Articles | Volume 20, issue 3
https://doi.org/10.5194/os-20-817-2024
https://doi.org/10.5194/os-20-817-2024
Research article
 | 
18 Jun 2024
Research article |  | 18 Jun 2024

Anomalous North Pacific subtropical mode water volume and density decrease in a recent stable Kuroshio Extension period from Argo observations

Jing Sheng, Cong Liu, Yanzhen Gu, Peiliang Li, Fangguo Zhai, and Ning Zhou

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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. 
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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.
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