I have been fighting a well-known problem with the anemometer since I first bought it. It randomly records insanely
high wind gusts (100+ MPH). It was a problem when I was using the AAG software, it was a problem with the WService software,
and it was a problem with my 1-Wire Weather Service for Java. This article describes how I solved the problem.
I have heard a lot of discussion about "contact bounce", in which the reed switches bounce mechanically, causing the
counters to register multiple events for each passage of a magnet. This seems unlikely, since the DS2423 has built-in debouncing
logic, and it is pretty fail-safe (note 13 from the DS2423 data sheet
Each low-going edge on a counter input resets the channel’s debounce timer. The debounce time starts as the input
voltage rises beyond the trip point. In order for the next pulse to be counted the debounce time must have expired.
This means that the DS2423 keeps extending the debounce window until the switch has remained quiet for the debounce time
(170 to 460 microseconds, representing 5.9KHz to 2.2KHz respectively). That is in line with the faint "ping" tone you hear
when the switches turn on.
What I thought might be contact bounce in the magnetic reed switches, or problems with the MicroLan, or problems with
the power supply, or radio interference, might just be a timebase problem. I wrote my software to detect and filter out the
insanely high gusts, but I was never satisfied with that solution, particularly since my filter could lop off some legitimate
gusts in the process. So I built a "flight recorder" that records a running history of ten samples, along with collection
times. When the filter detects an out of range sample, it records five more samples, for a total of five samples before and
five samples after the out-of-range sample.
I captured a few of these events. Instead of an unusual jump in the spin counter data, I
found a gap in the timebase: The anemometer task thread got suspended at a critical time (i.e., between reading the anemometer
spin counter and reading the current time). While the thread is suspended, the anemometer continues to spin, and the counter
continues to count. We calculate the RPM, which reads low because we have a long time interval and a low count. But look out
for that next sample! If it starts at the scheduled time, it will be shorter than usual, and the count will include all the
rotations that occurred while the thread was suspended during the previous sample. Here is an example:
Spin Counter History Buffer
8: 1137475009667 5662 5664
9: 1137475014283 5667 5668
0: 1137475018309 5707 5710
2: 1137475019150 5752 5752
3: 1137475019381 5754 5754
4: 1137475019461 5755 5755
1137475019551 5756 5755
6: 1137475019641 5757 5756
7: 1137475019741 5758 5757
The first column is the buffer index. The second column is the system time in milliseconds since January 01, 1970 UTC.
The third and fourth columns are the spin counter values. (Each counter is connected to a separate magnetic reed switch. The
counts may differ slightly depending on where the magnet is when the count is sampled. The choice of which one to use for
wind speed calculations is arbitrary.)
Note the interval between index 9 and 0. The elapsed time is nearly 4000 milliseconds (4 seconds), while the count increased
by only 40. The thread got suspended for nearly 4 seconds. The interval between 0 and 1 was a mere 651 milliseconds, but the
count increased by 40 again. Since the rotor RPM is expressed as
rotorRPM = (((count – prevCount) * 60000 / n) / (msec –
where n is the number of magnets in the instrument (2), the RPM for the first interval was calculated as 300,
whereas the RPM for the second interval was calculated as 1843. Those correspond to wind speeds of 12 MPH and 75 MPH, respectively.
The average wind speed at that time was about 11 MPH.
The wind speed obtained by plugging in the times and counts
from the first and last entry calculates to about 12 MPH, so the overall counts and overall times are correct. If the anomaly
had been due to contact bounce, the overall calculation would have been much higher.
I chose a timing tolerance of plus or minus 20% of the nominal sampling interval,
and the time to access the sensor may not exceed 20% of the nominal sampling interval. If the measured interval exceeds this
tolerance, I throw an exception, and try again next time.
Insanely high wind readings can also be caused by automatic time synchronization with an internet or domain time server.
If the on-board clock drifts too much between synchronizations, the resulting stepwise system clock correction can be several
seconds when the system clock is updated. Another source of error is network lag time, which can significantly and unpredictably
delay the time signal coming from the time server.
NTP clients that fully implement RFC1305 - Network Time Protocol
are capable of incremental corrections that chase the time server by adjusting the clock speed instead of performing
a stepwise correction. However, stand-alone Windows computers (ones that are not part of a network domain) are configured
by default to perform only stepwise corrections, on the assumption that they do not have continuous access to an NTP server.
By tweaking the registry, you can make it do incremental corrections, which are not as disruptive. Please refer to my tech notes page
for how to do this.