Are You Embarrassed By Your Drain Repairs Skills? Here’s What To Do

On September 21, a tropical wave emerged into the Atlantic from the west coast of Africa. Beta soon became an extratropical low inland near the Texas coast. A large, extratropical low-pressure area developed over the northeast Atlantic Ocean on September 14, following the interaction between a surface front and an upper-level low. The extratropical remnants of Beta brought heavy rainfall to other states, especially Louisiana and Mississippi. The storm produced strong winds, heavy rainfall, flash flooding, landslides, and mudslides in the region. In preparation for Alpha on September 18, orange warnings were raised for high wind and heavy rain in Coimbra and Leiria districts of Portugal. The depression headed slowly northeastward and intensified, becoming Tropical Storm Beta late on September 18. Although dry air generated by a surface trough and an upper-level trough prevented Beta from rapidly intensifying, the cyclone was able to reach a peak wind speed of 65 mph (105 km/h) around 12:00 UTC on September 20 and a minimum pressure of 993 mbar (29.3 inHg) around 00:00 UTC on the next day. It’s a bit of a long story, so I’ll probably cover it some other day.

Dry air limited convection associated with the wave for several days, before convection increased as the system reached the western Caribbean on September 30. A surface low-pressure area developed early on October 2, and then the convection became sufficiently organized, resulting in the formation of Tropical Depression Twenty-Five by 06:00 UTC that day about 300 mi (485 km) southeast of Cozumel, Quintana Roo. It continued to produce disorganized convection through its final landfall, which occurred at 03:00 UTC on October 6, near San Felipe, Yucatán, with winds of 35 mph (55 km/h). Beta made landfall at 02:45 UTC on September 22, over the southern end of Matagorda Peninsula, near Port O’Connor, Texas, with winds of 50 mph (80 km/h). The low peaked with sustained winds of 70 mph (115 km/h) on September 15. Although the low weakened as it headed south-southeastward, the wind field contracted and convection began forming closer to the circulation due to marginally warm sea surface temperatures and sufficient atmospheric instability. Despite extremely strong shear partially caused by Hurricane Teddy’s outflow removing all but a small convective cluster to the northeast of its center, Vicky intensified further, reaching its peak intensity with maximum sustained winds of 50 mph (80 km/h) and a pressure of 1,001 mbar (29.6 inHg) at 12:00 UTC on September 15. Over the ensuing couple of days, the storm was beset by increasing wind shear, and it weakened to a tropical depression around 12:00 UTC on September 17. Then, about six hours later, it degenerated into a remnant low about 920 mi (1,480 km) west-northwest of the northwesternmost Cabo Verde Islands and subsequently dissipated.

Three hours later, it degenerated to a post-tropical remnant low near Viseu, Portugal. Six hours later, the storm attained its peak intensity with sustained winds of 40 mph (65 km/h) and a minimum pressure of 1,006 mbar (29.7 inHg). Alpha continued to strengthen and attained its peak intensity as a subtropical system around 00:00 UTC on September 18, with maximum sustained winds of 50 mph (80 km/h) and a minimum pressure of 996 mbar (29.4 inHg). An area of disturbed weather, composed of a tropical wave, an upper-level low-pressure area, and a frontal trough, stretched from the western Caribbean to offshore the Southeastern United States on September 5 and September 6. Drifting westward, the disturbance reached the northeastern Gulf of Mexico and consolidated by September 12. However, development of the system was not expected at the time due to strong upper-level winds produced by Hurricane Sally, which made landfall in Alabama on September 16 and then moved across the Southeastern United States. Numerous tropical storm watches and warnings were issued by the government of Mexico for parts of the Yucatán Peninsula following the formation of Gamma and several thousand people were evacuated to shelters.

Extensive flooding was reported in the city, while at least 30 people were forced to evacuate their homes due to rising floodwaters. People in the following West Thurrock locations recently needed a drainage specialist: Salisbury Avenue, Southend Road, Mucking Wharf Road, Fairview Avenue, Valmar Avenue, The Hollies, Kingsman Road, Corringham Road, Romsey Close, Adams Road, Baryta Close, Broadhope Avenue, Butts Road, St Margarets Avenue, High Road, Walton’s Hall Road, Rayleigh Road, Bell-reeves Close, Victoria Road, The Green, Fetherston Road, Chantry Crescent, Poley Road, Billet Lane, and also in these nearby postcodes RM16 1XL, RM20 3JA, RM20 4AB, RM20 3AL, RM20 3LJ, RM20 3NE, RM20 3HR, RM16 1EE, RM16 1GP, RM16 1AB. These places recently saw activity by specialists in drain unblocking. Houston officials reported that over 100,000 gallons of domestic wastewater spilled at five locations in the city as a result. At least 20-25 homes in the Houston metropolitan area suffered flood damage. Beta caused widespread moderate to major flooding in portions of the Greater Houston metropolitan area. Flooding in Chiapas damaged 543 homes, 326 roadways, 13 sections of a waterpipe network, and 2 schools. Gamma caused at least six deaths in Mexico, with four in Chiapas and two in Tabasco.

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