Primary productivity measurements from the Hawaii Ocean Time-Series (HOT) from 1988 to 2021. 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. All incubations from 1990 through mid-2000 were conducted in situ at eight depths (5, 25, 45, 75, 100, 125, 150 and 175m) over one daylight period using a free-drifting array as described by Win...
Show moreMonthly measurements of primary production were collected at station ALOHA as part of the HOT program.
White, A. E., Karl, D. M., Fujieki, L. A. (2023) Primary productivity measurements from the Hawaii Ocean Time-Series (HOT) project from 1988-2021 at Station ALOHA. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2) Version Date 2023-08-12 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.737163.2 [access date]
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