A process and the required apparatus for 
air conditioning the interior of a structure located within a harsh desert like exterior environment. The 
air conditioning system is particularly effective at times when the exterior temperature is in excess of approximately 90 to 95 degrees Fahrenheit, and the exterior 
relative humidity is less than approximately 35 to 40 percent. A tube and shell 
heat exchanger wherein the shell side is wet and the tube side is dry is employed to air condition the interior of the structure. In the operation of the air conditioner, a 
mass of distributed water, for example, a spray, is established on the wet shell side, and a flow of 
ambient air is passed through the wet shell side to form a resulting 
stream of moist air. A flow of 
ambient air is passed through the dry tube side and a resulting 
stream of dry cooled air is recovered. The streams of moist and cooled air are combined and the resulting 
stream of combined air is discharged into the exterior of the structure. The structure is not hermetically sealed so there is little or no 
pressure difference between the interior of the structure and the surrounding environment. The 
system requires so little power that it can be operated on a 
battery system charged from an 
ambient energy source harvested by, for example, a 
small wind turbine or an array of conventional 30 
volt 4 amp hour 
solar power cells. The 
water consumption rate is generally less then approximately 10 percent that of a conventional 
evaporative cooler. The 
humidity in the interior of the structure is generally no more than approximately 2 to 2.3 times that of the exterior environment.