Articles | Volume 20, issue 3
https://doi.org/10.5194/os-20-817-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-20-817-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Anomalous North Pacific subtropical mode water volume and density decrease in a recent stable Kuroshio Extension period from Argo observations
Jing Sheng
Hainan Institute, Zhejiang University, Sanya, 572000, China
Ocean College, Zhejiang University, Zhoushan, 316000, China
Hainan Institute, Zhejiang University, Sanya, 572000, China
Hainan Observation and Research Station of Ecological Environment and Fishery Resource in Yazhou Bay, Sanya, 572000, China
Yanzhen Gu
CORRESPONDING AUTHOR
Hainan Institute, Zhejiang University, Sanya, 572000, China
Ocean College, Zhejiang University, Zhoushan, 316000, China
Hainan Observation and Research Station of Ecological Environment and Fishery Resource in Yazhou Bay, Sanya, 572000, China
Peiliang Li
Hainan Institute, Zhejiang University, Sanya, 572000, China
Ocean College, Zhejiang University, Zhoushan, 316000, China
Hainan Observation and Research Station of Ecological Environment and Fishery Resource in Yazhou Bay, Sanya, 572000, China
Fangguo Zhai
College of Oceanic and Atmospheric Science, Ocean University of China, Qingdao, 266000, China
Ning Zhou
Hainan Institute, Zhejiang University, Sanya, 572000, China
Ocean College, Zhejiang University, Zhoushan, 316000, China
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Previous studies show that only when water flows into and out of the Luzon Strait (LS), material and energy exchange between the South China Sea (SCS) and the Northwest Pacific (NWP) will take place. However, our studies demonstrate that mesoscale eddies in the NWP can transfer vorticity to mesoscale eddies in the SCS, without water exchange in the LS. This provides a new perspective for the study of material and energy exchange between the SCS and NWP.
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Salar Karam, Céline Heuzé, Mario Hoppmann, and Laura de Steur
Ocean Sci., 20, 917–930, https://doi.org/10.5194/os-20-917-2024, https://doi.org/10.5194/os-20-917-2024, 2024
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A long-term mooring array in the Fram Strait allows for an evaluation of decadal trends in temperature in this major oceanic gateway into the Arctic. Since the 1980s, the deep waters of the Greenland Sea and the Eurasian Basin of the Arctic have warmed rapidly at a rate of 0.11°C and 0.05°C per decade, respectively, at a depth of 2500 m. We show that the temperatures of the two basins converged around 2017 and that the deep waters of the Greenland Sea are now a heat source for the Arctic Ocean.
Helene Asbjørnsen, Tor Eldevik, Johanne Skrefsrud, Helen L. Johnson, and Alejandra Sanchez-Franks
Ocean Sci., 20, 799–816, https://doi.org/10.5194/os-20-799-2024, https://doi.org/10.5194/os-20-799-2024, 2024
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The Gulf Stream system is essential for northward ocean heat transport. Here, we use observations along the path of the extended Gulf Stream system and an observationally constrained ocean model to investigate variability in the Gulf Stream system since the 1990s. We find regional differences in the variability between the subtropical, subpolar, and Nordic Seas regions, which warrants caution in using observational records at a single latitude to infer large-scale circulation change.
Herlé Mercier, Damien Desbruyères, Pascale Lherminier, Antón Velo, Lidia Carracedo, Marcos Fontela, and Fiz F. Pérez
Ocean Sci., 20, 779–797, https://doi.org/10.5194/os-20-779-2024, https://doi.org/10.5194/os-20-779-2024, 2024
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We study the Atlantic Meridional Overturning Circulation (AMOC) measured between Greenland and Portugal between 1993–2021. We identify changes in AMOC limb volume and velocity as two major drivers of AMOC variability at subpolar latitudes. Volume variations dominate on the seasonal timescale, while velocity variations are more important on the decadal timescale. This decomposition proves useful for understanding the origin of the differences between AMOC time series from different analyses.
Romain Caneill, Fabien Roquet, and Jonas Nycander
Ocean Sci., 20, 601–619, https://doi.org/10.5194/os-20-601-2024, https://doi.org/10.5194/os-20-601-2024, 2024
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In winter, heat loss increases density at the surface of the Southern Ocean. This increase in density creates a mixed layer deeper than 250 m only in a narrow deep mixing band (DMB) located around 50° S. North of the DMB, the stratification is too strong to be eroded, so mixed layers are shallower. The density of cold water is almost not impacted by temperature changes. Thus, heat loss does not significantly increase the density south of the DMB, so no deep mixed layers are produced.
Harry Bryden, Jordi Beunk, Sybren Drijfhout, Wilco Hazeleger, and Jennifer Mecking
Ocean Sci., 20, 589–599, https://doi.org/10.5194/os-20-589-2024, https://doi.org/10.5194/os-20-589-2024, 2024
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There is widespread interest in whether the Gulf Stream will decline under global warming. We analyse 19 coupled climate model projections of the AMOC over the 21st century. The model consensus is that the AMOC will decline by about 40 % due to reductions in northward Gulf Stream transport and southward deep western boundary current transport. Whilst the wind-driven Gulf Stream decreases by 4 Sv, most of the decrease in the Gulf Stream is due to a reduction of 7 Sv in its thermohaline component.
Jessica Kolbusz, Jan Zika, Charitha Pattiaratchi, and Alan Jamieson
Ocean Sci., 20, 123–140, https://doi.org/10.5194/os-20-123-2024, https://doi.org/10.5194/os-20-123-2024, 2024
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We collected observations of the ocean environment at depths over 6000 m in the Southern Ocean, Indian Ocean, and western Pacific using sensor-equipped landers. We found that trench locations impact the water characteristics over these depths. Moving northward, they generally warmed but differed due to their position along bottom water circulation paths. These insights stress the importance of further research in understanding the environment of these deep regions and their importance.
Jinling Lu, Ling Du, and Shuhao Tao
Ocean Sci., 19, 1773–1789, https://doi.org/10.5194/os-19-1773-2023, https://doi.org/10.5194/os-19-1773-2023, 2023
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With the recent developments in observations and reanalysis data in the Beaufort Gyre, we investigate an improved understanding of eddy activity and asymmetrical halocline variability in the upper ocean. The halocline structures on the southern and northern sides of the central gyre have tended to be identical since 2014. The results suggest that enhanced eddy modulation through eddy fluxes influences oceanic stratification, resulting in reduced meridional asymmetry of the halocline.
Enrico P. Metzner and Marc Salzmann
Ocean Sci., 19, 1453–1464, https://doi.org/10.5194/os-19-1453-2023, https://doi.org/10.5194/os-19-1453-2023, 2023
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The Arctic Ocean cold halocline separates the cold surface mixed layer from the underlying warm Atlantic Water, and thus provides a precondition for sea ice formation. Here, we introduce a new method for detecting the halocline base and compare it to two existing methods. We show that the largest differences between the methods are found in the regions that are most prone to a halocline retreat in a warming climate, and we discuss the advantages and disadvantages of the three methods.
Bogi Hansen, Karin M. H. Larsen, Hjálmar Hátún, Steffen M. Olsen, Andrea M. U. Gierisch, Svein Østerhus, and Sólveig R. Ólafsdóttir
Ocean Sci., 19, 1225–1252, https://doi.org/10.5194/os-19-1225-2023, https://doi.org/10.5194/os-19-1225-2023, 2023
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Based on in situ observations combined with sea level anomaly (SLA) data from satellite altimetry, volume as well as heat (relative to 0 °C) transport of the Iceland–Faroe warm-water inflow towards the Arctic (IF inflow) increased from 1993 to 2021. The reprocessed SLA data released in December 2021 represent observed variations accurately. The IF inflow crosses the Iceland–Faroe Ridge in two branches, with retroflection in between. The associated coupling to overflow reduces predictability.
Cited articles
Akima, H.: A new method of interpolation and smooth curve fitting based on local procedures, J. ACM JACM, 17, 589–602, 1970.
Argo: Argo float data and metadata from Global Data Assembly Centre (Argo GDAC), SEANOE [data set], https://doi.org/10.17882/42182, 2000.
Bond, N. A. and Cronin, M. F.: Regional Weather Patterns during Anomalous Air–Sea Fluxes at the Kuroshio Extension Observatory (KEO), J. Clim., 21, 1680–1697, https://doi.org/10.1175/2007JCLI1797.1, 2008.
Cerovečki, I. and Giglio, D.: North Pacific Subtropical Mode Water Volume Decrease in 2006–09 Estimated from Argo Observations: Influence of Surface Formation and Basin-Scale Oceanic Variability, J. Clim., 29, 2177–2199, https://doi.org/10.1175/JCLI-D-15-0179.1, 2016.
Cerovečki, I. and Marshall, J.: Eddy modulation of air–sea interaction and convection, J. Phys. Oceanogr., 38, 65–83, 2008.
Cerovečki, I., Hendershott, M. C., and Yulaeva, E.: Strong North Pacific Subtropical Mode Water Volume and Density Decrease in Year 1999, J. Geophys. Res.-Ocean., 124, 6617–6631, https://doi.org/10.1029/2019JC014956, 2019.
Cushman-Roisin, B.: Subduction. Dynamics of the oceanic surface mixed layer: Proc. 'Aha Huliko'a Hawaiian winter Workshop, Vol. 181, p. 196, University of Hawaii at Manoa, 1987.
Davis, X. J., Rothstein, L. M., Dewar, W. K., and Menemenlis, D.: Numerical Investigations of Seasonal and Interannual Variability of North Pacific Subtropical Mode Water and Its Implications for Pacific Climate Variability, J. Clim., 24, 2648–2665, https://doi.org/10.1175/2010JCLI3435.1, 2011.
Garrett, C. and Tandon, A.: The effects on water mass formation of surface mixed layer timedependence and entrainment fluxes, Deep-Sea Res. Pt. I, 44, 1991–2006, 1997.
Global Ocean Gridded: Global Ocean Gridded L 4 Sea Surface Heights And Derived Variables Reprocessed 1993 Ongoing, E.U. Copernicus Marine Service Information (CMEMS), Marine Data Store (MDS) [data set], https://doi.org/10.48670/moi-00148, 2023a.
Global Ocean Gridded: Global Ocean Gridded L 4 Sea Surface Heights And Derived Variables Nrt, E.U. Copernicus Marine Service Information (CMEMS), Marine Data Store (MDS) [data set], https://doi.org/10.48670/moi-00149, 2023b.
Guo, Y., Lin, X., Wei, M., Liu, C., and Men, G.: Decadal Variability of North Pacific Eastern Subtropical Mode Water, J. Geophys. Res.-Ocean., 123, 6189–6206, https://doi.org/10.1029/2018JC013890, 2018.
Hanawa, K. and Kamada, J.: Variability of core layer temperature (CLT) of the North Pacific Subtropical Mode Water, Geophys. Res. Lett., 28, 2229–2232, https://doi.org/10.1029/2000GL011716, 2001.
Hanawa, K. and Sugimoto, S.: “Reemergence” areas of winter sea surface temperature anomalies in the world's oceans, Geophys. Res. Lett., 31, L10303, https://doi.org/10.1029/2004GL019904, 2004.
Hersbach, H., Bell, B., Berrisford, P., Biavati, G., Horányi, A., Muñoz Sabater, J., Nicolas, J., Peubey, C., Radu, R., Rozum, I., Schepers, D., Simmons, A., Soci, C., Dee, D., and Thépaut, J.-N.: ERA5 monthly averaged data on single levels from 1979 to present, Copernic. Clim. Change Serv. C3S Clim. Data Store CDS, 10, 252–266, 2019.
Holbrook, N. J., Scannell, H. A., Sen Gupta, A., Benthuysen, J. A., Feng, M., Oliver, E. C. J., Alexander, L. V., Burrows, M. T., Donat, M. G., Hobday, A. J., Moore, P. J., Perkins-Kirkpatrick, S. E., Smale, D. A., Straub, S. C., and Wernberg, T.: A global assessment of marine heatwaves and their drivers, Nat. Commun., 10, 2624, https://doi.org/10.1038/s41467-019-10206-z, 2019.
Hosoda, S.: Grid Point Value of the Monthly Objective Analysis using the Argo data, JAMSTEC [data set], https://doi.org/10.17596/0000102, 2007.
Hosoda, S., Ohira, T., and Nakamura, T.: A monthly mean dataset of global oceanic temperature and salinity derived from Argo float observations, JAMSTEC Rep. Res. Dev., 8, 47–59, 2008.
Hu, H., Liu, Q., Zhang, Y., and Liu, W.: Variability of subduction rates of the subtropical North Pacific mode waters, Chin. J. Oceanol. Limnol., 29, 1131–1141, 2011.
Kawakami, Y., Nakano, H., Urakawa, L. S., Toyoda, T., Aoki, K., and Usui, N.: Northward shift of the Kuroshio Extension during 1993–2021, Sci. Rep., 13, 16223, https://doi.org/10.1038/s41598-023-43009-w, 2023.
Kuroda, H. and Setou, T.: Extensive Marine Heatwaves at the Sea Surface in the Northwestern Pacific Ocean in Summer 2021, Remote Sens., 13, 3989, https://doi.org/10.3390/rs13193989, 2021.
Levitus, S.: Climatological atlas of the world ocean, p. 173, US Government Printing Office, NOAA professional paper 13, 1982.
Liu, C., Xie, S., Li, P., Xu, L., and Gao, W.: Climatology and decadal variations in multicore structure of the North Pacific subtropical mode water, J. Geophys. Res.-Ocean., 122, 7506–7520, https://doi.org/10.1002/2017JC013071, 2017.
Mantua, N.: The Pacific Decadal Oscillation: a brief overview for non-specialists, Encycl. Environ. Change, Joint Institute for the Study of the Atmosphere and Oceans University of Washington, Seattle, Washington, USA, 1999.
Marshall, D.: Subduction of water masses in an eddying ocean, J. Mar. Res., 55, 201–222, https://doi.org/10.1357/0022240973224373, 1997.
Marshall, J., Jamous, D., and Nilsson, J.: Reconciling thermodynamic and dynamic methods of computation of water-mass transformation rates, Deep-Sea Res. Pt. I, 46, 545–572, https://doi.org/10.1016/S0967-0637(98)00082-X, 1999.
Masuzawa, J.: Subtropical mode water, Deep-Sea Res. Oceanogr. Abstr., 16, 463–468, https://doi.org/10.1016/0011-7471(69)90034-5, 1969.
Newman, M., Alexander, M. A., Ault, T. R., Cobb, K. M., Deser, C., Di Lorenzo, E., Mantua, N. J., Miller, A. J., Minobe, S., Nakamura, H., Schneider, N., Vimont, D. J., Phillips, A. S., Scott, J. D., and Smith, C. A.: The Pacific Decadal Oscillation, Revisited, J. Clim., 29, 4399–4427, https://doi.org/10.1175/JCLI-D-15-0508.1, 2016.
Nishikawa, S., Tsujino, H., Sakamoto, K., and Nakano, H.: Diagnosis of water mass transformation and formation rates in a high-resolution GCM of the North Pacific: DIAGNOSIS OF WATER MASS TRANSFORMATION, J. Geophys. Res.-Ocean., 118, 1051–1069, https://doi.org/10.1029/2012JC008116, 2013.
Oka, E. and Qiu, B.: Progress of North Pacific mode water research in the past decade, J. Oceanogr., 68, 5–20, https://doi.org/10.1007/s10872-011-0032-5, 2012.
Oka, E., Talley, L. D., and Suga, T.: Temporal variability of winter mixed layer in the mid-to high-latitude North Pacific, J. Oceanogr., 63, 293–307, https://doi.org/10.1007/s10872-007-0029-2, 2007.
Oka, E., Suga, T., Sukigara, C., Toyama, K., Shimada, K., and Yoshida, J.: “Eddy Resolving” Observation of the North Pacific Subtropical Mode Water, J. Phys. Oceanogr., 41, 666–681, https://doi.org/10.1175/2011JPO4501.1, 2011.
Oka, E., Qiu, B., Takatani, Y., Enyo, K., Sasano, D., Kosugi, N., Ishii, M., Nakano, T., and Suga, T.: Decadal variability of Subtropical Mode Water subduction and its impact on biogeochemistry, J. Oceanogr., 71, 389–400, https://doi.org/10.1007/s10872-015-0300-x, 2015.
Oka, E., Yamada, K., Sasano, D., Enyo, K., Nakano, T., and Ishii, M.: Remotely Forced Decadal Physical and Biogeochemical Variability of North Pacific Subtropical Mode Water Over the Last 40 Years, Geophys. Res. Lett., 46, 1555–1561, https://doi.org/10.1029/2018GL081330, 2019.
Oka, E., Nishikawa, H., Sugimoto, S., Qiu, B., and Schneider, N.: Subtropical Mode Water in a recent persisting Kuroshio large-meander period: Part I – formation and advection over the entire distribution region, J. Oceanogr., 77, 781–795, 2021.
Qiu, B.: Interannual variability of the Kuroshio Extension system and its impact on the wintertime SST field, J. Phys. Oceanogr., 30, 1486–1502, 2000.
Qiu, B.: Kuroshio Extension Variability and Forcing of the Paci?c Decadal Oscillations: Responses and Potential Feedback, J. Phys. Oceanogr., 33, 2465–2482, https://doi.org/10.1175/1520-0485(2003)033<2465:KEVAFO>2.0.CO;2, 2003.
Qiu, B. and Chen, S.: Variability of the Kuroshio Extension Jet, Recirculation Gyre, and Mesoscale Eddies on Decadal Time Scales, J. Phys. Oceanogr., 35, 2090–2103, https://doi.org/10.1175/JPO2807.1, 2005.
Qiu, B. and Chen, S.: Decadal Variability in the Formation of the North Pacific Subtropical Mode Water: Oceanic versus Atmospheric Control, J. Phys. Oceanogr., 36, 1365–1380, https://doi.org/10.1175/JPO2918.1, 2006.
Qiu, B. and Chen, S.: Revisit of the occurrence of the Kuroshio large meander South of Japan, J. Phys. Oceanogr., 51, 3679–3694, 2021.
Qiu, B. and Kelly, K. A.: Upper-ocean heat balance in the Kuroshio Extension region, J. Phys. Oceanogr., 23, 2027–2041, 1993.
Qiu, B., Hacker, P., Chen, S., Donohue, K. A., Watts, D. R., Mitsudera, H., Hogg, N. G., and Jayne, S. R.: Observations of the Subtropical Mode Water Evolution from the Kuroshio Extension System Study, J. Phys. Oceanogr., 36, 457–473, https://doi.org/10.1175/JPO2849.1, 2006.
Qiu, B., Chen, S., and Hacker, P.: Effect of Mesoscale Eddies on Subtropical Mode Water Variability from the Kuroshio Extension System Study (KESS), J. Phys. Oceanogr., 37, 982–1000, https://doi.org/10.1175/JPO3097.1, 2007.
Qiu, B., Chen, S., Schneider, N., Oka, E., and Sugimoto, S.: On the reset of the wind-forced decadal Kuroshio Extension variability in late 2017, J. Clim., 33, 10813–10828, 2020.
Qiu, B., Chen, S., and Oka, E.: Why did the 2017 Kuroshio large meander event become the longest in the Past 70 years?, Geophys. Res. Lett., 50, e2023GL103548, https://doi.org/10.1029/2023GL103548, 2023.
Qu, T. and Chen, J.: A North Pacific decadal variability in subduction rate, Geophys. Res. Lett., 36, L22602, https://doi.org/10.1029/2009GL040914, 2009.
Rainville, L., Jayne, S. R., McClean, J. L., and Maltrud, M. E.: Formation of Subtropical Mode Water in a high-resolution ocean simulation of the Kuroshio Extension region, Ocean Model., 17, 338–356, https://doi.org/10.1016/j.ocemod.2007.03.002, 2007.
Rainville, L., Jayne, S. R., and Cronin, M. F.: Variations of the North Pacific Subtropical Mode Water from Direct Observations, J. Clim., 27, 2842–2860, https://doi.org/10.1175/JCLI-D-13-00227.1, 2014.
Roemmich, D. and Gilson, J.: The 2004–2008 mean and annual cycle of temperature, salinity, and steric height in the global ocean from the Argo Program, Prog. Oceanogr., 82, 81–100, 2009.
Sasaki, Y. N. and Minobe, S.: Climatological mean features and interannual to decadal variability of ring formations in the Kuroshio Extension region, J. Oceanogr., 71, 499–509, https://doi.org/10.1007/s10872-014-0270-4, 2015.
Small, R. J., Bryan, F. O., and Bishop, S. P.: Surface Water Mass Transformation in the Southern Ocean: The Role of Eddies Revisited, J. Phys. Oceanogr., 52, 789–804, https://doi.org/10.1175/JPO-D-21-0087.1, 2022.
Stammer, D.: Steric and wind-induced changes in TOPEX/POSEIDON large-scale sea surface topography observations, J. Geophys. Res.-Ocean., 102, 20987–21009, 1997.
Suga, T. and Hanawa, K.: The mixed-layer climatology in the northwestern part of the North Pacific subtropical gyre and the formation area of Subtropical Mode Water, J. Mar. Res., 48, 543–566, 1990.
Suga, T. and Hanawa, K.: Interannual variations of North Pacific subtropical mode water in the 137° E section, J. Phys. Oceanogr., 25, 1012–1017, 1995.
Suga, T., Hanawa, K., and Toba, Y.: Subtropical mode water in the 137 E section, J. Phys. Oceanogr., 19, 1605–1618, 1989.
Sugimoto, S. and Hanawa, K.: Remote reemergence areas of winter sea surface temperature anomalies in the North Pacific, Geophys. Res. Lett., 32, L01606, https://doi.org/10.1029/2004GL021410, 2005.
Sugimoto, S. and Hanawa, K.: Impact of Aleutian Low activity on the STMW formation in the Kuroshio recirculation gyre region: IMPACT OF AL ON THE STMW FORMATION, Geophys. Res. Lett., 37, L03606, https://doi.org/10.1029/2009GL041795, 2010.
Sugimoto, S. and Kako, S.: Decadal Variation in Winter Mixed Layer Depth South of the Kuroshio Extension and Its Influence on Winter Mixed Layer Temperature, J. Clim., 29, 1237–1252, https://doi.org/10.1175/JCLI-D-15-0206.1, 2016.
Tak, Y.-J., Song, H., and Cho, Y.-K.: Impact of the reemergence of North Pacific subtropical mode water on the multi-year modulation of marine heatwaves in the North Pacific Ocean during winter and early spring, Environ. Res. Lett., 16, 074036, https://doi.org/10.1088/1748-9326/ac0cad, 2021.
Taneda, T., Suga, T., and Hanawa, K.: Subtropical mode water variation in the northwestern part of the North Pacific subtropical gyre, J. Geophys. Res.-Ocean., 105, 19591–19598, https://doi.org/10.1029/2000JC900073, 2000.
Tomita, H., Kako, S., Cronin, M. F., and Kubota, M.: Preconditioning of the wintertime mixed layer at the Kuroshio Extension Observatory, J. Geophys. Res.-Ocean., 115, 2010JC006373, https://doi.org/10.1029/2010JC006373, 2010.
Toyama, K., Iwasaki, A., and Suga, T.: Interannual Variation of Annual Subduction Rate in the North Pacific Estimated from a Gridded Argo Product, J. Phys. Oceanogr., 45, 2276–2293, https://doi.org/10.1175/JPO-D-14-0223.1, 2015.
Uehara, H., Suga, T., Hanawa, K., and Shikama, N.: A role of eddies in formation and transport of North Pacific Subtropical Mode Water: MESOSCALE EDDIES AND NPSTMW, Geophys. Res. Lett., 30, 1705, https://doi.org/10.1029/2003GL017542, 2003.
Usui, N.: Progress of Studies on Kuroshio Path Variations South of Japan in the Past Decade, in: Geophysical Monograph Series, edited by: Nagai, T., Saito, H., Suzuki, K., and Takahashi, M., Wiley, 147–161, https://doi.org/10.1002/9781119428428.ch9, 2019.
Vivier, F., Kelly, K. A., and Thompson, L.: Contributions of wind forcing, waves, and surface heating to sea surface height observations in the Pacific Ocean, J. Geophys. Res.-Ocean., 104, 20767–20788, 1999.
Walin, G.: On the relation between sea-surface heat flow and thermal circulation in the ocean, Tellus, 34, 187–195, https://doi.org/10.1111/j.2153-3490.1982.tb01806.x, 1982.
Wang, R., Yu, F., and Nan, F.: Weakening of subduction in the Subtropical Mode Water formation region observed during 2003–2013, J. Geophys. Res.-Ocean., 120, 7271–7281, 2015.
Williams, R. G.: The influence of air–sea interaction on the ventilated thermocline, J. Phys. Oceanogr., 19, 1255–1267, 1989.
Williams, R. G.: The role of the mixed layer in setting the potential vorticity of the main thermocline, J. Phys. Oceanogr., 21, 1803–1814, 1991.
Wu, B., Lin, X., and Yu, L.: North Pacific subtropical mode water is controlled by the Atlantic Multidecadal Variability, Nat. Clim. Change, 10, 238–243, https://doi.org/10.1038/s41558-020-0692-5, 2020.
Wu, B., Lin, X., and Yu, L.: Poleward Shift of the Kuroshio Extension Front and Its Impact on the North Pacific Subtropical Mode Water in the Recent Decades, J. Phys. Oceanogr., 51, 457–474, https://doi.org/10.1175/JPO-D-20-0088.1, 2021.
Xu, L., Wang, K., and Wu, B.: Weakening and Poleward Shifting of the North Pacific Subtropical Fronts from 1980 to 2018, J. Phys. Oceanogr., 52, 399–417, https://doi.org/10.1175/JPO-D-21-0170.1, 2022.
Short summary
The homogeneous water column, named mode water, retains atmosphere conditions and biogeochemical elements from the deep winter mixed layer and became weaker and warmer in the North Pacific subtropical ocean in 2018–2021 even though the Kuroshio Extension was stable. Locally anomalous east wind transporting warm water to the north and enhanced near-surface stratification hinder the deepening of the winter mixed layer. This study has broad implications for climate change and biogeochemical cycles.
The homogeneous water column, named mode water, retains atmosphere conditions and biogeochemical...