Fish community temperature indices increased by 0.12 C per 1 C SST anomaly in 13 of 14 North American trawl surveys in 1970-2020; the long-term increase was 0.04-0.07 C per decade
Question: do demersal fish communities on North American shelves change toward warm-water species when the sea becomes warmer, from year to year and over decades? Data: 14 OceanAdapt fixed-strata bottom trawl surveys (121,135 hauls, 1970-2020, nine geographic groups), 667 fish species, ERSSTv5 and HadISST1 sea surface temperature (SST), and the WOA23 climatology. Method: the species temperature index (STI) is the mean climatological bottom temperature at the hauls that caught the species, fixed in time. The community temperature index (CTI) is the incidence-weighted mean STI of a survey year. We compared it with the footprint SST of the 12 months before the survey. Results: after linear detrending, the CTI was higher in warmer years in 13 of 14 surveys (10 with 95% CI above zero, none below). The pooled slope was 0.12 C of CTI per 1 C of SST (95% CI 0.08 to 0.16; group level 0.11). A species-shuffle null gave a combined z of 5.0 (3.8 over groups). The slope stayed positive with vessel-change steps, footprint and richness controls (0.08), core species, STI from other regions, HadISST1, and in both periods before and from 2000. It was smaller with biomass weights (0.036) and survey-season SST (0.05). The pooled long-term CTI trend was +0.041 C per decade (-0.005 to +0.088), against +0.26 C per decade of ERSSTv5 warming (ratio 0.19, CI -0.13 to 0.56). With step terms at reported vessel changes the trend was +0.059 (0.033 to 0.085; ratio 0.29). Only the two Northeast US surveys had long-term trends beyond the species-shuffle null. The two negative trends (Gulf of St. Lawrence) became near zero with vessel-change steps, but part of that decrease agrees with a real cold period. Limitations: SST is not bottom temperature; the two SST products disagree on trends; the STI comes from the same surveys; incidence depends on detection, and species per haul increased in 11 of 14 surveys; nominal survey months; association only. Conclusion: the year-to-year warm-species response is consistent but small, and the long-term change is about one fifth to one third of the SST warming rate.
community temperature index · species temperature index · climate debt · bottom trawl survey · demersal fish · OceanAdapt · sea surface temperature · ERSSTv5 · HadISST1 · World Ocean Atlas · thermophilization · observation bias · vessel change · species shuffle null · North America · continental shelf · range shift · regional replication
References
14- Bird 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 sci:sha256:c0a3a9aa7b4c6115119528bcd43c4f51b7bc2de204c571e3c468161b72cf1b91
Bird CTI tracking result in this campaign; we compare the fish tracking ratio with it.
- supportsDemersal fish in three Alaska trawl surveys experienced about 93% of year-to-year bottom temperature anomalies in 1982-2026; a thermal-niche model predicted about 55% sci:sha256:80df002698b6546a701987b85654b633fa3f791c020273119ac8a48dfcb50886
Alaska groundfish showed small year-to-year redistribution; our small Alaska CTI slopes agree.
- Prior-year cold pool area did not change groundfish northing in eastern Bering Sea trawl surveys in 1982-2026; a northward offset of about 9 km stayed after 2000 sci:sha256:b83b9063138622a70c8fa5421cd2b2d578c62dcf01789f8d0f7a30c430b68a33
Earlier eastern Bering Sea groundfish distribution study in this campaign.
- 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 sci:sha256:7714830c552415458e0fbece8fb93ae05d88d18000b801144071d2993a034a3e
Bird centroid tracking fraction in this campaign, for comparison.
- useshttps://github.com/pinskylab/OceanAdapt
Fixed-strata trawl survey data, commit 0d4bcaffe649e970674fe165fe892ab4d787e76a.
- usesdoi:10.1175/JCLI-D-16-0836.1
ERSSTv5 SST.
- usesdoi:10.1029/2002JD002670
HadISST1 SST.
- useshttps://www.ncei.noaa.gov/products/world-ocean-atlas
WOA23 temperature climatology for the STI.
- useshttps://www.marinespecies.org
WoRMS taxonomy to select fish.
- doi:10.1038/s41558-019-0631-5
- doi:10.1038/nclimate1347
- doi:10.1111/gcb.15614
- doi:10.1038/s41586-023-06449-y
- doi:10.1126/science.1239352
Cited by
3 publicationsPublic catalog entries on Sciscape.
- Marine warming-by-baseline links to assemblage richness and abundance trends were not clear when the link could vary among studies, in 2020 BioTIME data and 29 new BioTIME 2.0 studies
Related campaign work on trawl-survey community temperature indices.
- North Sea fish latitude did not follow winter temperature in 2002-2025 as Perry et al. (2005) found for 1977-2001, in two IBTS survey seasons
Campaign study of fish community temperature indices in 14 North American trawl surveys.
- Pre-2014 temperature slopes predicted the 2014-2016 heatwave change of southern California fish larvae, not of central California juvenile catches; the 2017-2019 change did not follow SST
Campaign study of fish community temperature indices in North American trawl surveys.