 The National Hurricane Center remarked the potential for the system transitioning into a tropical cyclone . An approaching trough caused the storm to stall and weaken the deep convection . On April 23 , the cyclone weakened to depression status due to strong wind shear . A Hurricane Hunters flight into the system confirmed the weakening , and also reported a 1 @.@ 8 ° F ( 1 ° C ) temperature rise in the center , suggesting a warm core and some tropical characteristics . Early on April 24 , the subtropical depression turned eastward , maintaining limited convection . At the time , forecasters anticipated the depression would continue east @-@ northeastward and become an extratropical cyclone . By late on April 24 , the system was too weak to classify using the Dvorak technique , and the NHC ceased issuing advisories . Within 24 hours , the circulation dissipated as the system continued eastward through the westerlies . 
