Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Stochastic Modeling of Sea Ice Concentration to Assess Navigation Conditions along the Northern Sea Route. / Май, Руслан Игоревич; ГУЗЕНКО , РОМАН БОРИСОВИЧ; Tarovik, Oleg V.; Топаж, А. Г.; Юлин, А.В.
в: Izvestiya - Atmospheric and Oceanic Physics, Том 59, № 1, 01.10.2023, стр. S57-S69.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Stochastic Modeling of Sea Ice Concentration to Assess Navigation Conditions along the Northern Sea Route
AU - Май, Руслан Игоревич
AU - ГУЗЕНКО , РОМАН БОРИСОВИЧ
AU - Tarovik, Oleg V.
AU - Топаж, А. Г.
AU - Юлин, А.В.
PY - 2023/10/1
Y1 - 2023/10/1
N2 - Abstract: This article describes a probabilistic model (stochastic generator) of spatiotemporal variability of sea ice concentration. The values of the concentration are generated at the nodes of the spatial grid with 10‑km resolution; the model time step is 1 day. The change in ice concentration with time (temporal variability) is modeled on the basis of a matrix of transient probabilities (discrete Markov chain), each row of which is a distribution function of the conditional probability of changes in the concentration. Spatial variability is determined by empirical probability fields, with which the observed changes in fields of concentration are associated with known conditional probability distribution functions. To identify the parameters of the stochastic generator, satellite data from the OSI SAF project for 1987–2019 were used. The generator takes into account seasonal, interannual, and climatic variability. Interannual and climatic variability are determined on the basis of a stochastic model of changes in the types of ice coverage. In order to verify the developed stochastic generator, we compare the statistical indicators of observed and calculated ice fields. The results show that the field-average absolute error of statistical characteristics of the ice concentration (average and standard deviation) does not exceed 3.3%. The discrepancy between the correlation intervals of ice coverage calculated from the model and measured ice concentration fields does not exceed 2 days. The variograms of the modeled and observed fields have a similar form and close values. As an example, we determine the duration of navigation of Arc4 ice class ships between the Barents and Kara seas using synthetic fields of the concentration reproduced by the stochastic generator.
AB - Abstract: This article describes a probabilistic model (stochastic generator) of spatiotemporal variability of sea ice concentration. The values of the concentration are generated at the nodes of the spatial grid with 10‑km resolution; the model time step is 1 day. The change in ice concentration with time (temporal variability) is modeled on the basis of a matrix of transient probabilities (discrete Markov chain), each row of which is a distribution function of the conditional probability of changes in the concentration. Spatial variability is determined by empirical probability fields, with which the observed changes in fields of concentration are associated with known conditional probability distribution functions. To identify the parameters of the stochastic generator, satellite data from the OSI SAF project for 1987–2019 were used. The generator takes into account seasonal, interannual, and climatic variability. Interannual and climatic variability are determined on the basis of a stochastic model of changes in the types of ice coverage. In order to verify the developed stochastic generator, we compare the statistical indicators of observed and calculated ice fields. The results show that the field-average absolute error of statistical characteristics of the ice concentration (average and standard deviation) does not exceed 3.3%. The discrepancy between the correlation intervals of ice coverage calculated from the model and measured ice concentration fields does not exceed 2 days. The variograms of the modeled and observed fields have a similar form and close values. As an example, we determine the duration of navigation of Arc4 ice class ships between the Barents and Kara seas using synthetic fields of the concentration reproduced by the stochastic generator.
KW - Arctic navigation
KW - Markov chain
KW - ice concentration
KW - ice conditions
KW - sea ice generator
KW - stochastic modeling
UR - https://www.mendeley.com/catalogue/e5c17174-0994-3b46-b4d7-27f412ea98bd/
U2 - 10.1134/s0001433823130091
DO - 10.1134/s0001433823130091
M3 - статья
VL - 59
SP - S57-S69
JO - Izvestiya - Atmospheric and Oceanic Physics
JF - Izvestiya - Atmospheric and Oceanic Physics
SN - 0001-4338
IS - 1
ER -
ID: 113574360