Climate-Driven Variation in Yellowfin Tuna Productivity in the Western and Central Pacific Ocean Inferred from a State-Space Model
Simple Summary
Abstract
1. Introduction
2. Materials and Methods
2.1. Fisheries Data
2.2. Model Description
2.3. Model Parameterization and Scenarios Design
2.4. Analysis of Environmental Effects
3. Results
3.1. Comparison of Model Fit Across Different Scenarios
3.2. Time-Varying r and K
3.3. Time-Varying Biological Reference Points
3.4. Population Status Estimates Under Different Scenarios
3.5. Correlation Analysis of Environmental Factors
4. Discussion
5. Conclusions
Supplementary Materials
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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| Scenario | Details | r | K | Time-Varying Parameters | Dependency |
|---|---|---|---|---|---|
| Constant-parameter model (CM) | Both the and the were treated as constant through time. | ||||
| Time-varying model (RM) | The was allowed to vary over time, whereas the was assumed to be constant. | , | |||
| Time-varying model (KM) | The was allowed to vary over time, whereas the was assumed to be constant. | , | |||
| Proportional and covarying model (PKRM) | Proportional and covarying model. The and were assumed to vary proportionally through time. | , , , | |||
| Linked and covarying model (Power-law form) (LKRM) | The and rate were assumed to co-vary over time according to a power-law relationship with exponent . | , , , | |||
| Independently varying and model (IKRM) | The and varied independently over time. | , , , | Independent |
| Variable | Abbreviation | Data Source | Spatial Resolution | Temporal Aggregation | Definition |
|---|---|---|---|---|---|
| Sea Surface Temperature | SST | Copernicus Marine Service | 0.25° × 0.25° | Annual mean (1992–2021) | Sea surface temperature, representing the thermal conditions of the ocean surface layer. |
| Sea Surface Salinity | SSS | Sea surface salinity, reflecting surface water mass properties and ocean circulation. | |||
| Sea Surface Dissolved Oxygen Concentration | SSO | Dissolved oxygen concentration at the sea surface, indicating oxygen-related habitat conditions. | |||
| Sea Surface Chlorophyll-a Concentration | SSCA | Chlorophyll-a concentration at the sea surface, commonly used as a proxy for primary productivity. | |||
| Mixed Layer Thickness | MLT | Thickness of the ocean surface mixed layer, associated with vertical mixing and upper-ocean structure. | |||
| Sea Surface Height | SSH | Sea surface height relative to the geoid, reflecting large-scale circulation and mesoscale ocean dynamics. | |||
| El Niño–Southern Oscillation | ENSO | National Oceanic and Atmospheric Administration | Basin-scale index | A large-scale climate mode in the tropical Pacific, represented by the Niño 3.4 sea surface temperature index. | |
| Pacific Decadal Oscillation | PDO | A basin-scale climate index describing decadal variability in North Pacific sea surface temperature patterns. | |||
| Interdecadal Pacific Oscillation | IPO | A low-frequency climate mode representing interdecadal variability in Pacific basin sea surface temperature. | |||
| Warm Pool Sea Surface Temperature Anomalies | WPSTA | Sea surface temperature anomalies averaged over the western Pacific warm pool region, calculated relative to a long-term climatological mean. |
| Schaefer | ||||||
| Parameter | CM | RM | KM | PKRM | LKRM | IKRM |
| r | 0.45 (0.32–0.64) | 0.46 (0.32–0.67) | 0.46 (0.32–0.66) | 0.46 (0.32–0.67) | 0.46 (0.32–0.67) | 0.46 (0.32–0.67) |
| (×103 t) | 6633 (3499–12,573) | 6143 (3290–11,469) | 6802 (3145–14,706) | 6608 (3150–13,861) | 6285 (3114–12,684) | 6909 (2408–19,823) |
| MSY (×103 t) | 739 (458–1227) | 710 (426–1182) | 784 (397–1550) | 763 (405–1439) | 725 (401–1308) | 800 (286–2234) |
| FMSY | 0.23 (0.16–0.32) | 0.23 (0.16–0.33) | 0.23 (0.16–0.33) | 0.23 (0.16–0.33) | 0.23 (0.16–0.33) | 0.23 (0.16–0.33) |
| BMSY (×103 t) | 3317 (1750–6287) | 3072 (1645–5735) | 3401 (1573–7353) | 3304 (1575–6931) | 3142 (1557–6342) | 3454 (1204–9912) |
| AICc | −53.44 | −49.17 | −48.76 | −48.91 | −46.70 | −43.79 |
| Fox | ||||||
| Parameter | CM | RM | KM | PKRM | LKRM | IKRM |
| r | 0.43 (0.30–0.61) | 0.45 (0.31–0.65) | 0.45 (0.31–0.65) | 0.45 (0.31–0.65) | 0.45 (0.31–0.65) | 0.45 (0.31–0.67) |
| (×103 t) | 5852 (2346–14,602) | 5164 (2178–12,245) | 6300 (1593–24,909) | 5834 (1651–20,612) | 5286 (1823–15,330) | 6782 (1126–40,847) |
| MSY (×103 t) | 922 (409–2079) | 851 (388–1869) | 1039 (258–4184) | 959 (278–3304) | 870 (323–2346) | 1128 (169–7526) |
| FMSY | 0.43 (0.30–0.61) | 0.45 (0.31–0.65) | 0.45 (0.31–0.65) | 0.45 (0.31–0.64) | 0.45 (0.31–0.65) | 0.45 (0.31–0.67) |
| BMSY (×103 t) | 2154 (863–5374) | 1901 (802–4507) | 2319 (586–9168) | 2147 (608–7587) | 1946 (671–5642) | 2496 (414–15,034) |
| AICc | −52.41 | −48.70 | −48.26 | −48.41 | −46.20 | −43.35 |
| Pella-Tomlinson | ||||||
| Parameter | CM | RM | KM | PKRM | LKRM | IKRM |
| r | 0.47 (0.32–0.68) | 0.47 (0.32–0.68) | 0.47 (0.32–0.69) | 0.47 (0.32–0.69) | 0.47 (0.32–0.68) | 0.47 (0.32–0.69) |
| (×103 t) | 7802 (3246–18,754) | 6604 (2566–16,998) | 7542 (2834–20,071) | 7215 (2655–19,611) | 6869 (2531–18,637) | 7574 (2351–24,403) |
| MSY (×103 t) | 697 (436–1115) | 683 (378–1234) | 739 (387–1412) | 731 (391–1365) | 693 (369–1302) | 768 (326–1812) |
| FMSY | 0.15 (0.04–0.64) | 0.19 (0.03–1.16) | 0.18 (0.03–0.94) | 0.19 (0.03–1.04) | 0.19 (0.03–1.11) | 0.19 (0.03–1.07) |
| BMSY (×103 t) | 4520 (1249–16,358) | 3547 (776–16,222) | 4181 (959–18,228) | 3925 (852–18,086) | 3737 (793–17,604) | 4124 (774–21,970) |
| AICc | −54.48 | −49.92 | −49.56 | −49.68 | −47.43 | −44.48 |
| Environmental Variables | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| SST | SSS | SSO | SSCA | SSH | ENSO | MLT | PDO | IPO | WPSTA | |
| Variance inflation factors | 125.91 | 31.99 | 24.47 | 9.47 | 79.92 | 102.78 | 33.17 | 17.02 | 49.18 | 39.72 |
| 7.27 | 22.69 | 9.23 | 26.61 | 47.17 | 9.61 | 15.03 | 36.65 | 14.73 | ||
| 5.08 | 9.32 | 5.13 | 24.45 | 8.70 | 5.32 | 10.50 | 6.42 | |||
| 3.92 | 8.61 | 4.28 | 3.48 | 4.89 | 4.72 | 6.31 | ||||
| Scenario | Optimal Model Formulation | p-Value | |||
|---|---|---|---|---|---|
| PDO | MLT | SSS | SSO | ||
| RM | ~ s(year, k = 3) + s(PDO) + s(MLT, k = 4) + s(SSO) | 0.002 | 0.055 | 0.674 | |
| KM | ~ s(year, k = 3) + s(PDO) + s(MLT) + s(SSS) | 0.001 | 0.002 | 0.061 | |
| PKRM | ~ s(year, k = 3) + s(PDO) + s(MLT) + s(SSS) | 0.001 | 0.002 | 0.066 | |
| LKRM | ~ s(year, k = 3) + s(PDO) + s(MLT, k = 3) + s(SSS) | 0.001 | 0.004 | 0.062 | |
| IKRM | ~ s(year, k = 3) + s(PDO) + s(MLT, k = 3) + s(SSS) | 0.007 | 0.049 | 0.182 | |
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Li, X.; Geng, Z.; Cao, J.; Zhu, J.; Zhu, J. Climate-Driven Variation in Yellowfin Tuna Productivity in the Western and Central Pacific Ocean Inferred from a State-Space Model. Animals 2026, 16, 856. https://doi.org/10.3390/ani16050856
Li X, Geng Z, Cao J, Zhu J, Zhu J. Climate-Driven Variation in Yellowfin Tuna Productivity in the Western and Central Pacific Ocean Inferred from a State-Space Model. Animals. 2026; 16(5):856. https://doi.org/10.3390/ani16050856
Chicago/Turabian StyleLi, Xiaodong, Zhe Geng, Jie Cao, Jizhang Zhu, and Jiangfeng Zhu. 2026. "Climate-Driven Variation in Yellowfin Tuna Productivity in the Western and Central Pacific Ocean Inferred from a State-Space Model" Animals 16, no. 5: 856. https://doi.org/10.3390/ani16050856
APA StyleLi, X., Geng, Z., Cao, J., Zhu, J., & Zhu, J. (2026). Climate-Driven Variation in Yellowfin Tuna Productivity in the Western and Central Pacific Ocean Inferred from a State-Space Model. Animals, 16(5), 856. https://doi.org/10.3390/ani16050856

