Research output: Contribution to journal › Article › peer-review
The intensity of variations of the Kara Sea Level on different time scales. / Zakharchuk, E. A.
In: Russian Meteorology and Hydrology, No. 7, 2001, p. 47-58.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - The intensity of variations of the Kara Sea Level on different time scales
AU - Zakharchuk, E. A.
N1 - Copyright: Copyright 2005 Elsevier Science B.V., Amsterdam. All rights reserved.
PY - 2001
Y1 - 2001
N2 - Based on direct observations of the Kara Sea level from 20 coastal points, the mean contributions of processes on different time scales (nontidal mesoscale oscillations, semidiurnal and diurnal tides, synoptic-scale oscillations, long-term tides, seasonal and long-term variations) to the total variance of sea level variations are estimated and maximum nontidal oscillations on different time scales are determined. It was found that synoptic-scale sea level variations prevailed at most points of the Kara Sea. Their mean contribution to the total variance ranges from 26 to 71%. Maximum variations reach 88 cm in the north of the sea, increasing up to 300 cm in Yenisei Bay. The most intensive synoptic-scale sea level variations are generated at intervals from 52 to 122 days and from 7 to 16 days.
AB - Based on direct observations of the Kara Sea level from 20 coastal points, the mean contributions of processes on different time scales (nontidal mesoscale oscillations, semidiurnal and diurnal tides, synoptic-scale oscillations, long-term tides, seasonal and long-term variations) to the total variance of sea level variations are estimated and maximum nontidal oscillations on different time scales are determined. It was found that synoptic-scale sea level variations prevailed at most points of the Kara Sea. Their mean contribution to the total variance ranges from 26 to 71%. Maximum variations reach 88 cm in the north of the sea, increasing up to 300 cm in Yenisei Bay. The most intensive synoptic-scale sea level variations are generated at intervals from 52 to 122 days and from 7 to 16 days.
UR - http://www.scopus.com/inward/record.url?scp=0035570740&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0035570740
SP - 47
EP - 58
JO - Russian Meteorology and Hydrology
JF - Russian Meteorology and Hydrology
SN - 1068-3739
IS - 7
ER -
ID: 76723677