Optimizing mooring placement to constrain southern ocean air-sea fluxes

Proposals from multiple nations to deploy airsea flux moorings in the Southern Ocean have raised the question of how to optimize the placement of these moorings in order to maximize their utility, both as contributors to the network of observations assimilated in numerical weather prediction and als...

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Bibliographic Details
Published in:Journal of Atmospheric and Oceanic Technology
Main Authors: Wei, Y, Gille, ST, Mazloff, MR, Tamsitt, V, Swart, S, Chen, D, Newman, L
Format: Article in Journal/Newspaper
Language:English
Published: Amer Meteorological Soc 2020
Subjects:
Online Access:https://doi.org/10.1175/JTECH-D-19-0203.1
http://ecite.utas.edu.au/142930
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Summary:Proposals from multiple nations to deploy airsea flux moorings in the Southern Ocean have raised the question of how to optimize the placement of these moorings in order to maximize their utility, both as contributors to the network of observations assimilated in numerical weather prediction and also as a means to study a broad range of processes driving airsea fluxes. This study, developed as a contribution to the Southern Ocean Observing System (SOOS), proposes criteria that can be used to determine mooring siting to obtain best estimates of net airsea heat flux ( Q net ). Flux moorings are envisioned as one component of a multiplatform observing system, providing valuable in situ point time series measurements to be used alongside satellite data and observations from autonomous platforms and ships. Assimilating models (e.g., numerical weather prediction and reanalysis products) then offer the ability to synthesize the observing system and map properties between observations. This paper develops a framework for designing mooring array configurations to maximize the independence and utility of observations. As a test case, within the meridional band from 35 to 65S we select eight mooring sites optimized to explain the largest fraction of the total variance (and thus to ensure the least variance of residual components) in the area south of 20S. Results yield different optimal mooring sites for low-frequency interannual heat fluxes compared with higher-frequency subseasonal fluxes. With eight moorings, we could explain a maximum of 24.6% of high-frequency Q net variability or 44.7% of low-frequency Q net variability.