Transactions of KarRC RAS :: Scientific publications
Transactions of KarRC RAS :: Scientific publications

Transactions of KarRC RAS :: Scientific publications
Karelian Research Centre of RAS
ISSN (print): 1997-3217
ISSN (online): 2312-4504
Transactions of KarRC RAS :: Scientific publications
Background Editorial committee Editorial Office For authors For reviewer Russian version
Transactions of KarRC RAS :: Scientific publications

Electronic Journal OJS



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Biogeography

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Precambrian Geology

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1999-2008


SCIENTIFIC PUBLICATIONS
Гузиватый В.В., Науменко М.А.
Применение метода максимальной кросс-корреляции для оценки течений на поверхности крупных внутренних акваторий
Guzivaty V.V., Naumenko M.A. Application of the maximum crosscorrelation method for estimation of surface currents of large inland water areas // Transactions of Karelian Research Centre of Russian Academy of Science. No 2. Limnology and oceanology. 2024. P. 65–78
Keywords: currents on the surface of seas and large lakes; MCC method; Lake Ladoga; Lake Onego; White Sea; Baltic Sea; Black and Caspian Seas
The maximum cross-correlation (MCC) method was first used for Lake Ladoga in 2016. The method enables the assessment of water dynamics at meso- and synoptic scales on the surface of seas and large lakes using sequential satellite infrared images with a spatial resolution of 1×1 km. The article discusses methodological aspects of application and limitations of the MCC method for large water areas. The procedures of selecting the most favorable meteorological conditions and space data analysis proposed for Lake Ladoga have shown their effectiveness when applying the MCC method for areas from 9.7 to 422 thous. km2. The maximum cross-correlation method was used to estimate surface currents for large inland water areas of the European part of the Russian Federation, including Lake Ladoga, Lake Onego, the White, Baltic, Black and Caspian Seas for specific wind situations during the open water period. The period in the seasonal aspect, for which the MCC method for these water areas is the most effective, is revealed, and its prospects in the absence of in situ measurements of currents are shown.
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  Last modified: April 3, 2024