Internal Tides From SWOT: A 75-Day Instantaneous Mode-1 M 2 ${\mathrm{M}}_{2}$ Internal Tide Model

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Zhongxiang Zhao
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Abstract

Seventy-five days of sea surface height measurements made by the Surface Water and Ocean Topography (SWOT) mission from 7 September to 21 November 2023 are used to explore SWOT's capability of observing internal tides. Mode-1 M 2 ${\mathrm{M}}_{2}$ internal tides are mapped by our updated mapping technique. SWOT-75d represents a 75-day instantaneous model. Nadir-30y is constructed using 30 years of nadir altimetry data from 1993 to 2022 and represents a climate normal. The nadir altimetry data in 2023 are used for model evaluation. Despite its large errors, SWOT-75d reveals the basic features of the global mode-1 M 2 ${\mathrm{M}}_{2}$ internal tide field, and causes positive variance reduction in regions of strong internal tides. Nadir-30y performs better overall, but SWOT-75d performs better in the tropical South Atlantic Ocean, the central North Pacific Ocean, and the Melanesian region. Evaluation using seasonally subsetted altimetry data reveals that M 2 ${\mathrm{M}}_{2}$ internal tides have significant temporal variations. SWOT-75d performs the best in fall, because the model is constructed using data largely in fall. SWOT-75d has large phase anomalies, which are spatially smoothed and used to adjust the phases in Nadir-30y. The phase-adjusted model can better make internal tide correction for SWOT and its performance is improved by 20%. Our results demonstrate that (a) mode-1 M 2 ${\mathrm{M}}_{2}$ internal tides can be extracted from 75 days of SWOT data by our mapping technique, and (b) the instantaneous internal tide model can be used to improve internal tide correction for SWOT.

来自 SWOT 的内潮:75 天瞬时模式-1 M 2 ${mathrm{M}}_{2}$ 内潮模型
由地表水和海洋地形(SWOT)任务于2023年9月7日至11月21日进行的75天海面高度测量用于探索SWOT观测内部潮汐的能力。Mode-1 m2 ${\mathrm{M}}_{2}$内部潮汐通过我们更新的映射技术进行映射。SWOT-75d是一个75天的瞬时模型。nadir -30y是根据1993年至2022年30年的最低点高度数据构建的,代表气候正常。2023年的最低点测高数据用于模式评估。尽管误差较大,但swt -75d揭示了全球模态1 M 2 ${\ mathm {M}}_{2}$内潮场的基本特征,并在强内潮区引起正方差减小。Nadir-30y总体表现更好,但SWOT-75d在热带南大西洋、北太平洋中部和美拉尼西亚地区表现更好。利用季节亚集高程资料进行评价,发现m2 ${\ mathm {M}}_{2}$内部潮汐具有显著的时间变化。SWOT-75d在秋季表现最好,因为该模型主要是使用秋季的数据构建的。SWOT-75d具有较大的相位异常,将其空间平滑并用于调整Nadir-30y的相位。相位调整模型能更好地对SWOT进行内部潮汐校正,其性能提高20%。结果表明:(a)利用我们的映射技术可以从75天的SWOT数据中提取出model -1 m2 ${\mathrm{M}}_{2}$内部潮汐,(b)瞬时内部潮汐模型可以用来改进SWOT的内部潮汐校正。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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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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