page_title: Cyclone Daman
section_title: Meteorological history
hierarchical_section_title: Cyclone Daman / Meteorological history
caption_attribution_description: English: Track map of Severe Tropical Cyclone Daman of the 2007-08 South Pacific cyclone season. The points show the location of the storm at 6-hour intervals. The colour represents the storm's maximum sustained wind speeds as classified in the Saffir–Simpson scale (see below), and the shape of the data points represent the nature of the storm, according to the legend below. Saffir–Simpson scale Tropical depression≤38 mph≤62 km/h Category 3111–129 mph178–208 km/h Tropical storm39–73 mph63–118 km/h Category 4130–156 mph209–251 km/h Category 174–95 mph119–153 km/h Category 5≥157 mph≥252 km/h Category 296–110 mph154–177 km/h Unknown Storm type Tropical cyclone Subtropical cyclone Extratropical cyclone / Remnant low / Tropical disturbance / Monsoon depression
context_page_description: Severe Tropical Cyclone Daman was the strongest cyclone of the 2007–08 South Pacific cyclone season. Cyclone Daman was the fourth tropical depression and the first severe tropical cyclone to form east of longitude 180° during the 2007–08 South Pacific cyclone season. Due to the severity of the storm, the name Daman was retired and replaced with Denia.
  On December 3, the Regional Specialized Meteorological Centre in Nadi, Fiji, upgraded a tropical disturbance, located to the west of the Solomon Islands, to Tropical Depression 04F. On December 5, as the depression moved towards the west into the Fijian archipelago, both the Joint Typhoon Warning Center and RSMC Nadi upgraded it to Cyclone Daman. On December 7 the cyclone reached its peak intensity with winds of 185 km/h, which made Daman a Category 4 cyclone on the Australian Tropical Cyclone Intensity Scale. Later that day Daman also reached its peak intensity by 1-minute means with winds of 205 km/h which made it a Category 3 tropical cyclone on the Saffir-Simpson Hurricane Scale. Early on December 8, Cyclone Daman brushed by the Fijian island of Cikobia, causing damage to housing, crops and vegetation.
context_section_description: During December 3, the Fiji Meteorological Service and the United States Joint Typhoon Warning Center reported that an area of atmospheric convection, had persisted about 1,000 km (620 mi) to the north-west of Suva the capital of Fiji. At this time the system was located within an area of minimal vertical wind shear and warm sea surface temperatures. Over the next two days, the depression moved towards the west, conditions surrounding the depression barely changed and as a result the depression steadily intensified. Early on December 5, the system had convective bands spiraling into and wrapping tightly around the low level circulation center. As a result of this, the JTWC started advisories on Tropical Cyclone 05P, with winds equivalent to a tropical storm. At 0200 UTC, RSMC Nadi reported that the tropical depression had intensified into a category one tropical cyclone on the Australian tropical cyclone intensity scale and named it as Daman. During that day Daman passed over Rotuma island while gradually intensifying further.
  At 0600 UTC, on December 6, the JTWC reported that Daman had intensified into a category one tropical cyclone on the Saffir-Simpson Hurricane scale. Shortly after this, the cyclone made an abrupt turn and started to move towards the east instead of moving towards the south. Later that day at 1200 UTC, RSMC Nadi reported that Daman had intensified into a category three severe tropical cyclone as it was now sporting a cloud filled eye. The cyclone continued to intensify over the next 12 hours becoming a category four severe tropical cyclone at 0000 UTC on December 7. At that time RSMC Nadi forecasted, that there was a possibility that Daman could become a category five severe tropical cyclone, with windspeeds of 215 km/h, (130 mph), within 12 hours. However six hours later as the general organization of the eye had weakened, RSMC Nadi reported that the cyclone had peaked as a category four severe tropical cyclone with ten-minute winds of 195 km/h, (120 mph) and a peak pressure of 925 hPa (27.3 inHg). The JTWC also reported that Cyclone Daman had peaked with one-minute winds of 195 km/h, (120 mph). In their post storm analysis, both RSMC Nadi and the JTWC revised their estimated peak windspeeds, with RSMC Nadi lowering their estimated windspeeds to 185 km/h, (115 mph), while the JTWC elevated their estimates to 205 km/h, (125 mph). As the Cyclone peaked in intensity, it started to accelerate towards the southeast and passed over or close to Thikombia island, before becoming under the influence of a mid-level ridge of high pressure. As it came under the influence of the mid-level ridge of high pressure, Daman turned once more and started to move slowly towards the southeast, into an area of strengthening vertical windshear and cooler sea surface temperatures. As a result, Daman rapidly weakened during December 8, before both the next day as the system moved through the Lau Islands, both the JTWC and RSMC Nadi reported that it had weakened into a tropical depression. The final advisories on the system were issued the next day as Daman merged with a frontal system.
caption: Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale
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