Study of relationship between wave transport and sea surface temperature anomaly (SSTA) in the tropical Pacific

Shi, Yanxin; Wu, Kejian; Zhu, Xianye; Yang, Fan; Zhang, Yuming

doi:10.1007/s13131-016-0928-4

Cited by 5 publications

(7 citation statements)

References 11 publications

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“…The effect of wave transport on the upper ocean is of the same order of magnitude as Ekman transport (Kern, 1970) and it is confirmed by Bi et al (2012) and Shi et al (2016). In particular, the northward wave transport in the Southern Ocean inevitably transmits abnormal signals from high latitudes to low latitudes.…”

Section: Relationship Between Northward Wave Transport and El Niñomentioning

confidence: 68%

Large‐Scale Signals in the South Pacific Wave Fields Related to ENSO

et al. 2021

JGR Oceans

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Variability of the sea surface temperature (SST) in the equatorial Pacific plays an important role in the global climate. The El Niño-Southern Oscillation (ENSO) is a typical abnormal climate phenomenon. The ocean experiences both El Niño and La Niña climate patterns; however, the mechanism of El Niño is still not fully understood (L'Heureux et al., 2017;Li et al., 2019). Growing and breaking ocean waves play an important role in air-sea momentum and heat transfer and affect the mixing of the upper ocean (Janssen et al., 2013). Multiple large-scale effects of waves have been studied, including the driving effect of waves on ocean currents (

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Section: Relationship Between Northward Wave Transport and El Niñomentioning

confidence: 68%

Large‐Scale Signals in the South Pacific Wave Fields Related to ENSO

et al. 2021

JGR Oceans

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“…Shi et al. (2016) compared these two transports in mid‐ and low‐latitude regions of the Pacific Ocean, and found that their magnitudes were the same. Bi et al.…”

Section: Wave Transport In the Indian Oceanmentioning

confidence: 99%

“…It has been shown that wave‐induced water transport due to SD can affect a wide range of ocean states in dramatic ways (Hasselmann, 1971). The magnitude of SD can reach the same as that of wind transport in high‐ and mid‐latitude oceans (McWilliams & Restrepo, 1999; Shi et al., 2016). Tamura et al.…”

Section: Introductionmentioning

confidence: 99%

“…It has been shown that wave-induced water transport due to SD can affect a wide range of ocean states in dramatic ways (Hasselmann, 1971). The magnitude of SD can reach the same as that of wind transport in high-and mid-latitude oceans (McWilliams & Restrepo, 1999;Shi et al, 2016). Tamura et al (2012) proposed that SD plays an important role in the momentum balance of the upper ocean through introduction into the average Eulerian flow.…”

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confidence: 99%

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Relating a Large‐Scale Variation of Waves in the Indian Ocean to the IOD

et al. 2022

JGR Oceans

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Wind-generated ocean surface waves give rise to a near-surface velocity known as Stokes drift (SD) (Stokes, 1847), which can contribute substantially to near-surface mass transport. SD is widely applied in representation of nearshore circulation in coastal zones and in modeling of tracer transport as the difference between Lagrangian and Eulerian averages, and it is responsible for the Coriolis-Stokes force in the upper-ocean layer in Eulerian models (van den Bremer & Breivik, 2018). It has been shown that wave-induced water transport due to SD can affect a wide range of ocean states in dramatic ways (Hasselmann, 1971). The magnitude of SD can reach the same as that of wind transport in high-and mid-latitude oceans (McWilliams & Restrepo, 1999;Shi et al., 2016). Tamura et al. (2012) proposed that SD plays an important role in the momentum balance of the upper ocean through introduction into the average Eulerian flow. Moreover, SD also influences the mixed layer of the ocean by causing Langmuir turbulence generation (McWilliams et al., 2014).

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“…Temperature anomaly has various definition among researchers (Efimov & Barabanov, 2017;Kiselev, 2016;Shi et al, 2016). It refers to unique temperature condition which appear at hours before earthquake and after earthquake (Akhoondzadeh, 2013).…”

Section: Introductionmentioning

confidence: 99%

Identification of Sea Surface Temperature Anomaly during Earthquake in Southern Java Island using Google Earth Engine Datasets

Rusydi

Masitoh

2023

IJG

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The certainty of Sea Surface Temperature (SST) anomaly during earthquakes in Java Island was still not clear identified. This research tried to identify any possibilities of SST anomaly during earthquake in Southern Java Island. It used Google Earth Engine datasets including daily NOAA Climate Data Record (CDR) - Woods Hole Oceanographic Institution (WHOI): Sea Surface Temperature Version 2 which has resolution of 0.25 arc degrees for 20 years and processed them to depict SST trends in pre-earthquake and post-earthquake situation. The statistic test of t-Test Paired Two Sample was also applied to certain the significant difference of SST in both situations. SST fluctuation during the earthquake was still inconsistent and unclear to consider as an anomaly. There were other complicated factors excluding earthquake to influence SST fluctuation. The earthquake did not trigger directly to fluctuate SST, even not to make it being an anomaly.

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Study of relationship between wave transport and sea surface temperature anomaly (SSTA) in the tropical Pacific

Cited by 5 publications

References 11 publications

Large‐Scale Signals in the South Pacific Wave Fields Related to ENSO

Large‐Scale Signals in the South Pacific Wave Fields Related to ENSO

Relating a Large‐Scale Variation of Waves in the Indian Ocean to the IOD

Identification of Sea Surface Temperature Anomaly during Earthquake in Southern Java Island using Google Earth Engine Datasets

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