日本地球惑星科学連合2025年大会

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[E] 口頭発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS13] Exploring Variability and Changes in Ocean Biogeochemical Cycles

2025年5月28日(水) 15:30 〜 17:00 101 (幕張メッセ国際会議場)

コンビーナ:高野 陽平(British Antarctic Survey)、Tjiputra Jerry(Norwegian Research Centre, Bjerknes Centre for Climate Research)、小林 英貴(富山大学理学部)、山口 凌平(海洋研究開発機構)、座長:高野 陽平(British Antarctic Survey)、Jerry Tjiputra(Norwegian Research Centre, Bjerknes Centre for Climate Research)、山口 凌平(海洋研究開発機構)、小林 英貴(富山大学理学部)

16:00 〜 16:15

[AOS13-09] Particle Size Distribution and sinking velocity of Large Marine Particles in the Global Ocean With In Situ Optical
Observations and Supervised Learning for the all global ocean

*Gian Giacomo Navarra1、Curtis Deutsch1、Yohei Takano2、Redouanne Lguensat3 (1.Princeton University、2.British Antarctic Survey、3.Institut Pierre-Simon Laplace)

The abundance and size distribution of marine particles control a range of biogeochemical and ecological processes in the ocean, including carbon sequestration. These quantities are the result of complex physical-biological interactions that are difficult to observe, and their spatial and temporal patterns remain uncertain. Here, we present a novel analysis of particle size distributions (PSDs) from a global compilation of in situ Underwater Vision Profiler 5 (UVP5) optical measurements. Using a machine learning algorithm,we extrapolate sparse UVP5 observations to the global ocean from well-sampled oceanographic variables.We reconstruct global maps of PSD parameters (biovolume [BV] and slope) for particles for the all water column. These reconstructions reveal consistent global patterns, with high chlorophyll regions generally characterized by high particle BV and flatter PSD slope, that is, a high relative abundance of large versus small particles. The resulting negative correlations between particle BV and slope further suggests synergistic effects on size-dependent processes such as sinking particle fluxes. Our approach and estimates provide a baseline for an improved understanding of particle cycles in the ocean, and pave the way to global, three-dimensional reconstructions of PSD and sinking particle fluxes from the growing body of UVP5 observations.