oh my - thank you for all that information everyone.
I was thinking of a budget of $300-$400.. Is that too unreasonable? Do I need to consider spending a lot more?
I am in New Mexico and just about anything I put out on my
property gets destroyed by the sun. (So I would need a radiation
shield?) I'm a serious gardener and interested in weather.
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Specific to the ET calculation, I think the reason is correlation of the parametric readings. When you’re building a calculated value from a bag of parametric values it’s important to be sampling the same environment. You’d have a similar problem with a calculated dew point if there was too much distance between the temp sensor and humidity sensor. You would expect there to be a lot of difference between winds at 10 meters and the movement of air that’s protected by a grove of trees or a stand of corn, and what’s relevant for ET is the airflow over the leaves of the plant - whatever is happening at 10-meters is not likely to be relevant, although it likely will be relative.
So, ET air movement is really completely different than meteorological surface winds; the only thing they have in common is the instruments they can be measured with, but they are two different parameters. Just as indoor air temperature and outdoor air temperature are both measured with a thermometer, but obviously represent different things. What matters is what the thing is vs. what you're passing it off as.
What's magic - not really - about 10-meters is it's considered to be more "undisturbed". Yes, it will be disturbed by terrain features, but not as much by man-made structures. I can take a dataset and a topographic map and build a model that has a good fit. But if I start taking lower readings and start building man-made structures the model becomes impossibly complex and "R" (goodness of fit) goes to hell.
Also, due to surface friction you'd need to apply a correction value if you take wind readings at an elevation other than 10-meters. Going back to the, "Modeling the Variation of Wind Speed with Height for Agricultural Source Pollution Control" paper, and using the Power Law model, wind speed of 4.75 m/s taken at 2-meters (6.6') would need to be transformed to ~8.1 m/s in order to submit it as meteorological surface winds. This is because another thing that's magic about 10-meters is the drag transfer function (skin, form and gravity wave drag). Just like pressure: we never report Station Pressure, we always at least add an altitude correction.
Now, if you're in the rocky mountains you've got a whole other thing going on: dynamic viscosity. Air is much less dense at 3,000 feet than it is at MSL, so the drag has less of an effect on the lower viscosity air. But since the station elevation is part of the metadata we can further transform wind using elevation, temperature, and humidity as long as we were provided with TRUE meteorological surface wind taken at, or at least corrected to, 10-meters. Ten meters is magic in that some transfer functions assume that constant where the height of the measurement is germane to the calculation. If you supply something different then the transfer function becomes garbage in, garbage out.
Sending MSLP to CWOP is largely an education issue, and then a software one. First someone needs to be educated to understand their software, which they trust, is getting it wrong. Then there's the matter of how to hack it so it's right, because the problem is not usually the result of a wrong configuration value that can simply be changed. All of which is moot unless there is a desire and willingness to do something about it. All we can really do is education outreach and hope for the best.
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