Unlocking Southern Ocean Under-Ice Seasonality With a New Monthly Climatology

IF 3.4 2区 地球科学 Q1 OCEANOGRAPHY Journal of Geophysical Research-Oceans Pub Date : 2025-01-07 DOI:10.1029/2024JC020920
Kaihe Yamazaki, Nathaniel L. Bindoff, Helen Elizabeth Phillips, Maxim Nikurashin, Laura Herraiz-Borreguero, Paul Spence
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Abstract

The advent of under-ice profiling float and biologging techniques has enabled year-round observation of the Southern Ocean and its Antarctic margin. These under-ice data are often overlooked in widely used oceanographic datasets, despite their importance in understanding seasonality and its role in sea ice changes, water mass formation, and glacial melt. We develop a monthly climatology of the Southern Ocean (south of 40°S and above 2,000 m) using Data Interpolating Variational Analysis, which excels in multi-dimensional interpolation and consistent handling of topography and horizontal advection. The climatology successfully captures thermohaline variability under sea ice, previously hard to obtain, and outperforms other observation-based products and state estimate simulations in data fidelity, with smaller root-mean-square errors and biases. To demonstrate its multi-purpose capability, we present a qualitative description of the seasonal variation, including (a) the surface mixed layer, (b) the water mass volume census, (c) the Antarctic Slope Front, and (d) shelf bottom waters. The circumpolar variation in the extent of dense shelf water—including its presence outside the four major formation sites—and the annual volume overturning that reaches deep waters are revealed for the first time. The present work offers a new monthly climatology of the Southern Ocean and the Antarctic margin, which will be instrumental in investigating the seasonality and improving ocean models, thereby making valuable winter observations more accessible. We further highlight the quantitative significance of under-ice data in reproducing ocean conditions, advocating for their increased use to achieve a better Southern Ocean observing system.

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用新的月度气候学揭示南大洋冰下季节
冰下剖面、浮子和生物学技术的出现,使得对南大洋及其南极边缘的全年观测成为可能。这些冰下数据在广泛使用的海洋学数据集中经常被忽视,尽管它们对了解季节性及其在海冰变化、水团形成和冰川融化中的作用很重要。我们利用数据插值变分分析(Data interpolation Variational Analysis)建立了南大洋(40°S以南和2000 m以上)的月度气气学,该方法在多维插值和地形和水平平流的一致处理方面表现出色。气候学成功地捕获了海冰下的温盐变化,以前很难获得,并且在数据保真度方面优于其他基于观测的产品和状态估计模拟,均方根误差和偏差较小。为了证明其多用途能力,我们提出了季节变化的定性描述,包括(a)地表混合层,(b)水质量体积普查,(c)南极坡锋,以及(d)陆架底部水域。首次揭示了密集陆架水范围的极地变化,包括其在四个主要地层之外的存在,以及每年到达深水的体积翻转。目前的工作提供了一个新的南大洋和南极边缘的月度气候学,这将有助于研究季节性和改进海洋模式,从而使有价值的冬季观测更容易获得。我们进一步强调了冰下数据在再现海洋状况方面的定量意义,提倡增加使用冰下数据,以实现更好的南大洋观测系统。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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