Beryl A well-developed tropical wave exited Africa on August 27. The next day, it developed into a tropical depression, and shortly thereafter it intensified into Tropical Storm Beryl. On August 29, it passed just south of Cape Verde as it continued intensifying on its west-northwest track. An eye feature appeared in the convection on August 31, suggesting winds of near hurricane status; since the feature was located on the western side of the deep convection and the storm was slightly asymmetric, the intensity was held just below hurricane status. Shortly after, strong wind shear caused the storm to deteriorate, leaving the low-level circulation exposed on the western side. Beryl weakened to a tropical depression the next day due to the lack of convection, and it continued westward without redevelopment. On September 5, a reconnaissance flight into the depression found winds of ; this was deemed unrepresentative of the actual intensity as it was recorded in a squall line. The depression became disorganized once more and by September 6, it was no longer identifiable on satellites. Early in its duration, Tropical Storm Beryl produced heavy rainfall and gusty winds on the Cape Verde island of Sal. The storm caused moderate damage across the archipelago, totaling $3 million (1982 USD). The passage of Beryl resulted in three casualties in Brava Island, as well as 122 injuries. In the period after the storm's passage, the United States provided humanitarian aid and economic assistance to the country, helping the archipelago to reverse the effects of Beryl. Tropical Depression Three This system formed east of the Lesser Antilles on September 6 to the southeast of Tropical Storm Beryl in the tropical North Atlantic Ocean. The depression moved northeast of the Leeward Islands during the afternoon of September 7 while experiencing southwest vertical wind shear, and moved into the southwest North Atlantic before dissipating east of the Bahamas on September 9. Tropical Storm Chris A surface low-pressure area developed on September 8 in the Gulf of Mexico. It drifted westward, and the next day it organized into a subtropical depression. Under the influence of a trough of low pressure, the depression turned northward, and after steadily becoming better organized it transitioned into Tropical Storm Chris by late on September 10. The storm attained peak winds of before moving ashore near Sabine Pass in Texas. Chris continued inland until it dissipated over central Arkansas on September 13.