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Patrick Hawbecker

Publications and source records attributed to Patrick Hawbecker.

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Developing an Offshore Machine Learning Surface Layer Scheme

Turbulent fluxes between the surface and the atmosphere are typically parameterized using empirically fit relationships. Here we test machine learning techniques for fitting the relationship for the offshore environment. To do that, data from three offshore sites are used: the Martha's Vineyard Coastal Observatory (MVCO) air-sea interaction tower, the FINO1 research platform, and the CASPER-West FLIP research vessel deployed off the coast of California. Two machine learning methods were employed: Neural Networks (NN) and Random Forests (RF). Because the observational sites had towers with measurements at different levels, the vertical differences were input as gradients. Models were built for both momentum flux and heat flux. ML models trained at the individual sites were competitive with and in some cases, better than the physically-based COARE-3 model tailored to offshore fluxes. The heat flux ML models generally outperformed the physics-based parameterizations for most metrics, but the results were mixed for momentum flux, with only the site with the most training data (MVCO) producing results better than COARE-3. When the ML models from that site were applied to the other sites, results were degraded from using data from the site being tested. ML models built from data combined from the three sites generally showed improvements for the sites with less available training data. When assessing which variables were most important, the wind speed was most important for momentum flux and temperature gradient for heat flux.

physics.ao-ph

Explaining Surface Layer Theory Departures in Marine Flux Profiles with Data-Driven Discovery

Monin--Obukhov Similarity Theory (MOST), which underpins nearly all bulk estimates of surface fluxes in the atmospheric surface layer, assumes monotonic wind profiles and vertically uniform momentum and heat fluxes. Here, we show that conditions frequently arise in coastal marine settings where these assumptions do not hold. Using flux measurements from the Coastal Land-Air-Sea Interaction (CLASI) project's Air-Sea Interaction Spar (ASIS) buoys with wind and flux measurements at typically ~3m and ~5m above the sea surface, we find that wind speed decreases with height in nearly 20% of observations, and that large vertical gradients in sensible heat flux occur near the surface, contrary to what would be predicted by MOST. Both anomalies are strongly modulated by coastal proximity and wind direction, with the highest occurrence rates near shore under offshore winds. These patterns were found using the Discovery Engine, a general-purpose automated system for scientific discovery, which identifies complex relationships in data without prior hypotheses. The Discovery Engine uncovered three distinct mechanisms responsible for breakdowns in MOST assumptions: internal boundary layers formed by offshore continental flow, wave-driven wind jets associated with high wave age, and thermally stable boundary layers over cold sea surfaces where warm, moist air overlies cooler water far from shore. These findings highlight the limitations of current flux algorithms and suggest directions for improved parameterisation in coastal and open-ocean conditions.

physics.ao-ph