It has been suggested that this article be merged into 2008 Atlantic hurricane season . ( Discuss ) Proposed since December 2025. |
| Tropical Storm Laura at peak intensity on September 30 | |
| Meteorological history | |
|---|---|
| Formed | September 29,2008 |
| Extratropical | October 1,2008 |
| Dissipated | October 4,2008 |
| Tropical storm | |
| 1-minute sustained (SSHWS/NWS) | |
| Highest winds | 60 mph (95 km/h) |
| Lowest pressure | 994 mbar (hPa);29.35 inHg (990 mbar (29.53 inHg) while extratropical) |
| Overall effects | |
| Fatalities | None |
| Damage | Minimal |
| Areas affected | Azores,Atlantic Canada,Greenland,Europe |
| IBTrACS | |
Part of the 2008 Atlantic hurricane season | |
Tropical Storm Laura was a large but short-lived tropical cyclone that developed over the north-central Atlantic Ocean in late September during the 2008 Atlantic hurricane season. Laura's remnants later impacted the Netherlands,Germany,and Norway. The 12th named storm of the season,Laura formed out of a large extratropical area of low pressure located about 1,015 miles (1,633 km) west of the Azores on September 29. Laura slowly developed tropical characteristics throughout the day as it moved over warmer waters. On the afternoon of September 30,Laura had acquired enough tropical characteristics to be designated a tropical storm. Shortly after being declared tropical,Laura began to undergo an extratropical transition,which did not fully take place until the morning of October 1. Laura degenerated into a post-tropical cyclone later that morning,and the final advisory by the National Hurricane Center was issued. The remnants of Laura contributed to heavy rainfall and power outages in the British Isles,the Netherlands,and Norway on October 5 to 8.
On September 26, a large extratropical area of low pressure developed along a frontal system west of the Azores. The low intensified into the equivalent of a hurricane with winds of 80 mph (130 km/h) at 12:00 UTC on September 27. Over the following days, the low lost its frontal features and weakened as it traveled westward. By September 29, the low developed sufficient convection around the center, and the NHC classified it as Subtropical Storm Laura at 06:00 UTC. The subtropical designation was due to the storm's proximity to an upper-level low. At the time, Laura had peak winds of 60 mph (95 km/h), based on estimates from satellite imagery. The storm's wind field contracted as it moved northward, steered by the remnants of Hurricane Kyle over Atlantic Canada. On September 30, Laura's structure transitioned into a tropical cyclone, based on more organized convection, and the storm's distance from the upper-level low. This was despite the storm moving over colder waters at a relatively high latitude. Cold air and increasingly colder water temperatures caused Laura to lose tropical characteristics on October 1, as it became a remnant low to the southeast of Newfoundland. On October 2, the remnants of Laura became extratropical and re-intensified, attaining hurricane-force winds the next day to the southeast of Greenland. The storm turned to the east and was absorbed by a large extratropical cyclone on October 4 to the west of the British Isles. [1] [2] [3] [4]
| Precipitation | Storm | Location | Ref. | ||
|---|---|---|---|---|---|
| Rank | mm | in | |||
| 1 | 150.0 | 5.91 | Bertha 2014 | Inverness, Highland | [5] |
| 2 | 135.0 | 5.31 | Charley 1986 | Abergwyngregyn, Gwynedd | [6] |
| 3 | 130.0 | 5.12 | Nadine 2012 | Ravensworth, North Yorkshire | [7] |
| 4 | 76.0 | 2.99 | Lili 1996 | Chale Bay, Isle of Wight | [8] |
| 5 | 61.7 | 2.43 | Zeta 2020 | Chipping, Lancashire | [9] |
| 6 | 48.8 | 1.92 | Grace 2009 | Capel Curig, Conwy | [10] |
| 7 | 42.2 | 1.66 | Gordon 2006 | Wainfleet All Saints, Lincolnshire | [11] |
| 8 | 38.0 | 1.50 | Gonzalo 2014 | Glenmoriston, Highland | [12] |
| 9 | 31.0 | 1.22 | Bill 2009 | Shap, Cumbria | [13] |
| 10 | 30.0 | 1.18 | Laura 2008 | Windermere, Cumbria | [14] |
Laura's remnants contributed to heavy rainfall across portions of Great Britain on October 5, causing floods that closed several roads. [15] [16] One person had to be rescued from her car after driving into a flooded street. The UK Environment Agency issued 76 flood watches and 21 severe flood warnings as a result of the rainfall. [17] On October 8, the remnants of Laura contributed to heavy rainfall in the Netherlands reaching 113 mm (4.4 in), [18] [19] Streets and homes in the village of Hippolytushoef were inundated. The large amounts of precipitation broke the daily and monthly rainfall records for October, which were previously set in 2006. [20] Gradually passing through Norway, the remnants of the storm caused significant damage to electric utilities. As a result, more than 10,000 people lost power in southern parts of the country. [21]