Matches in DBpedia 2015-10 for { ?s ?p "Severe Tropical Cyclone Rusty was a strong, slow-moving tropical cyclone that produced record duration gale-force winds in Port Hedland, Western Australia in late February 2013. Originating as an area of low pressure on 22 February well to the northwest of the Kimberley region of Western Australia, the precursor to Rusty steadily developed within a favourable environment. Gradually decreasing surface pressures in the region signaled intensification and the low was classified as Tropical Cyclone Rusty on 23 February. Although a large, sprawling system, near-record high sea surface temperatures enabled Rusty to quickly deepen. Becoming essentially stationary on 25 February, the system acquired hurricane-force winds as its core improved in structure. The cyclone achieved its peak intensity two days later with maximum ten-minute sustained winds of 165 km/h (105 mph) and a barometric pressure of 945 mbar (hPa; 27.91 inHg). Thereafter, interaction with land caused its core to collapse before the system made landfall near Pardoo Station. Rusty weakened below cyclone strength on 28 February. Its remnants persisted over Western Australia for several more days before being absorbed into an extratropical cyclone on 5 March.Owing to the slow-moving nature of Rusty, a large swath of coastal Western Australia saw heavy rains from the storm with a storm peak of 374 mm (14.7 in) at De Grey Station. Substantial flooding took place accordingly; the De Grey River crested just shy of its all-time record at 17.23 m (56.5 ft). Some structural damage took place, but the predominant effects of the storm were sustained by agriculture and infrastructure. Economic losses related to the storm were estimated to be as high as A$500 million (US$480 million). The name Rusty was later retired and replaced with Rubina."@en }
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- Cyclone_Rusty abstract "Severe Tropical Cyclone Rusty was a strong, slow-moving tropical cyclone that produced record duration gale-force winds in Port Hedland, Western Australia in late February 2013. Originating as an area of low pressure on 22 February well to the northwest of the Kimberley region of Western Australia, the precursor to Rusty steadily developed within a favourable environment. Gradually decreasing surface pressures in the region signaled intensification and the low was classified as Tropical Cyclone Rusty on 23 February. Although a large, sprawling system, near-record high sea surface temperatures enabled Rusty to quickly deepen. Becoming essentially stationary on 25 February, the system acquired hurricane-force winds as its core improved in structure. The cyclone achieved its peak intensity two days later with maximum ten-minute sustained winds of 165 km/h (105 mph) and a barometric pressure of 945 mbar (hPa; 27.91 inHg). Thereafter, interaction with land caused its core to collapse before the system made landfall near Pardoo Station. Rusty weakened below cyclone strength on 28 February. Its remnants persisted over Western Australia for several more days before being absorbed into an extratropical cyclone on 5 March.Owing to the slow-moving nature of Rusty, a large swath of coastal Western Australia saw heavy rains from the storm with a storm peak of 374 mm (14.7 in) at De Grey Station. Substantial flooding took place accordingly; the De Grey River crested just shy of its all-time record at 17.23 m (56.5 ft). Some structural damage took place, but the predominant effects of the storm were sustained by agriculture and infrastructure. Economic losses related to the storm were estimated to be as high as A$500 million (US$480 million). The name Rusty was later retired and replaced with Rubina.".