Winter-to-winter recurrence of sea surface temperature, salinity and mixed layer depth anomalies
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Regions characterised by a strong seasonal variation in MLD may display the phenomenon of re-emergence of winter-to-winter SSTA.
“Regions characterised by a strong seasonal variation in MLD may also display the phenomenon of re-emergence of winter-to-winter SSTA9–13.”
From Tendencies, variability and persistence of sea surface temperature anomalies (2020) · cites this paper as [12]
Winter SST anomalies persist at depth during the summer months below the shallow mixed layer, reemerging in the SSTA the following winter as the summer seasonal thermocline is eroded.
“Winter SST anomalies persist at depth during the summer months below the shallow mixed layer, reemerging in the SSTA the following winter as the summer seasonal thermocline is eroded.”
From Tendencies, variability and persistence of sea surface temperature anomalies (2020) · cites this paper as [12]
Winter-to-winter re-emergence is typically characterised by a time lag that can be variable, ranging from 7-13 months, and is usually seen in the mid-latitudes.
“This is typically characterised as winter-to-winter re-emergence although the time lag can be variable, ranging from 7–13 months15, and is usually seen in the mid-latitudes12,15–19.”
From Tendencies, variability and persistence of sea surface temperature anomalies (2020) · cites this paper as [12]
Cites
Temporal coherence in North Pacific sea-surface temperature patterns
Namias, J., & Born, R. M. (1970) · Journal of Geophysical Research · doi:10.1029/jc075i030p05952 · Cited by 161 · see citing works
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Tendencies, variability and persistence of sea surface temperature anomalies
Bulgin, C. E., Merchant, C. J., & Ferreira, D. (2020) · Scientific Reports · doi:10.1038/s41598-020-64785-9 · Cited by 150 · see citing works
Remote reemergence areas of winter sea surface temperature anomalies in the North Pacific
Sugimoto, S., & Hanawa, K. (2005) · Geophysical Research Letters · doi:10.1029/2004gl021410 · Cited by 71 · see citing works
- Authors
- Alexander, M. A., Timlin, M. S., & Scott, J. D.
- Affiliations
- National Oceanic and Atmospheric Administration (US)
- Corresponding author
- Alexander, Michael A
- Venue
- Progress in Oceanography
- Publisher
- Elsevier BV
- Published
- 2001
- Volume
- 49
- Issue
- 1-4
- Pages
- 41-61
- ISSN
- 0079-6611 (ISSN-L)
- OpenAlex
- W2007398168
- Cited by
- 65
- References
- 1
- Citations by year
- 2026: 1 · 2025: 2 · 2024: 6 · 2023: 1 · 2022: 1 · 2021: 3 · 2020: 6 · 2018: 2 · 2017: 3 · 2016: 4 · 2015: 2 · 2014: 2 · 2013: 2 · 2012: 2
- FWCI
- 2.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Progress In Oceanography (publishedVersion)
- Funders
- National Oceanic and Atmospheric Administration
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Keywords
- sea surface temperature anomalies, salinity anomalies, mixed layer depth, North Pacific, seasonal cycle, seasonal thermocline, vertical stratification, El Niño, tropical Pacific SST, ocean-atmosphere interaction
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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