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Chen Peng, Chen Xinjun. Evaluating the effects of sea surface temperature variations on fishing ground of anchoveta (Engraulis ringens) in the southeast Pacific Ocean[J]. Haiyang Xuebao, 2017, 39(4): 79-88. doi: 10.3969/j.issn.0253-4193.2017.04.0088
Citation: Chen Peng, Chen Xinjun. Evaluating the effects of sea surface temperature variations on fishing ground of anchoveta (Engraulis ringens) in the southeast Pacific Ocean[J]. Haiyang Xuebao, 2017, 39(4): 79-88. doi: 10.3969/j.issn.0253-4193.2017.04.0088

Evaluating the effects of sea surface temperature variations on fishing ground of anchoveta (Engraulis ringens) in the southeast Pacific Ocean

doi: 10.3969/j.issn.0253-4193.2017.04.0088
  • Received Date: 2016-07-28
  • Rev Recd Date: 2016-12-18
  • Anchoveta (Engraulis ringens) is one of the important small pelagic species living in the southeast Pacific Ocean. Exploring the process that fishing grounds vary with oceanic environmental factors could help us to understand the variations in fish stocks, which is beneficial for fishing industry. In this study, based on the Peruvian fishery logbooks of anchoveta from 2005 to 2014 as well as sea surface temperature (SST) data, we developed the fishing ground index (FGI) by using the catch per unit effort (CPUE) and fishing effort to understand the variation of fishing ground. The fishing ground were also divided into different types and correlated with the SST isotherms in order to evaluate their forming mechanism. The results indicated that significant differences (P<0.01) were="" found="" for="" fgi="" with="" the="" fishing="" periods="" earlier="" mid="" stage="" and="" later="" areas="" north="" middle="" area="" south="" on="" basis="" of="" analysis="" variance.="" according="" to="" distribution="" we="" defined="" ground="" anchoveta="" as="" type="" ground.="" when="" warm="" sea="" surface="" waters="">20℃) had not intruded into the near shore area, the "A" type fishing ground occurred. Otherwise, the "B" type fishing ground occurred. Our findings suggested that the surface temperature structure with "A" type is favorable for the formation of fishing ground in the earlier or mid stage of fishing periods. Moreover, the 19℃ or 20℃ SST isotherm in earlier stage and the 18℃ or 19℃ SST isotherm in mid stage could be used as an indicator to search for the productive fishing ground.

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