Seasonal characteristics of the hydrology and circulation in the northwest Aegean Sea (eastern Mediterranean)

Observations and modeling

H. Kontoyiannis, Vassiliki H Kourafalou, V. Papadopoulos

Research output: Contribution to journalArticle

34 Citations (Scopus)

Abstract

During four seasonal surveys in 1997-1998 the shelf circulation is dominated by a semipermanent cyclone originating in the higher-salinity waters from lower Aegean latitudes. Another cyclone in the Sporades Basin has the same origin and has a semipermanent nature in the upper ∼200 m, while it is robust in all deeper layers. The variability in the upper ∼200 m depends strongly on the local river discharge and on the inflow of Black Sea Water (BSW) (evident in summer and autumn). Consequently, the shelf cyclone coexists with anticyclones in the vicinity of the river mouths (February 1998 and May 1997) or coexists with and anticyclone due to BSW (September 1997). In July 1997 the upper ∼20 m of the entire shelf is occupied by an anticyclone of BSW. The deep part of the Sporades Basin cyclone has possibly originated by deep water formation and spreading in the central north Aegean in the early 90s. In the numerical experiments the northern rivers form one plume that tends to occupy the northernmost part of the shelf due to the smaller domain scales therein. The western river (Pinios) plume expands north of the discharge site due to the abrupt shelf slope near the river mouth. Northerly winds can merge the northern and western river plumes, as in February 1998, while southerly winds can restrict the southward coastal current, thus separating northern and western river plumes, as in May 1997. A northward momentum imposed by an external Aegean flow along the east coast influences the spreading of north and west plumes.

Original languageEnglish (US)
Pages (from-to)18-11
Number of pages8
JournalJournal of Geophysical Research C: Oceans
Volume108
Issue number9
StatePublished - Sep 15 2003
Externally publishedYes

Fingerprint

hydrology
Hydrology
cyclone
rivers
river plume
anticyclone
Rivers
shelves
cyclones
plumes
anticyclones
Black Sea
seawater
sea water
Water
modeling
plume
river
mouth
Discharge (fluid mechanics)

Keywords

  • Aegean Sea
  • Black Sea water
  • Circulation
  • Mediterranean
  • River input influence on circulation
  • Thermaikos Gulf

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)
  • Atmospheric Science
  • Geochemistry and Petrology
  • Geophysics
  • Oceanography
  • Space and Planetary Science
  • Astronomy and Astrophysics

Cite this

@article{f5f60976c6fa4ef69f4b924f9bcce0d0,
title = "Seasonal characteristics of the hydrology and circulation in the northwest Aegean Sea (eastern Mediterranean): Observations and modeling",
abstract = "During four seasonal surveys in 1997-1998 the shelf circulation is dominated by a semipermanent cyclone originating in the higher-salinity waters from lower Aegean latitudes. Another cyclone in the Sporades Basin has the same origin and has a semipermanent nature in the upper ∼200 m, while it is robust in all deeper layers. The variability in the upper ∼200 m depends strongly on the local river discharge and on the inflow of Black Sea Water (BSW) (evident in summer and autumn). Consequently, the shelf cyclone coexists with anticyclones in the vicinity of the river mouths (February 1998 and May 1997) or coexists with and anticyclone due to BSW (September 1997). In July 1997 the upper ∼20 m of the entire shelf is occupied by an anticyclone of BSW. The deep part of the Sporades Basin cyclone has possibly originated by deep water formation and spreading in the central north Aegean in the early 90s. In the numerical experiments the northern rivers form one plume that tends to occupy the northernmost part of the shelf due to the smaller domain scales therein. The western river (Pinios) plume expands north of the discharge site due to the abrupt shelf slope near the river mouth. Northerly winds can merge the northern and western river plumes, as in February 1998, while southerly winds can restrict the southward coastal current, thus separating northern and western river plumes, as in May 1997. A northward momentum imposed by an external Aegean flow along the east coast influences the spreading of north and west plumes.",
keywords = "Aegean Sea, Black Sea water, Circulation, Mediterranean, River input influence on circulation, Thermaikos Gulf",
author = "H. Kontoyiannis and Kourafalou, {Vassiliki H} and V. Papadopoulos",
year = "2003",
month = "9",
day = "15",
language = "English (US)",
volume = "108",
pages = "18--11",
journal = "Journal of Geophysical Research: Oceans",
issn = "2169-9275",
publisher = "Wiley-Blackwell",
number = "9",

}

TY - JOUR

T1 - Seasonal characteristics of the hydrology and circulation in the northwest Aegean Sea (eastern Mediterranean)

T2 - Observations and modeling

AU - Kontoyiannis, H.

AU - Kourafalou, Vassiliki H

AU - Papadopoulos, V.

PY - 2003/9/15

Y1 - 2003/9/15

N2 - During four seasonal surveys in 1997-1998 the shelf circulation is dominated by a semipermanent cyclone originating in the higher-salinity waters from lower Aegean latitudes. Another cyclone in the Sporades Basin has the same origin and has a semipermanent nature in the upper ∼200 m, while it is robust in all deeper layers. The variability in the upper ∼200 m depends strongly on the local river discharge and on the inflow of Black Sea Water (BSW) (evident in summer and autumn). Consequently, the shelf cyclone coexists with anticyclones in the vicinity of the river mouths (February 1998 and May 1997) or coexists with and anticyclone due to BSW (September 1997). In July 1997 the upper ∼20 m of the entire shelf is occupied by an anticyclone of BSW. The deep part of the Sporades Basin cyclone has possibly originated by deep water formation and spreading in the central north Aegean in the early 90s. In the numerical experiments the northern rivers form one plume that tends to occupy the northernmost part of the shelf due to the smaller domain scales therein. The western river (Pinios) plume expands north of the discharge site due to the abrupt shelf slope near the river mouth. Northerly winds can merge the northern and western river plumes, as in February 1998, while southerly winds can restrict the southward coastal current, thus separating northern and western river plumes, as in May 1997. A northward momentum imposed by an external Aegean flow along the east coast influences the spreading of north and west plumes.

AB - During four seasonal surveys in 1997-1998 the shelf circulation is dominated by a semipermanent cyclone originating in the higher-salinity waters from lower Aegean latitudes. Another cyclone in the Sporades Basin has the same origin and has a semipermanent nature in the upper ∼200 m, while it is robust in all deeper layers. The variability in the upper ∼200 m depends strongly on the local river discharge and on the inflow of Black Sea Water (BSW) (evident in summer and autumn). Consequently, the shelf cyclone coexists with anticyclones in the vicinity of the river mouths (February 1998 and May 1997) or coexists with and anticyclone due to BSW (September 1997). In July 1997 the upper ∼20 m of the entire shelf is occupied by an anticyclone of BSW. The deep part of the Sporades Basin cyclone has possibly originated by deep water formation and spreading in the central north Aegean in the early 90s. In the numerical experiments the northern rivers form one plume that tends to occupy the northernmost part of the shelf due to the smaller domain scales therein. The western river (Pinios) plume expands north of the discharge site due to the abrupt shelf slope near the river mouth. Northerly winds can merge the northern and western river plumes, as in February 1998, while southerly winds can restrict the southward coastal current, thus separating northern and western river plumes, as in May 1997. A northward momentum imposed by an external Aegean flow along the east coast influences the spreading of north and west plumes.

KW - Aegean Sea

KW - Black Sea water

KW - Circulation

KW - Mediterranean

KW - River input influence on circulation

KW - Thermaikos Gulf

UR - http://www.scopus.com/inward/record.url?scp=0348165957&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0348165957&partnerID=8YFLogxK

M3 - Article

VL - 108

SP - 18

EP - 11

JO - Journal of Geophysical Research: Oceans

JF - Journal of Geophysical Research: Oceans

SN - 2169-9275

IS - 9

ER -