Standard

Адвекция хлорофилла волнами Россби. / Белоненко, Т.В.; Колдунов, А.В.; Фукс, В.Р.

в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том 2011, № 4, 2011, стр. 106-109.

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

Harvard

Белоненко, ТВ, Колдунов, АВ & Фукс, ВР 2011, 'Адвекция хлорофилла волнами Россби', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Том. 2011, № 4, стр. 106-109.

APA

Белоненко, Т. В., Колдунов, А. В., & Фукс, В. Р. (2011). Адвекция хлорофилла волнами Россби. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2011(4), 106-109.

Vancouver

Белоненко ТВ, Колдунов АВ, Фукс ВР. Адвекция хлорофилла волнами Россби. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011;2011(4):106-109.

Author

Белоненко, Т.В. ; Колдунов, А.В. ; Фукс, В.Р. / Адвекция хлорофилла волнами Россби. в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011 ; Том 2011, № 4. стр. 106-109.

BibTeX

@article{cff901e04eb046538dc94d9a620865ec,
title = "Адвекция хлорофилла волнами Россби",
abstract = "As it was stated in many recent publications Rossby waves may be observed not only from isopleths of altimeter-measured variables (SSH and SLA) but from remotely-sensed sea surface temperatures (SST) and ocean colors bearing information of chlorophyll-a concentrations as well. This paper attempts to explain the above said phenomenon and to examine Rossby wave advection signatures in chlorophyll fields developed from satellite measurements. Theoretical explanation is given insisting that Rossby waves translocate water volumes with their special contents. Characteristics of travelling Rossby waves, detected by isopleths of the sea level altimetry are coincident with characteristics of wave disturbances in chlorophyll fields. Accordingly estimates of wave disturbances in chlorophyll concentration field can be identified with estimates of respective wave disturbances in the current velocity field or sea-level height field.",
keywords = "Advection, Altimeter measurements, Chlorophyll «a», Rossby waves, Sea level",
author = "Т.В. Белоненко and А.В. Колдунов and В.Р. Фукс",
year = "2011",
language = "русский",
volume = "2011",
pages = "106--109",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "2541-9668",
publisher = "Издательство Санкт-Петербургского университета",
number = "4",

}

RIS

TY - JOUR

T1 - Адвекция хлорофилла волнами Россби

AU - Белоненко, Т.В.

AU - Колдунов, А.В.

AU - Фукс, В.Р.

PY - 2011

Y1 - 2011

N2 - As it was stated in many recent publications Rossby waves may be observed not only from isopleths of altimeter-measured variables (SSH and SLA) but from remotely-sensed sea surface temperatures (SST) and ocean colors bearing information of chlorophyll-a concentrations as well. This paper attempts to explain the above said phenomenon and to examine Rossby wave advection signatures in chlorophyll fields developed from satellite measurements. Theoretical explanation is given insisting that Rossby waves translocate water volumes with their special contents. Characteristics of travelling Rossby waves, detected by isopleths of the sea level altimetry are coincident with characteristics of wave disturbances in chlorophyll fields. Accordingly estimates of wave disturbances in chlorophyll concentration field can be identified with estimates of respective wave disturbances in the current velocity field or sea-level height field.

AB - As it was stated in many recent publications Rossby waves may be observed not only from isopleths of altimeter-measured variables (SSH and SLA) but from remotely-sensed sea surface temperatures (SST) and ocean colors bearing information of chlorophyll-a concentrations as well. This paper attempts to explain the above said phenomenon and to examine Rossby wave advection signatures in chlorophyll fields developed from satellite measurements. Theoretical explanation is given insisting that Rossby waves translocate water volumes with their special contents. Characteristics of travelling Rossby waves, detected by isopleths of the sea level altimetry are coincident with characteristics of wave disturbances in chlorophyll fields. Accordingly estimates of wave disturbances in chlorophyll concentration field can be identified with estimates of respective wave disturbances in the current velocity field or sea-level height field.

KW - Advection

KW - Altimeter measurements

KW - Chlorophyll «a»

KW - Rossby waves

KW - Sea level

UR - http://www.scopus.com/inward/record.url?scp=84856340010&partnerID=8YFLogxK

M3 - статья

VL - 2011

SP - 106

EP - 109

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 4

ER -

ID: 5165477