In 2014–2024 Palmer LTER net tows, a 1993–2013 ENSO model predicted pteropod abundance, but the 5-year krill cycle and four other published relations did not
Question: do the 1993–2013 macrozooplankton relations reported for the Palmer LTER grid west of the Antarctic Peninsula (Steinberg et al. 2015) predict the nine later January–February surveys (2014–2020, 2023, 2024)? Approach: we wrote a protocol with six predictions before we looked at the new abundances. We rebuilt the annual abundance anomalies (1,450 tows; grid lines 200–600 as the primary domain) with the published method. We fitted each model to 1993–2013 only and extrapolated it. Each test used a correlation with a permutation p, a skill score against the 1993–2013 mean, and eight index variants, including an independently harmonised data set. Results: the 1993–2013 fits reproduced the published values (krill ~ primary production 2 years before, R² = 0.73; 5-year krill period, permutation p = 0.002; pteropod ~ winter ENSO, R² = 0.58). Only the pteropod (Limacina rangii) ~ prior-winter MEI model predicted 2014–2024: r = 0.79 (p = 0.008), skill 0.60, and r = 0.76–0.85 in all variants. The fixed 5-year krill cycle (r = −0.25, skill −2.1) and the krill–production model (r = −0.47, skill −6.9, n = 6) failed, although the krill–production fit was stronger than the best of 53 candidate predictors by chance. The salp ~ SAM + ENSO, ice krill ~ SAM + ENSO and Thysanoessa macrura trend models had no skill. Krill recruitment pulses continued (2018, 2024), but later than the 5-year phase predicted; the best period for 1993–2024 recruitment is 5.6 years (p = 0.019). Limitations: the test has only 6–9 years. There were fewer tows after 2009. We used the CPC SAM index and MEI.v2, and we tested the published final predictors, not a full repeat of the stepwise search.
Antarctic krill · Euphausia superba · Limacina · Salpa thompsoni · pteropod · ENSO · Southern Annular Mode · western Antarctic Peninsula · Palmer LTER · out-of-sample test · zooplankton · recruitment cycle · primary production · forecast skill
References
9- challengesdoi:10.1016/j.dsr.2015.02.009
Source of the six tested 1993–2013 relations. The pteropod–ENSO relation predicted 2014–2024, but the krill 5-year cycle, krill–production, salp, ice krill and T. macrura relations did not.
- doi:10.1038/s43247-025-02720-4
Shows how Palmer LTER sampling changes affect zooplankton indices; motivates our cell- and date-adjusted index variant.
- usesdoi:10.6073/pasta/03e6d72a78bc2512ef5bb327e686f8fa
Palmer LTER zooplankton tows 1993–2008.
- usesdoi:10.6073/pasta/25b4c17c2c53892d09721299d1a070cb
Palmer LTER zooplankton tows 2009–2024.
- usesdoi:10.6073/pasta/7ae0cd62ffad55d8ac29442a6e65578f
Krill length frequencies for the recruitment index.
- usesdoi:10.6073/pasta/3443da26bd04c93becc1883f2a7fc279
Independently harmonised AMLR+LTER macrozooplankton data, used as a robustness check.
- usesdoi:10.6073/pasta/4207e529832840db2282498d9f4f4f05
Sea-ice timing indices.
- usesdoi:10.6073/pasta/3978e5f4b5e43ee0247c05de7226bcd5
Sea-ice extent and area.
- usesdoi:10.6073/pasta/ff5102af132e6e65d83370d6c9ecfa9b
Cruise chlorophyll a and primary production.
Cited by
2 publicationsPublic catalog entries on Sciscape.
- usesThe adjusted krill–salp log-density link was uncertain at 16 Palmer survey cells in 1993–2024
We reuse its retained raw Palmer source files and source inventory. Its annual abundance forecast test provides prior context.
- usesSalp catch presence showed no clear rise at 16 Palmer survey cells from 1993–2008 to 2009–2024
We read this verified publication and used its source inventory to locate retained raw data. We wrote new parsing and analysis code for a different, fixed-cell presence and joint-catch test.