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Modified Technique for Calculating the Parameters of Climatic Variability of Upwelling by Thermal Index

  • PHYSICAL BASES AND METHODS OF STUDYING THE EARTH FROM SPACE
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Abstract

A modified technique for calculating the amplitude-phase characteristics of the seasonal cycle and long-term trends in the intensity of upwelling is discussed based on an analysis of the minimum (maximum in the absolute value) values of the thermal upwelling index (TUI). The TUI is calculated as the difference in satellite sea surface temperature (SST) between the coastal and offshore zones in the areas of large-scale oceanic upwelling. The proposed technique is used to calculate the climatic variability parameters of the Eastern Boundary Upwelling Systems (EBUS’s). The seasonal variations of the TUI calculated in this approach are in better agreement with the intra-annual variability of the upward motions of the wind origin than changes in the TUI values averaged over climatic masks. The long-term TUI trends obtained by using the modified method are more significant than those calculated in climatic masks and confirm the intensification of upwelling in the last ~35 years.

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ACKNOWLEDGMENTS

We are grateful to an anonymous reviewer for their encouraging report and constructive remarks.

Funding

This study was carried out as part of State Task no. 0012-2019-0002 (“Basic Studies of the Processes in a Climatic System that Determine the Spacetime Variability of the Natural Environment of Global and Regional Scales.”)

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Correspondence to A. B. Polonsky.

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Translated by M. Shmatikov

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Polonsky, A.B., Serebrennikov, A.N. Modified Technique for Calculating the Parameters of Climatic Variability of Upwelling by Thermal Index. Izv. Atmos. Ocean. Phys. 57, 1137–1145 (2021). https://doi.org/10.1134/S0001433821090590

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  • DOI: https://doi.org/10.1134/S0001433821090590

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