Assessing the UK′37-sea surface temperature relationship in shallow marine waters

Abstract

<p>To investigate the relationship between the alkenone unsaturation index (U^K′₃₇) and sea surface temperature (SST) in coastal and continental shelf waters, 58 surface sediment samples were collected from the South China Sea (SCS), Taiwan Strait, and East China Sea (ECS). We combined the new results with the previously published 71 data points from the SCS, the shallow water areas of the Yellow Sea (YS) and northern ECS, to form a dataset with sample sites spanning across 6°N and 37°N (including annual SST calibration between 14.3°C and 28.6°C). With this dataset, we examined the U^K′₃₇-SST relationship based on 129 samples from the Western North Pacific (WNP) margin as well as using 85 samples from specific WNP shallow water. The U^K′₃₇ index from the low-mid latitudinal WNP margin demonstrated a good correlation with the surface annual mean SST (0–50 m water depth; <em>R</em>²=0.89). The slope of linear regression (U^K′₃₇-SST) based on the coastal-continental shelf samples with water depth less than 200 m is similar to that of the published global open ocean regression equation. These results confirm that U^K′₃₇ can be used as a shallow sea water SST proxy in mid-low latitudes of the WNP marginal seas. In addition, our reintegrated U^K′₃₇-SST results based on 172 global shallow water samples are similar (similar slopes and intercepts) to the shallow ocean results in the WNP marginal seas. However, the similarity of the regression formula to the open ocean does not imply that the formula is applicable. For example, of the 85 data in the shallow waters from the marginal sea in this study, the majority of data points lie above the regression line, showing positive residuals for U^K′₃₇. This regression bias appears to be caused by specific marine environments, such as warm ocean currents and/or high nutrient conditions that result in positive U^K′₃₇ residuals. Taken together, considering the specific temperature and environmental factors in the shallow waters of the low-mid-latitude WNP margin, we propose a nonlinear U^K′₃₇-SST regression formula: U^K′₃₇ = −1.2488+0.1740×SST−0.0035×(SST)², <em>R</em>²=0.93, <em>N</em>=85, specifically for the environments with SST below 24°C.<br></p>