, 16. März 2023 um 00:29:26 UTC+1:
>>>>>>
>>>>>>> In order to look at different ways of presenting solar and UV
>>>>>>> radiation data, I dumped the contents of weewx.sdb to a csv file and 
>>>>>>> used
>>>>>>> Excel to manipulate and chart the relevant data. The attached charts 
>>>>>>> show
>>>>>>> daily averages for solar and UV radiation for four-month summer and 
>>>>>>> winter
>>>>>>> periods in 2021 and 2021/22. More (probably 'simple') averaging would
>>>>>>> probably be done in producing yearly charts for a website, but I 
>>>>>>> thought it
>>>>>>> helpful to get a somewhat more granular picture of the processed data. 
>>>>>>> For
>>>>>>> all the charts and both types of data, 'Avg ...' uses the current
>>>>>>> calculation (simple averaging of all readings for the 24 hr day), 'NZ 
>>>>>>> Avg
>>>>>>> ...' represents the average of all non-zero readings acquired during the
>>>>>>> 24hr day, and 'Day Avg ...' represents the average of all readings
>>>>>>> (including any zeroes) recorded between sunrise and sunset (calculated 
>>>>>>> for
>>>>>>> my location and the date by the standard NOAA method).
>>>>>>>
>>>>>>> For solar radiation, in both seasons, the non-zero and daytime
>>>>>>> averaging methods produce almost identical results (there are only a few
>>>>>>> places where the two lines do not coincide), and the numbers generated 
>>>>>>> are
>>>>>>> a bit more than 1.6 times the simple average numbers in the summer and 
>>>>>>> well
>>>>>>> over twice the simple average numbers in the winter. This additional
>>>>>>> seasonal difference is, of course, a result of the non-zero winter 
>>>>>>> averages
>>>>>>> not being 'diluted' by the zero values from the longer nights. The 
>>>>>>> results
>>>>>>> of the two more complex averaging methods make more sense to me as a 
>>>>>>> way to
>>>>>>> present solar radiation readings for long time-periods. Non-zero 
>>>>>>> averaging
>>>>>>> is computationally simpler and would probably be my preferred way to go.
>>>>>>>
>>>>>>> For UV radiation, the picture is rather different. Here, the simple
>>>>>>> average numbers are again lowest, but the other two averaging methods
>>>>>>> produce substantially different results, with non-zero averaging giving
>>>>>>> (particularly in the winter) results up to three times those generated 
>>>>>>> by
>>>>>>> non-zero averaging. Here, I think daytime averaging makes more sense. 
>>>>>>> As I
>>>>>>> indicated in my earlier post in this thread, I thought that non-zero
>>>>>>> averaging for UV radiation was likely to produce 'average' results that
>>>>>>> were distorted by periods of sunshine during an otherwise cloudy day, 
>>>>>>> and I
>>>>>>> believe that this is a substantial contributor to what is happening 
>>>>>>> here.
>>>>>>> Assuming, however, that stations which have UV sensors generally also 
>>>>>>> have
>>>>>>> solar radiation sensors, it might be computationally simpler to average 
>>>>>>> UV
>>>>>>> radiation readings if/when the accompanying solar radiation values are
>>>>>>> non-zero.
>>>>>>>
>>>>>>> Any thoughts or comments?
>>>>>>>
>>>>>>> On Saturday, March 11, 2023 at 4:05:18 PM UTC-5 Peter Fletcher wrote:
>>>>>>>
>>>>>>>> When looking at some of my 'yearly' charts (see
>>>>>>>> https://fletchers-uk.com/weather/index.html), the other day, I was
>>>>>>>> struck by how low the 'peaks' in the Solar Radiation and UV graphs
>>>>>>>> were.
>>>>>>>> On a sunny day in the summer (yes - we do have such days in
>>>>>>>> Buffalo!), I
>>>>>>>> typically see Solar Radiation numbers above 900 and UV values above
>>>>>>>> 7
>>>>>>>> for at least a couple of hours around solar noon, but the peaks of
>>>>>>>> the
>>>>>>>> yearly graphs barely exceed 325 and 2, respectively. A (very)
>>>>>>>> little
>>>>>>>> thought revealed the reason for this - the longer term charts
>>>>>>>> average
>>>>>>>> the raw values recorded over periods of more than 24 hours (a week,
>>>>>>>> in
>>>>>>>> my case), so the averages displayed on the charts include a large
>>>>>>>> number
>>>>>>>> of entirely predictable nocturnal zero readings. In the depths of a
>>>>>>>> Buffalo winter, it is dark for 15 hours out of the 24, and even in
>>>>>>>> high
>>>>>>>> summer here it is dark for a bit less than 9 hours out of 24.
>>>>>>>>
>>>>>>>> 'Straight' averages are easy to compute, and make reasonably good
>>>>>>>> sense
>>>>>>>> for displaying the majority of weather-related measurements, which
>>>>>>>> typically have no particular diurnal pattern - or, at least, not
>>>>>>>> such an
>>>>>>>> extreme one - but it doesn't seem totally to make sense to use them
>>>>>>>> when
>>>>>>>> you know in advance that there is such a pattern. OTOH, it clearly
>>>>>>>> wouldn't be very useful just to record and display the daily peak
>>>>>>>> values
>>>>>>>> for these measurements, since that would treat otherwise cloudy
>>>>>>>> days
>>>>>>>> during which the sun appeared through the clouds for ten minutes
>>>>>>>> around
>>>>>>>> noon in the same way as days on which the sun shone out of a
>>>>>>>> cloudless
>>>>>>>> sky from dawn to dusk. Some averaging is needed.
>>>>>>>>
>>>>>>>> One possibility that might produce (IMHO) more meaningful results
>>>>>>>> is
>>>>>>>> 'non-zero averaging' - do not count zero values in computing the
>>>>>>>> average. Solar Radiation rarely reads as zero during the day, so
>>>>>>>> the
>>>>>>>> results of this calculation should correspond reasonably well to a
>>>>>>>> daytime-only average. Daytime UV readings, OTOH, are frequently
>>>>>>>> zero if
>>>>>>>> it is reasonably heavily overcast, so 'non-zero averaging' would
>>>>>>>> produce
>>>>>>>> misleadingly high 'average' values on days with variable cloud
>>>>>>>> cover.
>>>>>>>>
>>>>>>>> A second, and, I think, better, possibility would be to explicitly
>>>>>>>> record and average only daytime values for both readings - defining
>>>>>>>> daytime as being between sunrise and sunset for the date and the
>>>>>>>> station's location.
>>>>>>>>
>>>>>>>> It might also be of interest to record and display the average
>>>>>>>> daily
>>>>>>>> number of minutes/hours for which the reading exceeded a particular
>>>>>>>> threshold, and/or the level reached for at least a certain length
>>>>>>>> of
>>>>>>>> time - the thresholds in each case being determined in advance -
>>>>>>>> but
>>>>>>>> computing these results on the fly would likely be more
>>>>>>>> challenging.
>>>>>>>>
>>>>>>>> I am going to be playing with implementing these ideas over time,
>>>>>>>> but I
>>>>>>>> would like to hear others' thoughts.
>>>>>>>>
>>>>>>>> --
>>>>>>>>
>>>>>>>> Peter R. Fletcher <[email protected]>
>>>>>>>> Home Page - https://pfletch.fletchers-uk.com
>>>>>>>>
>>>>>>>> --
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