Variability of frontal zones and short-period internal waves in the Barents and Kara Seas from satellite observations during the warm period of 2007

E. I. Svergun, A. V. Zimin, O. A. Atadzhanova, A. A. Konik, E. V. Zubkova, I. E. Kozlov

Research output

Abstract

In this work we analyze the influence of frontal zone dynamics on the generation and distribution of short-period internal waves (SIWs) in the Barents and the Kara Seas during an ice-free season based on analysis of satellite data. In the Barents Sea, marginal ice frontal zone and polar front zone are considered. They occupy up to 8 % of the total sea area. As shown, only 5 % of the total number of internal wave manifestations were recorded inside these frontal zones. In July, their number reaches 18 % in the marginal ice frontal zone. In the Kara Sea, estuarine and marginal ice frontal zones are considered, covering areas up to 10 % of the entire sea. On average, 18 % of the total number of SIW manifestations were observed inside frontal zone regions of the Kara Sea. The maximum number of internal waves (33 %) is observed in August in the most dynamic estuarine frontal zone, associated with the Ob and the Yenisei river runoff. Factors that determine the features of the space-time distribution of shortperiod internal waves in the regions of pronounced frontal dynamics are discussed.

Original languageEnglish
Pages (from-to)181-188
Number of pages8
JournalSovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa
Volume15
Issue number4
DOIs
Publication statusPublished - 1 Jan 2018

Fingerprint

internal wave
Satellites
Ice
ice
Sea ice
Runoff
estuarine dynamics
Rivers
marginal sea
polar front
sea
observation satellite
satellite data
runoff
river

Scopus subject areas

  • Computer Science Applications
  • Computers in Earth Sciences
  • Computer Networks and Communications

Cite this

@article{d0c6a4c486774937848f13ffd3843856,
title = "Variability of frontal zones and short-period internal waves in the Barents and Kara Seas from satellite observations during the warm period of 2007",
abstract = "In this work we analyze the influence of frontal zone dynamics on the generation and distribution of short-period internal waves (SIWs) in the Barents and the Kara Seas during an ice-free season based on analysis of satellite data. In the Barents Sea, marginal ice frontal zone and polar front zone are considered. They occupy up to 8 {\%} of the total sea area. As shown, only 5 {\%} of the total number of internal wave manifestations were recorded inside these frontal zones. In July, their number reaches 18 {\%} in the marginal ice frontal zone. In the Kara Sea, estuarine and marginal ice frontal zones are considered, covering areas up to 10 {\%} of the entire sea. On average, 18 {\%} of the total number of SIW manifestations were observed inside frontal zone regions of the Kara Sea. The maximum number of internal waves (33 {\%}) is observed in August in the most dynamic estuarine frontal zone, associated with the Ob and the Yenisei river runoff. Factors that determine the features of the space-time distribution of shortperiod internal waves in the regions of pronounced frontal dynamics are discussed.",
keywords = "Frontal zones, Internal waves, Satellite observations, The Barents Sea, The Kara Sea",
author = "Svergun, {E. I.} and Zimin, {A. V.} and Atadzhanova, {O. A.} and Konik, {A. A.} and Zubkova, {E. V.} and Kozlov, {I. E.}",
year = "2018",
month = "1",
day = "1",
doi = "10.21046/2070-7401-2018-15-4-181-188",
language = "English",
volume = "15",
pages = "181--188",
journal = "СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА",
issn = "2070-7401",
publisher = "ИКИ РАН",
number = "4",

}

TY - JOUR

T1 - Variability of frontal zones and short-period internal waves in the Barents and Kara Seas from satellite observations during the warm period of 2007

AU - Svergun, E. I.

AU - Zimin, A. V.

AU - Atadzhanova, O. A.

AU - Konik, A. A.

AU - Zubkova, E. V.

AU - Kozlov, I. E.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - In this work we analyze the influence of frontal zone dynamics on the generation and distribution of short-period internal waves (SIWs) in the Barents and the Kara Seas during an ice-free season based on analysis of satellite data. In the Barents Sea, marginal ice frontal zone and polar front zone are considered. They occupy up to 8 % of the total sea area. As shown, only 5 % of the total number of internal wave manifestations were recorded inside these frontal zones. In July, their number reaches 18 % in the marginal ice frontal zone. In the Kara Sea, estuarine and marginal ice frontal zones are considered, covering areas up to 10 % of the entire sea. On average, 18 % of the total number of SIW manifestations were observed inside frontal zone regions of the Kara Sea. The maximum number of internal waves (33 %) is observed in August in the most dynamic estuarine frontal zone, associated with the Ob and the Yenisei river runoff. Factors that determine the features of the space-time distribution of shortperiod internal waves in the regions of pronounced frontal dynamics are discussed.

AB - In this work we analyze the influence of frontal zone dynamics on the generation and distribution of short-period internal waves (SIWs) in the Barents and the Kara Seas during an ice-free season based on analysis of satellite data. In the Barents Sea, marginal ice frontal zone and polar front zone are considered. They occupy up to 8 % of the total sea area. As shown, only 5 % of the total number of internal wave manifestations were recorded inside these frontal zones. In July, their number reaches 18 % in the marginal ice frontal zone. In the Kara Sea, estuarine and marginal ice frontal zones are considered, covering areas up to 10 % of the entire sea. On average, 18 % of the total number of SIW manifestations were observed inside frontal zone regions of the Kara Sea. The maximum number of internal waves (33 %) is observed in August in the most dynamic estuarine frontal zone, associated with the Ob and the Yenisei river runoff. Factors that determine the features of the space-time distribution of shortperiod internal waves in the regions of pronounced frontal dynamics are discussed.

KW - Frontal zones

KW - Internal waves

KW - Satellite observations

KW - The Barents Sea

KW - The Kara Sea

UR - http://www.scopus.com/inward/record.url?scp=85053271840&partnerID=8YFLogxK

U2 - 10.21046/2070-7401-2018-15-4-181-188

DO - 10.21046/2070-7401-2018-15-4-181-188

M3 - Review article

AN - SCOPUS:85053271840

VL - 15

SP - 181

EP - 188

JO - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА

JF - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА

SN - 2070-7401

IS - 4

ER -