Capturing the Dynamics of Dissolved Organic Carbon (DOC) in Tidal Saltmarsh Estuaries Using Remote‐Sensing‐Informed Models
Authors:
- Aylin Tuzcu KokalAKAylin Tuzcu Kokal
- Joshua P. HarringmeyerJHJoshua P. Harringmeyer
- Olivia Cronin‐GolombOCOlivia Cronin‐Golomb
- Matthew W. WeiserMWMatthew W. Weiser
- Jiyeong HongJiyeong Hong
- Nilotpal GhoshNGNilotpal Ghosh
- Xiaohui ZhuXZXiaohui Zhu
- Nebiye MusaogluNebiye Musaoglu
- Cédric G. FichotCFCédric G. Fichot
- 4 October 2024
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Biogeosciences
- Vol. 129 (10)
Abstract
The fluxes of dissolved organic carbon (DOC) through tidal marsh‐influenced estuaries remain poorly quantified and have been identified as a missing component in carbon‐cycle models. The extreme variability inherent to these ecosystems of the land‐ocean interface challenge our ability to capture DOC‐concentration dynamics and to calculate accurate DOC fluxes. In situ discrete and continuous measurements provide high‐quality estimates of DOC concentration, but these strategies are constrained spatially and temporally and can be costly to operate. Here, field measurements and high‐spatial‐resolution remote sensing were used to train and validate a predictive model of DOC‐concentration distributions in the Plum Island Estuary (PIE), a mesotidal saltmarsh‐influenced estuary in Massachusetts. A large set of field measurements collected between 2017 and 2023 was used to develop and validate an empirical algorithm to retrieve DOC concentration with a ±15% uncertainty from Sentinel‐2 imagery. Implementation on 141 useable images produced a 6‐year time series (2017–2023) of DOC distributions along the thalweg. Analysis of the time series helped identify river discharge, tidal water level (WL), and a marsh enhanced vegetation index 2 as predictors of DOC distribution in the estuary, and facilitated the training and validation of a simple model estimating the distribution. This simple model was able to predict DOC along the PIE thalweg within ±16% of the in situ measurements. Implementation for three years (2020–2022) illustrated how this type of remote‐sensing‐informed models can be coupled with the outputs hydrodynamic models to calculate DOC fluxes in tidal marsh‐influenced estuaries and estimate DOC export to the coastal ocean.Keywords
Funding Information
- National Science Foundation (OCE‐2224608)
- National Aeronautics and Space Administration (80NSSC18K0344)
- National Aeronautics and Space Administration (80NSSC20K1648)
This publication has 60 references indexed in Scilit:
- Ocean carbon from space: Current status and priorities for the next decadeEarth-Science Reviews, 2023
- Fate of cohesive sediments in a marsh-dominated estuaryAdvances in Water Resources, 2019
- Carbon Budget of Tidal Wetlands, Estuaries, and Shelf Waters of Eastern North AmericaGlobal Biogeochemical Cycles, 2018
- Constraining Marsh Carbon Budgets Using Long‐Term C Burial and Contemporary Atmospheric CO2 FluxesJournal of Geophysical Research: Biogeosciences, 2018
- Dissolved organic carbon fluxes in the Middle Atlantic Bight: An integrated approach based on satellite data and ocean model productsJournal of Geophysical Research: Biogeosciences, 2015
- Abundance, stable isotopic composition, and export fluxes of DOC, POC, and DIC from the Lower Mississippi River during 2006–2008Journal of Geophysical Research: Biogeosciences, 2015
- Net ecosystem production and organic carbon balance of U.S. East Coast estuaries: A synthesis approachGlobal Biogeochemical Cycles, 2014
- The fate of terrigenous dissolved organic carbon in a river‐influenced ocean marginGlobal Biogeochemical Cycles, 2014
- Pulsed, cross‐shelf export of terrigenous dissolved organic carbon to the Gulf of MexicoJournal of Geophysical Research: Oceans, 2014
- Estimation of Dispersion and Characteristic Mixing Times in Plum Island Sound EstuaryEstuarine, Coastal and Shelf Science, 1998