LORA: a local ensemble transform Kalman filter-based ocean research analysis
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Published:2023-03-18
Issue:3-4
Volume:73
Page:117-143
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ISSN:1616-7341
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Container-title:Ocean Dynamics
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language:en
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Short-container-title:Ocean Dynamics
Author:
Ohishi ShunORCID, Miyoshi Takemasa, Kachi Misako
Abstract
AbstractWe have produced an eddy-resolving local ensemble transform Kalman filter (LETKF)-based ocean research analysis (LORA) for the western North Pacific (WNP) and Maritime Continent (MC) regions (LORA-WNP and LORA-MC, respectively). This paper describes the system configuration and validation comparisons with Japan Coastal Ocean Predictability Experiment 2M (JCOPE2M) reanalysis and Archiving, Validation, and Interpretation of Satellite Oceanographic Data (AVISO) observational datasets. The results show that the surface horizontal velocity in the LORA-WNP is closer to independent drifter buoy observations in the mid-latitude region, especially along the Kuroshio Extension (KE), and is less close in the subtropical region than the JCOPE2M, although the AVISO is the closest over the whole domain. The sea surface temperatures (SSTs) in the LORA-WNP correspond better to assimilated satellite observations than the JCOPE2M over most of the domain except for coastal regions. The results using an independent buoy south of the KE indicate that better fit of temperature in the LORA-WNP may be limited to the upper 300 m depth, probably because of the prescribed vertical localization cutoff length of 370 m. In the MC region, the surface velocity in the LORA-MC is closer to the independent drifter buoys in the equatorial coastal region and is less close in the offshore region than the AVISO. The SSTs in the LORA-MC correspond better to the assimilated satellite observations in the offshore region than the nearshore region. Therefore, the LORA-WNP and LORA-MC have sufficient accuracy for geoscience research applications as well as for fisheries, marine transport, and environment consultants.
Funder
Japan Science and Technology Corporation MEXT JSPS KAKENHI
Publisher
Springer Science and Business Media LLC
Reference88 articles.
1. Amante C, Eakins BW (2009) ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis. NOAA technical memorandum NESDIS NGDC-24. National geophysical data center, NOAA. https://doi.org/10.7289/V5C8276M 2. Balmaseda MA, Hernandez F, Storto A, Palmer MD, Alves O, Shi L, Smith GC, Toyoda T, Valdivieso M, Barnier B, Behringer D, Boyer T, Chang YS, Chepurin GA, Ferry N, Forget G, Fujii Y, Good S, Guinehut S, Haines K, Ishikawa Y, Keeley S, Köhl A, Lee T, Martin MJ, Masina S, Masuda S, Meyssignac B, Mogensen K, Parent L, Peterson KA, Tang YM, Yin Y, Vernieres G, Wang X, Waters J, Wedd R, Wang O, Xue Y, Chevallier M, Lemieux JF, Dupont F, Kuragano T, Kamachi M, Awaji T, Caltabiano A, Wilmer-Becker K, Gaillard F (2015) The ocean reanalyses intercomparison project (ORA-IP). J Oper Oceanogr 8:s80–s97. https://doi.org/10.1080/1755876X.2015.1022329 3. Bessho K, Date K, Hayashi M, Ikeda A, Imai T, Inoue H, Kumagai Y, Miyakawa T, Murata H, Ohno T, Okuyama A, Oyama R, Sasaki Y, Shimazu Y, Shimoji K, Sumida Y, Suzuki M, Taniguchi H, Tsuchiyama H, Uesawa D, Yokota H, Yoshida R (2016) An introduction to Himawari-8/9 – Japan’s new-generation geostationary meteorological satellites. J Meteorol Soc Japan 94:151–183. https://doi.org/10.2151/jmsj.2016-009 4. Bloom SC, Takacs LL, da Silva AM, Ledvina D (1996) Data assimilation using incremental analysis updates. Mon Weather Rev 124:1256–1271. https://doi.org/10.1175/1520-0493(1996)124%3c1256:DAUIAU%3e2.0.CO;2 5. Brodeau L, Barnier B, Gulev SK, Woods C (2017) Climatologically significant effects of some approximations in the bulk parameterizations of turbulent air–sea fluxes. J Phys Oceanogr 47:5–28. https://doi.org/10.1175/JPO-D-16-0169.1
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