2011
DOI: 10.5697/oc.53-1.081
|View full text |Cite
|
Sign up to set email alerts
|

Changes in Atlantic Water characteristics in the south-eastern Mediterranean Sea as a result of natural and anthropogenic activities

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
9
0

Year Published

2015
2015
2021
2021

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 10 publications
(9 citation statements)
references
References 11 publications
0
9
0
Order By: Relevance
“…It is connected to Atlantic Ocean through the narrow Gibraltar Strait, Kamel and Maiyza (2000). This Atlantic Water occupying the upper 200 m layer is likely to flow into Mediterranean Sea with its general salinity $36.0-36.5, Millot (2007) and Said et al (2011).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…It is connected to Atlantic Ocean through the narrow Gibraltar Strait, Kamel and Maiyza (2000). This Atlantic Water occupying the upper 200 m layer is likely to flow into Mediterranean Sea with its general salinity $36.0-36.5, Millot (2007) and Said et al (2011).…”
Section: Discussionmentioning
confidence: 99%
“…4, surface and 200 m depth. A higher surface water temperature was observed at longitudes 26°and latitude 30°E (16.6-18.5°C) with a general tendency to increase eastwards with lowest values (16.6-16.8°C) during the period 1959-2008, Said et al (2011). During winter 1971, the temperature varied between 15 and 18°C with maximum 17.8-18.0°C at stations located on the cross sections from Damitta to the Bay of El Salum, Al Kholy and El Wakeel (1975).…”
Section: Seawater Temperature and Salinitymentioning
confidence: 93%
“…Where T is the annual mean water temperature of the Egyptian Mediterranean water and was sit as 21. 3 C º [41].…”
Section: Population Parameters and Managementmentioning
confidence: 99%
“…The water mass formation cycle is characterized by the inflow of low-salinity Atlantic Water (AW) in the upper 100 m of the water column and with identification values of S = 36.0-36.5 psu in the Strait of Gibraltar (Said et al, 2011), and a return flow of the salty Levantine Intermediate Water (LIW), formed in the Levantine Basin and positioned in the intermediate layer (typically at a depth of 200-600 m). The depth variability of the LIW salinity maximum is largely regional; generally, depths increase westward.…”
Section: Introductionmentioning
confidence: 99%