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Empirical algorithms to estimate water column pH in the Southern Ocean

机译:估算南大洋水柱pH值的经验算法

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摘要

Empirical algorithms are developed using high-quality GO-SHIP hydrographic measurements of commonly measured parameters (temperature, salinity, pressure, nitrate, and oxygen) that estimate pH in the Pacific sector of the Southern Ocean. The coefficients of determination, R-2, are 0.98 for pH from nitrate (pH(N)) and 0.97 for pH from oxygen (pH(Ox)) with RMS errors of 0.010 and 0.008, respectively. These algorithms are applied to Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) biogeochemical profiling floats, which include novel sensors (pH, nitrate, oxygen, fluorescence, and backscatter). These algorithms are used to estimate pH on floats with no pH sensors and to validate and adjust pH sensor data from floats with pH sensors. The adjusted float data provide, for the first time, seasonal cycles in surface pH on weekly resolution that range from 0.05 to 0.08 on weekly resolution for the Pacific sector of the Southern Ocean.
机译:使用高质量的GO-SHIP水文测量技术开发经验算法,该测量技术可测量通常测量的参数(温度,盐度,压力,硝酸盐和氧气),这些参数可估算南大洋太平洋地区的pH值。对于硝酸盐(pH(N)),pH的测定系数R-2为0.98;对于氧气(pH(Ox)),pH的测定系数为0.97,RMS误差分别为0.010和0.008。这些算法适用于“南部海洋碳和气候观测与建模(SOCCOM)”生物地球化学剖面浮标,其中包括新型传感器(pH,硝酸盐,氧气,荧光和反向散射)。这些算法用于估计不带pH传感器的浮子的pH值,并验证和调整带pH传感器的浮子的pH传感器数据。调整后的浮点数据首次提供了按周分辨率计算的地表pH值的季节性周期,按周分辨率计,南大洋太平洋区域的范围为0.05至0.08。

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