Abstract

Sea spray can contribute significantly to the exchanges of heat and momentum across the air–sea interface. However, while critical, sea spray physics are typically not included in operational atmospheric and oceanic models due to large uncertainties in their parameterizations. In large part, this is because of the scarcity of in-situ sea spray observations which prevent rigorous validation of existing sea spray models. Moreover, while sea spray is critically produced through the fundamental interactions between wind and waves, traditionally, sea spray models are parameterized in terms of wind properties only. In this study, we present novel in-situ observations of sea spray derived from a laser altimeter through the adoption of the Beer–Lambert law. Observations of sea spray cover a broad range of wind and wave properties and are used to develop a wind–wave-dependent sea spray volume flux model. Improved performance of the model is observed when wave properties are included, in contrast to a parameterization based on wind properties alone. The novel in-situ sea spray observations and the predictive model derived here are consistent with the classic spray model in both trend and magnitude. Our model and novel observations provide opportunities to improve the prediction of air–sea fluxes in operational weather forecasting models.

Highlights

  • Sea spray comprises small water droplets ejected from the sea surface and is of great significance to weather and climate processes [1]

  • When sea spray droplets are separated from the wave crest and released into the air, the droplets accelerate towards the local wind speed [2,3,4,5]

  • It was reported that spray induced heat flux contributes to more than 10% of the total air–sea heat flux for near surface wind speeds larger than 12 m s−1, while its contribution would become larger than the air–sea heat flux produced directly at the ocean surface once the wind speed exceeds about 30 m s−1 [13]

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Summary

Introduction

Sea spray comprises small water droplets ejected from the sea surface and is of great significance to weather and climate processes [1]. Sea spray extracts momentum from the atmosphere and reduces the wind speed near the ocean surface [6]. When the heaviest droplets re-enter the ocean, part of the momentum they gained is transferred directly to the ocean surface [7] and as a result, sea spray can contribute to momentum exchange between the upper ocean and the atmosphere and alter the stability of the air–sea boundary layer [8,9,10,11]. As sea spray can contribute significantly to the momentum, heat, and water vapor flux exchange between the atmosphere and ocean [4,12,14,15], accurate prediction of how much spray is produced at the air–sea boundary is of critical importance

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