Year-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
Question: community temperature indices follow only a small part of warming. Which part of the species-level response is missing? Data: North American Breeding Bird Survey 2026 release (1966-2025; 320 species, 4,802 routes, 9.1 million species-route-year counts), UK Butterfly Monitoring Scheme site indices (1976-2024; 49 species, 2,410 British sites), GHCN_CAMS and E-OBS temperature. Method: for each species, the spatial gradient g is the slope of route mean log abundance on route climatology at each route. Per-species fixed-effects models (route x observer or site, and species x year) related log counts to local temperature anomalies of the same season, four previous summers, four winters, and placebo seasons after the count. The ratio lambda = temporal response / g is 1 for full space-for-time equivalence. We refitted all species without each of 10 year blocks (jackknife). Results: in birds, the long-run lambda was 0.14 (95% CI 0.05-0.24) with linear detrending, but the placebo next-summer term was as large as the previous-summer term. With 11-year high-pass anomalies the placebos were near 0, the same-season term stayed at 0.045 (0.017-0.074), and the lagged terms gave 0.014 (-0.10 to 0.13). Within species, the response followed 14-20% of the gradient (intervals exclude 0); between species, mean responses did not increase with mean gradients (-0.13 and -0.31). British butterflies followed 0.44 (0.14-0.75) and 0.54 (0.04-1.05) of their gradients within the same and previous summer, five to ten times the bird value, with clean placebos; longer lags and winters added nothing clear, and their between-species part was not determined. Neither year-to-year sensitivities nor spatial gradients forecast species trends (bird Spearman -0.00 and 0.09; out of sample 0.03; butterflies -0.27 and 0.18). The implied bird CTI change was about one third of the same-species spatial expectation and about 0.002 C per decade. Conclusion: weak bird tracking is not mainly a long lag; the clear response is small and transient (possibly part detection), and species that spatial gradients predict to gain do not gain. Butterflies follow temperature faster. Limitations: correlational design; no detection model; gradients include non-thermal factors; the high-pass variant was added after the main fits; butterfly long-run totals are imprecise.
References
17- uses, 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
- supportsBird 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
- supportsClimate 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
- 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
- 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)
- supports, usesCommunity 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)
- supportsA warm breeding season was followed by lower next-year counts in the warm part and higher counts in the cool part of 368 bird species ranges in North American surveys, 1970-2024
- Winter temperature changed next-summer counts of the same bird species only in states where the species stayed for winter, on 4,758 North American survey routes in 1967-2024
- usesFrozen bird thermal indices had spatial slopes of 0.33-0.44 C per climate C in four East and West samples in 1970-2024
- https://www.sciencebase.gov/catalog/item/6a0b0b0ab66b0188da36aedd
- doi:10.1029/2007JD008470
- doi:10.5285/53a1c705-4437-48bb-9bcd-b68977f8edd9
- doi:10.1029/2017JD028200
- doi:10.1111/ele.13898
- doi:10.1038/nclimate1347
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6 publications- Forest type explained about half of the gap between spatial and temporal bird community temperature slopes on 2,523 forested US routes (1966-2025), but not in open-habitat birds, the East, or species supports
- 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%
- 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 uses, supports
- Controls kept a weighted spring shift estimate near 1.25 days per C in 317 North American bird species reviews
- 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) uses, supports
- 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