Abstract:A recently commercialized sensor, the In Situ Ultraviolet Spectrophotometer (ISUS), can determine seawater nitrate concentrations rapidly. Procedures for incorporating ISUS data within routine conductivity, temperature, and depth (CTD) profiling studies have not been described. Using a CTD system with an ISUS, vertical hydrographic profiles with nutrient concentrations were determined at 42 sites across the shelf break on the Beaufort Sea, Alaska. Key data processing steps included elimination of redundant nitrate values, shifting the ISUS data so as to be simultaneous with the CTD data, and correcting the ISUS output voltages for warm-up drift. After regressing the corrected ISUS output voltages against nitrate concentrations determined on bottle samples, the ISUS-estimated nitrate concentrations reproduced the bottle results within +/-0.28 μM. The highly detailed ISUS profiles showed mesoscale intrusions of low nutrient water on the upper continental slope and strong nutrient upwelling near the shelf break.Keywords: Nitrate Concentration, Ultraviolet Spectrophotometer, CTD Observations, CTD Processing, Arctic Ocean, Beaufort Sea.With the recognition that the nitrate ion has a strong absorption peak in the lower ultraviolet spectrum below 230 nm [1][2][3], several separate approaches were developed which offered the potential for measurement of high-resolution nitrate distributions in near-surface waters of the oceans [4][5][6][7][8][9]. Several inorganic ions also absorb in this range of the ultraviolet spectrum [1, 9-11], but most are found at such low concentrations in normal ocean waters so as not to interfere, with the exception of bromide [3,11,12]. One instrument, the In Situ Ultraviolet Spectrophotometer (ISUS), was developed at the Monterey Bay Research Institute [11] and became commercially available in 2003 (Satlantic Inc., Halifax NS). The ISUS illuminates a volume of natural seawater in a cell of fixed width (10 mm) and the absorption spectra is measured thrice. The instrument's microprocessor pools the resulting spectra, fits ideal nitrate and bromide absorbance spectra to the observed seawater spectra, and then calculates both these concentrations. Since bromide is conservative with salinity [13,14], the bromide concentration is reported as a salinity. To correct for apparent absorbance due to dark current, every tenth spectrum is a dark scan in which the ultraviolet illumination is blocked. For the instrument used in our study (serial number 003), the manufacturer reported the usable nitrate range, accuracy, and precision to be 0.5-200 μM, +/-2 μM, and +/-0.05 μM. Based on conductivity, temperature, depth (CTD) and ISUS data collected in the Beaufort Sea north of Alaska, we developed the processing procedures for the ISUS data collected during routine CTD vertical profiling. Specifically, our routines eliminated redundant measurement values, corrected for time-delay and for the warm-up drift found in the ISUS data. The results were compared and normalized to measured nitrate concentrati...