The main salt-ways, though difficult to date, again led southeastwards.
Moving southeastward, the system slowly developed as wind shear in the region slowly decreased.
The depression tracked east-southeastward, under the influence of a mid-level ridge.
By this time, the storm had also begun a southeastward track.
After turning to the northwest, it looped southeastward and gradually became separated from the surface frontal system, due to the deepening of the upper-level trough over the system.
The storm moved southeastward, followed by a north, then northeast motion.
The road proceeds, bending southeastward and passing a few small houses and fields.
Moving southeastward, the convection quickly organized around the center, aided by warm sea surface temperatures and convergence.
