With the advancement of the night, an impressive maximum winds at lower layers of up to 60 knots, will develop ahead of the cold front advancing a line of instability, support rapid moisture transport to the south and increasing storm intensityThe dynamic jet provided by the lower layers and especially the contribution made thermal silver basin enhance the development of severe storms over the mouth of the river. As we move through the line of instability associated with the formation of arc-shaped echoes, you can observe the development of supercells. ..
As I mentioned on Wednesday, the center would end surface low pressure developing in nearby Monte Hermoso. These forecast maps seen as the center of it ends up being the S of the province of Buenos Aires.
In the last image seen as the low pressure system pushing cold air ends from the SW to the N. This front interaction region continue its travel when the dynamic contribution is important enough to do