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Iquique - CRC 1211
The Atacama desert (Chile) is one of the driest regions on earth with places receiving no precipation for years. It is considered to be one of the oldest deserts on earth. The collaborative research center SFB1211 'Earth Evolution at the Dry Limit' aims to investigate different aspects of landscape, and life evolution under this extreme conditions. The site in Iquique is funded within subproject A1 'Modern and past climate: Investigation of atmospheric water supply to the Atacama desert (Chile) from combined in-situ, ground-based and satellite remote sensing observations'. It consist of three state of the art remote sensing instruments
The Atacama is formed by a plateau at about 1000m above sea level between the pacific to the west and the Andes mountains to the east. This plateau drops at most places towards the pacific ocean in a cliff to the shoreline. As the plateau lies at about the same height as the stratus cloud deck of the eastern Pacific these clouds form as fog the main source of water along this cliff, and at certain pathways into the Atacama. With the instruments at the site it will be tried to characterize the clouds at the coast for one year. They will provide cloud base and top height, liquid water content, vertical and horizontal wind, temperature and humidity. Based on this data it will be possible to provide information on the occurence of fog in the past and under future climate conditions.
The site is located in the North of Chile between the Pazific Ocean and the Atacama desert on the grounds of Iquique airport.
- Latitude: 20.5394440 S = 20°32'22“ S
- Longitude: 70.1772694 W = 70°10'38” W
- Altitutde: 56m AMSL
Left: view over the site to the NE prior to installation with coastal cliff in the background. Right: The site with (from left to rigth) cloud radar Joyrad94 , windlidar Halo Streamline (provided by FMI), Microwave radiometer FOGHAT.
- Halo Doppler Windlidar . The instrument is provided by the finish meteorological institute (FMI, thanks to Heikki Lihavainen and Anne Hirsikko), but at JOYCE is running a similar instrument.
|wind lidar||Micorwave radiometer||Cloud radar|
|Horizontal wind (arrows) and aerosol backscatter (color)||Reflectivity, doppler speed and ohter parameters from Cloudradar JOYRAD94|
(click on plots to see more)