 Cristina initially had well @-@ established upper @-@ level outflow . It failed to reach hurricane status , peaking with maximum sustained winds of 65 mph ( 105 km / h ) due to movement of its associated upper @-@ level anticyclone to the north over Mexico which caused Cristina to be exposed to easterly vertical wind shear . Cristina moved generally northwestward , which eventually placed the storm in cooler waters , and caused the deep convection of the system to dissipate . On June 14 , Cristina diminished to a tropical depression . Cristina moved west @-@ northwestward with the low @-@ level flow . The depression dissipated as a tropical cyclone on June 16 , after a lack of deep convection for 48 hours . 
