Warm springs act like a 1.5-day later survey per 1 C in Breeding Bird Survey counts of 317 species (1966-2025); this phenology-detection artefact is real but too small to explain weak climate tracking
Question: the Breeding Bird Survey (BBS) counts each route once per year on a calendar date. In a warm spring the breeding cycle is earlier, so a warm spring must act like a later survey date. Does this phenology-detection artefact explain part of the weak climate tracking of bird communities? Data: 130,303 standard BBS runs on 5,319 US and Canadian routes (2026 release, 1966-2025), GHCN_CAMS April-May temperature anomalies, 317 species; UKBMS 2024 flight periods and site indices of 48 butterfly species with E-OBS temperature. Method: per-species models with route x observer and year fixed effects gave the within-route survey-date slope and the spring-anomaly response; a cross-fitted (odd/even years) random-effects meta-regression across species gave the implied phenological advance k. We wrote the plan before the outcomes. Results: species whose counts fall through the season had lower counts after warm springs. k was 1.45 days per 1 C (species bootstrap 1.19-1.72; permutation p = 0.001), 1.52 with migration, temperature-index and abundance covariates, 1.40 with family effects, and 1.24 from the within-species anomaly x date term. The previous spring (-0.07) and the next spring (-0.02) gave no relation. Residents gave 2.2 and migrants 1.3 days per 1 C (exploratory). The artefact explains about 20% of between-species variance in spring responses, but its effect on the community temperature index trend is +0.0003 C per decade, and survey-date drift adds -0.0011, against an observed 0.024 C per decade. In butterflies, flight dates advanced 3.9 days per 1 C, and an emulated single visit changed same-summer responses by 5-13% per 1 C, as much as the true response; the emulation showed that the count-based estimator recovers about 77% of k. Conclusion: the artefact is real and must be corrected in single-species weather responses, but it does not explain the tracking deficit. Limitations: correlational design, no breeding-date data, check terms after the survey gave small slopes (about one sixth of the main value), coarse temperature, Gaussian flight curves.
References
19- usesLong-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)
- uses, supportsYear-to-year temperature responses of 320 North American bird species followed 5-14% of own spatial gradients, with no clear lasting part; 49 British butterfly species followed about 50% in 2 summers
- supportsBird community temperature index followed less than 10% of May-July warming on 5,294 North American survey routes in 1970-2024 with route and observer controls
- supportsCommunity thermal composition in 75 monitoring networks followed about 12% of its own spatial temperature gradient in time; a lag fit gives fast adjustment to a small target (1948-2025)
- Bird abundance gradients between nearby US survey routes kept 69% of the regional temperature gradient per degree with 5 km route-path climate; year-to-year tracking stayed at about 3% (1966-2025)
- 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)
- Survey-date slope changes were uncertain in Canada and US bird records in 1985-2024
- supportsMarch-April warmth gave no clear common link to bird survey dates in Canada and the US in 1985-2024
- 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
- 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
- Climate suitability change predicted little of US bird abundance change in 2010-2025: 0.05 per log unit within species on survey routes, and no species-level forecast skill
- 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
- 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)
- doi:10.1111/ele.13898
- doi:10.5285/b9d237fc-5a79-4449-bcee-34c52d87608f
- doi:10.5285/53a1c705-4437-48bb-9bcd-b68977f8edd9
- doi:10.1029/2007JD008470
- doi:10.1029/2017JD028200
Cited by
4 publications- Passing vehicles hid low-pitched, warm-adapted birds at North American Breeding Bird Survey stops in 1997-2025, but traffic grew too little to change the bird temperature index trend by over 1% uses
- Uniform count-scale changes had small mean effects on a bird thermal trend in 1997-2025 reviews
- A spatial thermal benchmark needs a 1.90-fold late-count allowance in log-weighted indices on 2,075 paired bird routes reviews
- Controls kept a weighted spring shift estimate near 1.25 days per C in 317 North American bird species uses, supports