Physics-Informed Deep Learning for Forecasting Coastal Dead Zones

NSF Project Overview and Funding

  • Announcement Date: August 20, 2026.
  • Lead Institution: NC State University.
  • Funding Agency: U.S. National Science Foundation (NSF).
  • Total Project Investment: A combined total of 1,049,8751,049,875 over three years (more than 1 Million1\text{ Million}).
    • NC State Award: 800,013800,013.
    • Louisiana State University (LSU) Award: 249,862249,862.
  • Formal Project Title: "Collaborative Research: CAIG: Physics-Informed Deep Learning for Understanding Coastal Hypoxia Formation Mechanisms."
  • Primary Mission: To improve understanding and prediction of coastal hypoxia—marine areas with dangerously low dissolved oxygen levels, commonly known as "dead zones."
  • Practical Application: Developing forecasting tools that run faster than traditional numerical models while remaining physically consistent, aimed at supporting fisheries management and decision-making across Gulf Coast communities.

Research Team Leadership and Collaboration

  • Lead Principal Investigator (PI):
    • Paul Liu: Lead PI for the project and co-director of the AI Hub for Science at NC State.
  • NC State University Team Members:
    • Ruoying He: Faculty Fellow at the AI Hub for Science.
    • Dongkuan "DK" Xu: Faculty Fellow at the AI Hub for Science.
  • Louisiana State University (LSU) Team:
    • Kehui "Kevin" Xu: Professor at LSU leading the collaborating LSU team.

Hypoxia Formation Mechanisms and Environmental Dynamics

Satellite image of Mississippi and Atchafalaya rivers depositing sediment into the Gulf of Mexico

  • Geographic Scope:
    • The largest coastal dead zone in the United States forms every summer along the Louisiana–Texas continental shelf.
  • Environmental Drivers:
    • Nutrient Loading: High nutrient levels transported by the Mississippi River and Atchafalaya River stimulate intense biological production in coastal waters.
    • Physical Oceanography: Ocean circulation, water-column stratification (pycnocline formation separating the surface layer from the bottom layer), and seafloor benthic processes dictate where oxygen is depleted.
  • Image Credit: NASA (Liam Gumley, Space Science and Engineering Center, University of Wisconsin-Madison and the MODIS science team).
  • Scientific Challenge: Resolving how physical, chemical, and biological factors interact to determine the overall size, spatial distribution, and persistence of hypoxic zones.

Multi-Architecture Physics-Informed AI Framework

Integrated framework diagram connecting river systems, sediment dynamics, PINN, and GNN models to observe hypoxia frequency

  • Core Technical Architecture:
    • Multi-Architecture Physics-Informed Neural Network (PINN): Integrates physical constraints into deep learning algorithms.
    • Dynamic Graph Neural Networks (GNNs): Captures dynamic spatial-temporal relations across coastal grids.
    • Image-Segmentation Models: Analyzes dynamic spatial features and patterns in oceanographic data.
    • High-Resolution Ocean-Circulation Simulations: Provides baseline hydrodynamic input datasets.
    • Ocean Digital Twins: Offers high-fidelity virtual ocean environments for multi-scenario ocean modeling.
  • Embedded Physical Constraints:
    • Water movement and physical transport.
    • Oxygen transport equations.
    • Light attenuation in coastal waters.
    • Sediment oxygen consumption at the seabed.
  • Mathematical Governing Equations:
    • Fluid Momentum Equation:     ∂u∂t+Nu(u,p,c)=0\frac{\partial u}{\partial t} + \mathcal{N}_u(u, p, c) = 0
    • Oxygen Concentration Transport Equation:     ∂c∂t+∇⋅(uc)=∇⋅(K∇c)+S\frac{\partial c}{\partial t} + \nabla \cdot (u c) = \nabla \cdot (K \nabla c) + S
    • Sediment Transport Equation:     ∂s∂t+∇⋅(us)=∇⋅(Ks∇s)−ws∂s∂z+E\frac{\partial s}{\partial t} + \nabla \cdot (u s) = \nabla \cdot (K_s \nabla s) - w_s \frac{\partial s}{\partial z} + E
  • Benthic and Sediment Dynamics Innovation:
    • Incorporates seabed-to-water oxygen exchange measurements.
    • Dynamic modeling of three sediment phases:
    1. Settling: Transport of particulate matter down to the seafloor.
    2. Resuspension: Re-entrainment of benthic sediments back into the water column (especially prominent during storm events).
    3. Benthic Oxygen Consumption: Microbial oxygen depletion within seabed sediments.
    • Helps isolate exact mechanisms driving how hypoxic waters form, spread, and persist.

Educational Impacts and Open Science Initiatives

  • Interdisciplinary Student Training:
    • Educational and research training for graduate and undergraduate students spanning oceanography, coastal science, and artificial intelligence.
  • Educational Platform:
    • Educational materials shared publicly via an AI-powered learning platform.
  • Open Resources:
    • Project data, software tools, and trained AI models will be made available as open resources for the scientific community.