David Bowen

tele-present water
This installation draws information from the intensity and movement of the water in a remote location. Wave data is being collected and updated from National Oceanic and Atmospheric Administration data buoy station 51003. This station was originally moored 205 nautical miles Southwest of Honolulu on the Pacific. It went adrift and the last report from its moored position was around 04/25/2011.  It is still transmitting valid observation data but its exact location is unknown. The wave intensity and frequency collected from the buoy is scaled and transferred to the mechanical grid structure, resulting in a simulation of the physical effects caused by the movement of water from this distant unknown location. This work physically replicates a remote experience and makes observation of the activity of an isolated object, otherwise lost at sea, possible through direct communication.

WRO2011 NATIONAL MUSEUM- WROCLAW, POLAND - 2011

This installation draws information from the intensity and movement of the water in a remote location. Wave data is being collected in real-time from National Oceanic and Atmospheric Administration data buoy station 46246, 49.985 N 145.089 W (49°59'7" N 145°5'20" W) on the Pacific Ocean. The wave intensity and frequency is scaled and transferred to the mechanical grid structure resulting in a simulation of the physical effects caused by the movement of water from halfway around the world.

lake superior data version - 2011

This installation uses information from the intensity and movement of the water in a remote location. Wave g-force and acceleration data was collected during a voyage on Lake Superior. The wave data is scaled and transferred to the mechanical grid structure resulting in a simulation of the physical effects caused by the movement of water.