Observation and model-based analyses of ocean biological carbon fluxes and ecosystem dynamics

This dissertation examines the ocean biological carbon pump, a complex coupling of biophysical processes that exports carbon from the surface to the deep (5-15 Pg C yr-1), by focusing on the largest component, the gravitational sinking flux (4-9 Pg C yr-1). In the first chapter, I examine the impact...

Full description

Bibliographic Details
Main Author: Wyatt, Abigale
Other Authors: Resplandy, Laure, Geosciences Department
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Princeton, NJ : Princeton University 2024
Subjects:
Online Access:http://arks.princeton.edu/ark:/88435/dsp01ks65hg57b
Description
Summary:This dissertation examines the ocean biological carbon pump, a complex coupling of biophysical processes that exports carbon from the surface to the deep (5-15 Pg C yr-1), by focusing on the largest component, the gravitational sinking flux (4-9 Pg C yr-1). In the first chapter, I examine the impact of interannual variability, specifically marine heat waves, on ecosystem and export production in the Northeast Pacific using a suite of observational data and an ocean biogeochemical model. The model shows that warming-induced strati- fication during marine heat waves relieves winter light limitation while decreasing nutrient supply increasing small phytoplankton production at the expense of large phytoplankton, in agreement with observations. This shift in the phytoplankton assemblage is propagated through the food web, leading to a smaller zooplankton assemblage, and weaker export. I also show that previous observation-based estimates of ecosystem production misattributed a spatial gradient in nutrients to a rapid decline in productivity during a recent marine heat wave. These results highlight the difficulty in disentangling spatial and temporal variability when interpreting sparse observations. In Chapters two and three, I examine the export proxy, thorium-234, used to estimate particle fluxes in situ. I detail the collection of over 1500 individual water samples collected in the Northeast Pacific and the North Atlantic during the 2018 and 2022 NASA EX- PORTS field campaigns. These data were analyzed to produce dozens of particle sinking flux profiles using 1-dimensional (1D) thorium budgets that rely on the assumption that the influence of physical dynamics is negligible relative to the flux of thorium adsorbed on sinking particles. Using observed and simulated velocities, I find that physical processes could bias observed flux estimates by 30% in both regions (Chapter 2). In Chapter 3, using an idealized double gyre model to examine physical thorium transport in fine-scale struc- tures I show that coherent ...