A Phys ica l and Chemica l Descr ip t ion of the Med i te r ranean
Out f low in the Gu l f o f Cad iz
UDC 551.465.45:551.465.42; Northeast Atlantic, 5Iarsden Square 109
I. Ambar , M. R. Howe and M. I. Abdu l lah
Summary The Mediterranean outflow is considered as two separate cores (upper and
lower) which follow a well defined route between Gibraltar and Cabo SBo Vincente. Their physical and chemical properties are discussed in some detail and used as evidence for treating the upper core as a separate water mass. This core is also shown to suffer a 20 % depletion in ,its concentration as it traverses the Gulf of Cadiz, whereas that of the lower core remains almost constant. In addition there was some indication of winter cooling and sinking of the shelf water which seems to be enhanced by the presence of the more prominent canyons in the area.
Eine physikalische und ehemische Beschreibung des Mittelmeer-Ausstroms in den Golf yon Cadiz (Zusammenfassung)
Das Ausstr6men des Mittelmeerwassers geschieht in zwei getrennten (oberen und unteren) Kernmassen, die sich entlang einer deutlich abgegrenzten Route zwischen Gibraltar und Cabo Sgo Vicente ausbreiten. Ihre physikalischen und chemischen Eigenschaften werden ausfiihrlich beschrieben und als Beweis dafiir benutzt, dab man den oberen Kern als getrennte Wassermasse behandeln kann. Es wird auch gezeigt, dab dieser Kern beim Durchzug durch den Golf yon Cadiz in seiner Kon- zentration um 20 % abgeschw~icht wird, wohingegen die untere Kernkonzentration fast konstaut bleibt. AuBerdem gibt es Anzeichen fiir ein Abkiihlen und Absinken des Schelfwassers im Winter, welches durch das Vorhandensein yon Cations in diesem Gebiet verst~rkt zu werden scheint.
Une description physique et chimique du courant d'gcoulement m6diterran6en dans le Golfe de Cadix (R~sum~)
Le courant d'6coulement m@diterran~en est consid@r5 comme comportant deux couches distinctes (la sup6rieure et l'inf@Heure), qui suivent une route bien d@finie entre Gibraltar et le Cap Saint-Vincent. Leurs propri6t@s physiques et chimiques font l'objet d'une discussion d4taill@e et sont utilisSes comme t@moins permettant de traiter la couche sup4rieure comme une masse d'eau s@ar@e. On montre 5galement que cette couche subit une d@perdition de concentration de 20 % lors de la travers6e du Golfe de Cadix, alors que celle de la couche inf@rieure reste presque constante. :De plus, il a 6t6 constat@ un certain refroidissement hivernal et un enfoncement de l'eau du plateau continental, qui semble renforc@ par la presence des canyons les plus importants de la rSgion.
I t is now accepted that the outflow of the Mediterranean water from the Straits of Gibraltar can be influenced by several different processes. The seasonal changes that occur have been acknowledged for some time (S chot t ), and recently shorter period fluctua-
Ambar et al., Med i te r ranean Out f low in the Gu l f of Cadiz 59
tions in the flow have been attributed to the variations in atmospheric pressure between the regions to the East and West of the Straits (Lacombe ; Crepon ). There are strong tidal currents superimposed on the flow and Defant  has discussed the likely internal tidal oscillations in the Straits and their effect on the boundary between the inflowing Atlantic water at the surface and the deeper Mediterranean outflow, whereas Boyce  has made a similar study of internal waves. Furthermore, the outflow to the West of Gibraltar may also be influenced by the bottom topography and this has been considered in some detail by Madela in . Finally an explanation is required for the fact that a core of Mediter- ranean water can be observed in the Atlantic at depths other than the traditional 1200 m !~rel. Several publications have noted the existence of a prominent T-S maximum between 5~0 to 800 m which Howe, Abdu l lah and Deetae  have described in terms of its chemical and physical properties. They suggested that this water originates from a relatively shallow depth within the Straits.
There are therefore several processes which can influence the intensity and characteristics of the outflow as well as its most likely route, and their relative importance has yet tO be determined. The use of TSD systems in this area have provided observations which indicate a complex situation in which water masses are being generated under different circumstances and then mix at different depths to produce considerable variability in the properties in both the horizontal and vertical directions. The t~.t~.S. "Shaeldeton" cruise (2/73) included a study of the region between Cabo Sgo Vieente.and Gibraltar in March 1973, and this provided physical and chemical data which adequately demonstrated the degree of inhomogeneity in the water column. The four sections (Fig. 1) were completed within 5 days although most of the
/~e - - depth contours in fathoms
Qo77 . % / \ \ \ st2,t \ , , 10C~ < ~ ' ~ , ~, ~ ~, Gibraltar 9~ S ~ 7 ~
Fig'. 1. Station positions ill sections IV to VII. 9 TSD station. 9 TSD and chemical sampling
stations (59 to 91) were made within a period of 66 h. The remainder (92 to 100) were delayed due to a storm. The stations were purposely located along the prominent canyons in the area with the intention of observing any unusual effects which might be caused by these topo- graphical features. We shall describe the hydrography of the region at this time of the year ::a terms of the evidence presented in these sections and thereby attempt to explain the events which might occur as the outflow leaves the Straits and moves around the Gulf of Cadiz towards Cabo Sgo Vieente. A TSD system was used and this was supplemented by water samples from standard depths at certain stations (Fig. 1), from which the nutrient salts (nitrate, silicate and phosphate) were determined. The chemical methods of analysis have already been fully described (Howe, Abdu l lah and Deetae ).
60 Deutsche Hydrographische Zeitschrift, Jahrgang 29, 1976, Hef t 2
2. Temperature, salinity and nutrient profiles
An inspection of the T, S and nutrient distributions (Figs. 2, 3, 4, 5) will show that the normal Atlantic water column, which is best represented in this area by the offshore stations in each section, can be severely disturbed by the intrusion of the Mediterranean outflow. This main ly occurs near the continental slope between depths of 450 m and 1300 m.
s to t ion number 69 68 67 66 65 62~ 63 62 61 60 59
Ambar et al., Mediterranean Outflow in the Gulf of Cadiz 61
The unaffected surface layers between 50 to 400 m show, in general, a regular decrease of T and S with depth, from 15 ~ to 12 ~ and 36.2 ~ o to 35.7 ~ o respectively. This is accompanied by an increase in the values of the nutrient salts (Figs. 2b, 3b, 5b). However,
~ 1000 1200
s tat ion number ) 71 72 7,3 74 75 76 70 71 72 7? 74 75 76
!I\\ T .. k~--" ~ 1 1 . o - ~
Fig. 3a. Section V. Distribution of salinity and temperature
at several inshore stations these layers have also been disturbed, but in this case by an apparent surface sinking process. This is particularly evident in sections V and VII where it seems probable that the effect of winter cooling on the shelf has been encouraged by the presence of a prominent submarine canyon to produce a tongue of downwelled surface water to depths of 400 m or 500 m. Below 400 m the intrusion of the Mediterranean water (MW) can be observed by the relatively high salinities and temperatures and also the correspondingly low
station number 70 71 72 73 74 75
, , f f ,
Fig. 3b. Section V. Distribution of silicate, nitrate an,
s tat ion number 70 71 72 73 74 75
, , , i i 3
, l o
s tat ion number 70 71 72 73 74 75
I I t r ,
~176 1 ~ ~
nutrient values. This correlation between the distortion of the nutrient profiles in the Atlantic and the high salinities has already been analysed in some detail (Howe, Abdu l lah and Deetae ). The fact that MW of ]ow nutrient content intrudes into the Atlantic water column at depths where the nutrient values are normally much greater, has provided an additional means of identifying its presence. In sections VI and VII (Figs. 4, 5) nearest the
62 Deutsche :[-Iydrographische Zeitschrift, Jahrgang 29, 1976, Hef t 2
station number 88 87 86 8> 8,4 e? 87 8! 80 79 7,8 7,7
171 ~ ~35.8~
4 0 0 " ~ B S Y ~ -
5.6 ~ . . . .
a: : . - ' : :5 ' - -
12oo- Section ~ " ' "~k / 1~%~
8- 2 0 0 q ~ 1 4 o ~ __
I m ~ ~ X _ - - - l ~ . O ~ ~ 1 2 . 5 ~ 400 1 2 0 ~
.......... ~ ~za2 'e .s~ 8oo- "~ ~'%-Y._-~.~-~--:~.5 ~ ~-~1~0~
,ooo8~176 ' . . . . . - " Temperature ~ " : ~ .
1400. %"::: v4 :'~:~ ::: *"
Fig. 4. Section VI. Distribution of salinity and temperature
Straits, there is a continuous layer of MW on the slope extending from about 450 m to 1300 m whereas, in sections IV and V (Figs. 2, 3), the MW has separated into discrete upper and lower cores. Although the salinities are comparable, in all the sections the temperature in the MW above 900 m is consistently about 1 ~ greater than in that below 900 m. There is some indica- t ion of an offshore spreading of both cores in sectio