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On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation. / Zakharchuk, E. A.; Tikhonova, N. A.

в: Russian Meteorology and Hydrology, Том 36, № 8, 08.2011, стр. 534-541.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Zakharchuk, EA & Tikhonova, NA 2011, 'On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation', Russian Meteorology and Hydrology, Том. 36, № 8, стр. 534-541. https://doi.org/10.3103/S106837391108005X

APA

Zakharchuk, E. A., & Tikhonova, N. A. (2011). On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation. Russian Meteorology and Hydrology, 36(8), 534-541. https://doi.org/10.3103/S106837391108005X

Vancouver

Zakharchuk EA, Tikhonova NA. On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation. Russian Meteorology and Hydrology. 2011 Авг.;36(8):534-541. https://doi.org/10.3103/S106837391108005X

Author

Zakharchuk, E. A. ; Tikhonova, N. A. / On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation. в: Russian Meteorology and Hydrology. 2011 ; Том 36, № 8. стр. 534-541.

BibTeX

@article{c335132678bb458ba8d2af44ea453926,
title = "On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation",
abstract = "A comparative contribution of the sea level oscillations of various time scales (long-term, seasonal, synoptic, and mesoscale) to the formation of the Neva River floods is estimated. The identification of the Neva River flood waves as the long gravity ones existing nowadays is called in question. The comparison of estimated characteristics of flood waves with the theoretical variance relations of different types of long waves is carried out. This comparison as well as the results of analysis of meteorological information and numerical experiments carried out before on the basis of the hydrodynamic model of the Baltic Sea demonstrate that the Neva River flood waves are identified as the forced baroclinic topographic waves generated as a result of the resonance between the anemobaric forces in atmospheric cyclones and low-frequency eigenmodes of the open Baltic Sea-Gulf of Finland system.",
author = "Zakharchuk, {E. A.} and Tikhonova, {N. A.}",
year = "2011",
month = aug,
doi = "10.3103/S106837391108005X",
language = "Английский",
volume = "36",
pages = "534--541",
journal = "Russian Meteorology and Hydrology",
issn = "1068-3739",
publisher = "Allerton Press, Inc.",
number = "8",

}

RIS

TY - JOUR

T1 - On the Spatiotemporal Structure and Mechanisms of the Neva River Flood Formation

AU - Zakharchuk, E. A.

AU - Tikhonova, N. A.

PY - 2011/8

Y1 - 2011/8

N2 - A comparative contribution of the sea level oscillations of various time scales (long-term, seasonal, synoptic, and mesoscale) to the formation of the Neva River floods is estimated. The identification of the Neva River flood waves as the long gravity ones existing nowadays is called in question. The comparison of estimated characteristics of flood waves with the theoretical variance relations of different types of long waves is carried out. This comparison as well as the results of analysis of meteorological information and numerical experiments carried out before on the basis of the hydrodynamic model of the Baltic Sea demonstrate that the Neva River flood waves are identified as the forced baroclinic topographic waves generated as a result of the resonance between the anemobaric forces in atmospheric cyclones and low-frequency eigenmodes of the open Baltic Sea-Gulf of Finland system.

AB - A comparative contribution of the sea level oscillations of various time scales (long-term, seasonal, synoptic, and mesoscale) to the formation of the Neva River floods is estimated. The identification of the Neva River flood waves as the long gravity ones existing nowadays is called in question. The comparison of estimated characteristics of flood waves with the theoretical variance relations of different types of long waves is carried out. This comparison as well as the results of analysis of meteorological information and numerical experiments carried out before on the basis of the hydrodynamic model of the Baltic Sea demonstrate that the Neva River flood waves are identified as the forced baroclinic topographic waves generated as a result of the resonance between the anemobaric forces in atmospheric cyclones and low-frequency eigenmodes of the open Baltic Sea-Gulf of Finland system.

U2 - 10.3103/S106837391108005X

DO - 10.3103/S106837391108005X

M3 - статья

VL - 36

SP - 534

EP - 541

JO - Russian Meteorology and Hydrology

JF - Russian Meteorology and Hydrology

SN - 1068-3739

IS - 8

ER -

ID: 5504683