 Despite continuing effects from the strong wind shear , a large , deep burst of convection formed in the northern <unk> of <unk> . The center was found to have shifted towards the new convection leading to an increase in intensity . The forecast showed a slight decrease in wind shear as <unk> continued westward and no change in intensity over the 5 @-@ day forecast was predicted . However , the convection decreased once more and the low became completely exposed by the late morning hours and <unk> weakened again . By the afternoon , the center of <unk> was only a <unk> of clouds , devoid of convection . During the overnight hours on September 4 into the morning of September 5 , convection associated with <unk> began to <unk> somewhat , mostly to the north of the circulation , due to the strong <unk> wind shear . By mid @-@ morning , <unk> re @-@ intensified slightly due to the redevelopment of some convection . However , the redevelopment was short lived and wind shear again took its toll on <unk> by late morning . The convection around the system became <unk> from the center and <unk> weakened slightly . 
