Preprints
https://doi.org/10.5194/egusphere-2026-3910
https://doi.org/10.5194/egusphere-2026-3910
21 Jul 2026
 | 21 Jul 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Chlorophyll–particle backscattering displacement reveals multiple deep chlorophyll maximum structures in the North Pacific

Taketo Hashioka and Maki N. Aita

Abstract. Subsurface chlorophyll-a (Chl) maxima are common features of stratified oceans, but a Chl maximum does not necessarily indicate a maximum in particle-associated optical structure. Here we use Biogeochemical-Argo (BGC-Argo) observations from the North Pacific during 2022–2025 to examine how the previously recognized separation between Chl maxima and particle-associated optical structure is expressed across a large set of vertically resolved in situ profiles. For 10,801 usable paired Chl and particulate backscattering at 700 nm (BBP700) profiles, we diagnosed the depths of the Chl DCM (deep chlorophyll maximum) and BBP700 maximum within the upper 300 dbar and classified profiles by their vertical displacement. Coupled profiles, in which the two maxima occurred within 25 dbar of each other, were the most frequent class and had median Chl DCM and BBP700 maximum depths of 52.5 and 47.5 dbar, respectively. In Chl deeper profiles, the Chl DCM was displaced downward relative to a shallower BBP700 maximum, consistent with a stronger contribution of photoacclimation or pigment adjustment to the Chl maximum. In Chl shallower profiles, a shallow Chl maximum coexisted with a deeper BBP700 maximum, demonstrating that Chl–BBP700 decoupling is not unidirectional. The three displacement classes showed coherent basin-scale spatial organization and distinct nitracline contexts, with the nitracline generally deeper than both optical maxima in Coupled and Chl deeper profiles, whereas Chl shallower profiles tended to show a deeper BBP700 maximum near the nitracline depth range. Together, these findings indicate that North Pacific Chl DCMs do not represent a single uniform vertical bio-optical structure. Instead, the previously recognized separation between Chl maxima and particle-associated optical structure is expressed in mature BGC-Argo observations as coherent vertical, spatial, and nitracline-related structures across the North Pacific.

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Taketo Hashioka and Maki N. Aita

Status: open (until 01 Sep 2026)

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Taketo Hashioka and Maki N. Aita

Data sets

Processed BGC-Argo data for chlorophyll–particle backscattering displacement analysis in the North Pacific Taketo Hashioka and Maki N. Aita https://doi.org/10.5281/zenodo.20873450

Model code and software

Python analysis code for BGC-Argo chlorophyll–particle backscattering displacement analysis Taketo Hashioka and Maki N. Aita https://doi.org/10.5281/zenodo.20873450

Taketo Hashioka and Maki N. Aita
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Latest update: 21 Jul 2026
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Short summary
Many ocean studies use chlorophyll to describe where life is concentrated below the sea surface, but chlorophyll alone can be misleading. We analysed more than 10,000 recent robot-float profiles from the North Pacific and found that chlorophyll-rich layers and particle-rich layers often occur at different depths. This shows that subsurface ocean life has several distinct structures, improving how observations, satellites, and models interpret the hidden ocean.
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