©2026 Biological and Chemical Oceanography Data Management Office.Primary productivity measurements from the Hawaii Ocean Time-series (HOT) program from 1988 through 2024. The 14C-radiotracer method was used to measure the assimilation of dissolved inorganic carbon (DIC) by phytoplankton as an estimate of the rate of photosynthetic production of organic matter in the euphotic zone. Starting July 1989 (HOT-008), all incubations were conducted in situ on a free-floating, surface tethered array. From 1990 through mid-2000, incubations were conducted in situ at ei...
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The 14C-radiotracer method is used to measure the assimilation of dissolved inorganic carbon (DIC) by phytoplankton as an estimate of the rate of photosynthetic production of organic matter in the euphotic zone. These data are from monthly measurements of primary production collection at Station ALOHA as part of the HOT Time-series program
White, A. E., Karl, D. M., Fujieki, L. A. (2026). Primary productivity measurements for the Hawaii Ocean Time-series (HOT) program from October 1988 to December 2024 at Station ALOHA. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 5) Version Date 2026-04-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.737163.5 [access date]
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