I frequently see challenges to the US temperature record that claim that many stations are affected by poor station sighting, and that biases introduced by poor station siting may account for a significant fraction of observed warming in the US. The claim is that a significant number of stations located near asphalt or at airports or too close to buildings can cause thermometers to record artificially high temperatures, adding spurious warming trends to CONUS temperature trends.
With the USCRN project, NOAA developed a classification system based on exposure characteristics affecting the siting of stations, and this classification system was retroactively applied to the stations in the old USHCN network by Anthony Watts and surfacestations.org. In this classification system, ratings of 1 and 2 indicate "good siting" and ratings of 3, 4, and 5 indicate "poor siting." These classifications can actually be used to test whether station siting has any impact on CONUS temperature trends, and that's what was done in Menne et al 2010.[1] At the time of publication, 525 stations had been classified, and of them 71 were rated good (1 or 2), while 454 were rated poor. However, the sites with good exposure ratings were well-distributed across CONUS. The study compared both raw and homogenized data from stations with good siting and poor siting to see to what extent the stations differed, and to what extent homogenization corrected differences. It turns out that poor siting had only a small effect on Tmax and Tmin, and with homogenization those differences were corrected in favor of the well-sited stations.

The effectiveness is more clearly seen by comparing trends in Poor-Good sites. The adjusted Tmax and Tmin plots of Poor-Good stations show very little trend remaining.
At the time of publication, NOAA had also just started using the USCRN network, which is an all rural network of 114 well-sited stations. So Menne et al plotted both Tmax and Tmin for USCHN v2 with "all stations" stations with "good siting" and stations with "poor siting" along with about 5 years of data from the USCRN pristine dataset. The results look like this.
If the plots of good vs poor siting were not labeled, you wouldn't be able to tell which was which. The differences between them are minimal, and the trend for the poorly-sited stations is not higher than teh trend for all stations. This seems conclusive evidence that station siting is having very little effect on CONUS temperature trends. The authors conclude, "the adjusted USHCN temperatures are extremely well aligned with recent measurements from instruments whose exposure characteristics meet the highest standards for climate monitoring. In summary, we find no evidence that the CONUS average temperature trends are inflated due to poor station siting."
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We can take this a step further. The USHCN network ha been defunct since 2014; it was replaced by nClimDiv, a homogenized dataset that includes 10,000 stations in the GHCN-daily network, and the USHCN stations are a subset of GHCN-daily. And now in 2025, the all-rural, well-sited USCRN network has 20 years under its belt. If poor siting is causing spurious warming to CONUS trends, this would show up in nClimDiv while being absent from USHCN. So if we compare the two, we can get either definitive confirmation or falsification of the claim that poorly sited stations are adding spurious trends to CONUS temperatures. As you can see above, nClimDiv is not warming more rapidly than USCRN. If anything, USCRN is warming more rapidly.
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In fact, if we compare trends for Jan 2005 to May 2025 in USCRN, nClimDiv, the ERA5 reanalysis and UAH satellite TLT data for CONUS, USCRN is warming marginally more rapidly than all the others. Of the four, only nClimDiv could be affected by poor station siting, yet its trend ranks third, after both USCRN and ERA5 in terms of warming rate. There is simply no case to be made that poor station siting is having a significant effect on CONUS temperature trends.
References:
[1] Menne, M. J., C. N. Williams Jr., and M. A. Palecki (2010), On the reliability of the U.S. surface temperature record, J. Geophys. Res., 115, D11108, doi:10.1029/2009JD013094.
https://www.ncei.noaa.gov/pub/data/ushcn/papers/menne-etal2010.pdf
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