Programming ::
The Center for Deep Sea Marine Biology and Marine Seismology
The Center for Deep Sea Marine Biology and Marine Seismology
Beginning with the Site :: Venice Beach, CA [the old pier]
Begin breakdown of Programmatic Requirements
Preliminary organizational diagram
Break down of Square footages
Hard Numbers sqare footage allotments
Preliminary spatial organization :: Height of 24 stories is decided upon
Begin with a grid for organizational clarity [to be furhter expanded upon later in building development.]
Begin with equal amounts of space in "plan" - square footages will be adjusted further in section
Six organizational "plans" are developed - only six "plans" to be repeated throughout the tower
From the outer edges of the tower, the "open space" program allotments begin to be pulled out to reveal voids which will eventually act as outdoor spaces, courtyards, atriums and observation decks.
Remaining "open space" allotments act as infrastructure i.e. vertical circulation, horizontal circulation within floors, fire access, and mechanical areas. [will be further distributed when building form begins to be more thoroughly developed.]
Highlighted portions are remaining "open space" :: Tower Infrastructure
Infrastructure Maintains a mainly central core, but does have some horizontal variation at certain points in the building where necessary.
Entertainment/Education spaces as they relate to the central core. Where spaces are "stacked," second floor area dissolves and becomes a double height space.
Research spaces as they relate to the central core. Where spaces are "stacked," second floor area dissolves and becomes a double height space.
Exchange spaces [also includes any additional residences for guests, faculty, staff, and visitors.
In thermohaline circulation, differences in the temperature and density of ocean water masses cause the nutrient-rich deep ocean waters to rise and mix with surface waters.
The density of ocean water is not globally homogeneous, but varies significantly and discretely. Sharply defined boundaries exist between water masses which form at the surface, and subsequently maintain their own identity within the ocean. They position themselves one above or below each other according to their density, which depends on both temperature and salinity




















From the formal variation, variation between individual towers and their interconnection are also stressed.

















