BBS observers recorded about 41% fewer birds that sing at 7 kHz or more after 20 years on a route; route x observer models put this loss into 1966-2025 trends of 446 species
Question: long-serving North American Breeding Bird Survey (BBS) observers record fewer high-pitched birds. Standard trend models use observer-route effects and assume that detection does not drift while one observer serves. How large is the resulting bias in species trends? Data: 130,303 standard BBS runs (2026 release, 1966-2025; 5,319 routes; 10,417 observers), 446 species, song frequencies of Sagar et al. (2024), GHCN_CAMS climate, and the official USGS 1966-2025 trends (CC0). Methods: for each species, conditional Poisson models with (A) route x observer effects, (B) route effects, and (C) route effects plus a tenure term that resets at each observer change; all with year effects. We wrote the plan before we calculated trends. Post-hoc: tenure bins, end-of-service terms, a simulation, and song frequency as an external instrument. Results: the count change per year of tenure was -0.13% below 3 kHz, -0.55% at 3-5 kHz, -1.23% at 5-7 kHz and -2.06% at 7 kHz or more (slope -0.30% per kHz, SE 0.05). After a small gain in the first 2-4 years, counts after 20 or more years on a route were +2%, -8%, -24% and -41% relative to the first run in these classes. The visual control groups (raptors, water birds, swallows, swifts) had no late loss, but their linear drift also decreased with frequency. Model A put all of the drift into the trend (fraction 1.16, 95% CI 0.96-1.44). Its median 1966-2025 trends were 1.7 points per year lower than model C at 5-7 kHz and 0.4 lower below 3 kHz. A minus the drift had no frequency dependence (0.05). In the simulation, model C recovered the true trend and drift. The official USGS trends carried an uncertain part of the drift (0.39, CI -0.27 to 0.77); the pre-specified tests did not find it. Cold-adapted species had more drift (+0.053% per year per 1 C), which gives a false CTI warming of about 0.04 C per 10 years of tenure. With the drift removed, cold-adapted species did not decline more than warm-adapted species. Limitations: observer ages are not known; tenure is a proxy; the correction assumes no cohort-specific detection; a frequency-independent difference of 0.2-0.4 points per year between models remains unexplained; only 10 species sing at 7 kHz or more. Conclusion: route x observer trend models make trends of high-pitched, often cold-adapted species too negative unless they model tenure.
References
17- uses, supportsLong-serving Breeding Bird Survey observers recorded fewer high-pitched birds; because cold-adapted species sing higher, this drift made 31-77% of the within-observer CTI warming trend (1966-2025)
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- Bird species centroids moved about 35 km north on 1,471 fixed North American survey routes from 1975-1989 to 2010-2024, at about 14% of the isotherm shift and not in proportion to it
- Finnish atlas range margins of southern birds moved north more slowly in 2006-10 to 2022-25 than before while isotherms moved fast; lower detection in 2022-25 explains part of this
- Animal first-detection dates at 99 Japanese weather stations became later than local warming predicts, by about 1.1 days per decade more than plant dates, in 1953-2020
- Demersal species redistribution offset 24% of bottom temperature change in 11 North American trawl series in 1970-2020, but the offset came from the Northeast US fall survey
- Australian temperate reef fish thermal index followed 3-year SST at 0.35 C per C in 2008-2020 and again in 2021-2026, but only through region-wide year changes (549 sites)
- US breeding bird communities sort by temperature almost as strongly between nearby routes as across the continent, but in time they follow only 3-24% of this slope (BBS 1966-2025)
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