Increasing influence of human activities on global climate change has resulted in a gradual increase of SST by 0.64°C in the Yellow Sea than that observed in the 1960s. Temperature influences all aspects of physiology of ectotherms, plays an important role in the survival and growth, and controls the metabolic rate of fish by regulating the activities of enzymes. It also affects physiological and biochemical procedures such as feeding intensity, metabolic rate and protein synthesis rate (
Sun et al., 2000;
Hurst et al., 2012;
Bergstad, 2013;
Trueman et al., 2013). The responses of fish populations and communities to climate forcing represent the cumulative effects of changes in physiological and behavioral characteristics (
Rijnsdorp et al., 2009;
Ottmar and Hurst, 2012). Variations in physiological and morphological traits among fish serve as an indicator of persistent response to environmental history, for example, thermal reaction varied among the growth of different Pacific cod cohorts (
Hurst et al., 2012). The correlation index relating to SST and biological characteristics of the fish was relatively low in the Yellow Sea, which might be attributable to the fact that water temperatures in the Yellow Sea remained within a suitable range for small yellow croaker (
Ding et al., 2007). In addition, large-scale climatic phenomena such as the North Atlantic Oscillation (NAO) and El Niño-Southern Oscillation (ENSO) also affect the spawning, recruitment and distribution of fish populations (
Alheit et al., 2005;
Rojas-Mendez and Mendoza, 2008). During the ENSO years, SST increased and the thermal layer structure changed, which resulted variations in the primary and secondary productivity of fishery species (
Hong et al., 1998) and further changed the community structure, distribution and stock density of these species (
Fan et al., 2001). The habitat range of
Katsuwonus pelamis was markedly increased during ENSO events and extended an additional 6 000 km along the equator because of the warm pool caused by ENSO (
Lehodey et al., 1997). The effects of ENSO on biomass varied for different fishery species, for example, the biomass of
Sardinops sagax,
T. murphyi and
Scomber japonicus increased during ENSO years or after ENSO events. However, ENSO events led to a significant decline in the biomass of
E. ringens (
Ñiquen and Bouchon, 2004). The biomass of small yellow croaker also appeared to increase during ENSO years, or one to two years after ENSO events (
Li et al., 2011). This increase in biomass might have been caused by high water temperatures contributing to a high metabolic rate and short hatching period, which increased the survival rate and recruitment stock density of this species, or changes in environmental factors of the Yellow Sea led to an increased biomass of zooplankton in the spawning and feeding grounds of small yellow croaker and thus, an abundant food to support the growth and development of larvae and juveniles. Although the recruitment of small yellow croaker benefited from an increased SST, a high natural mortality was also observed during this period. Therefore, a positive correlation between natural mortality index and SST was evident. Climate change and human activities caused spatial and temporal heterogeneity, which resulted in changes in the migratory habits of fish along latitudes (
Cury et al., 2000;
Perry et al., 2005;
Cheung et al., 2009,
2013) and water depths (
Dulvy et al., 2008;
Theisen and Baldwin, 2012).