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    Water composition has some similarity to seawater, which is due to atmospheric deposition being dominated by marine aerosol and the high salinity to intense concentration by evapotranspiration (evapoconcentration) of precipitation.Soluble salts deposited in the soil are dissolved and transferred to aquifer recharge when some of rare significant precipitations occur.Temperatures at the coast are mild and stable most of the year due to the smoothing effect of the sea.Monthly mean values range between 13.5°C and 20.1°C in the city of Antofagasta (DGA, 1987).Sometimes this fog produces local small drizzle and horizontal rain when droplets are intercepted by vegetation, especially when the system is altered by the spread towards the north of cold fronts coming from the south (Ogaz and Fuenzalida, 1981; Houston, 2006).In the most favorable areas for fog condensation, further south of the area here considered, the total distributed contribution does not exceed 10 mm/yr (Román, 1999).It is one of the driest regions of the world, containing areas whose average annual precipitation in many cases is less than 1 mm, which means long periods of extreme aridity and occasional rainfall events widely separated in time.

    It consists on thin, small clouds trapped against the Cordillera de la Costa at the coastal side.

    On the other hand, the Andes range is an impressive mountain barrier preventing the arrival of moisture coming from the Atlantic Ocean through the Amazon Basin.

    Some of this moisture reaches the western slope of the Andes in the summer months, in the so-called 'Invierno Altiplánico' (highlands winter), but not the Central Depression.

    Chemical and water isotope data (H) show that the rainfall events that produced part of the recharge could correspond to wetter conditions than at present.

    Their origin could be related to the emplacement of warm sea currents facing the coast of northern Chile, possibly associated to incursions of El Niño Southern Oscillation (ENSO).

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