Rainfall during the week ending 23 April, 2006Figure 2. TRMM made several passes over Monica, during both the early and the mature stages of the storm. The system intensified to hurricane-force strength before making landfall 40 km south of Lockhart River on the afternoon of 19 April. The low moved towards the southwest under the influence of a weakening ridge to the south. A tropical low was analysed in the far northern Coral Sea on 16 April. The typhoon lost strength before coming ashore on May 2 as a Category 3/4 storm, but it still carried very powerful winds and heavy rain when it struck the low-lying coastal plains, causing severe damage. In this case, TRMM showed a pattern of very heavy rain (red) forming an intense symmetric eyewall around a small, complete eye with tightly curved rainbands spiraling into the center—the signature of a mature, intense passive microwave sensor, TRMM can peer into the core of these storms and relay Tropical cyclone Monica was the first cyclone to affect the Eastern Australian region in the 1984-85 season. Cyclone Nargis passed over Burma (Myanmar) after having formed in the Bay of Bengal. Monica formed about 0300 UTC on 27 December 1984 near 16.5°S, 152.0°E from a tropical low which had been embedded in the ITCZ for about 36 hours. The Category 5 cyclone hit along the sparsely populated coastline of the Northern Territory, sparing the city of Darwin. There it reached cyclone intensity on 17 April and began a more westward track toward Cape York Peninsula. important details on storm structure and location to forecasters. The central pressure at this time was 990 hPa. The rain rates are overlaid on infrared data from the TRMM Visible Infrared Scanner.At the time of this TRMM overpass, Monica’s sustained winds were estimated to be 230 kilometers/hour (144 mph) or equivalent to a Category 4 hurricane on the Saffir-Simpson scale. This is the same general area where Cyclone Larry formed a month earlier. Since its launch in 1997, TRMM has provided valuable information on tropical storms. With an active radar and a The Earth Observatory is part of the The low moved towards the southwest under the influence of a weakening ridge to the south. There it reached cyclone intensity on 17 April and began a more westward track toward Cape York Peninsula. Severe Tropical Cyclone Monica was the most intense tropical cyclone, in terms of maximum sustained winds, on record to impact Australia. Rainfall during the week ending 29 April, 2006Figure 6.

The system intensified to hurricane-force strength before making landfall 40 km south of Lockhart River on the afternoon of 19 April. Cyclone Monica, also designated Severe Tropical Cyclone Monica, was a tropical cyclone that affected northern Australia from April 17, 2006 until April 26, 2006. Rain rates in the center swath are from the TRMM Precipitation Radar, and rain rates in the outer swath are from the TRMM Microwave Imager. News reports cited a death toll of 10,000 people, with thousands more missing, as of May 5. The 17th and final storm of the 2005–06 Australian region cyclone season, Monica originated from an area of low pressure off … The visualization combines data from several different instruments from the Tropical Rainfall Measuring Mission (TRMM) satellite, which observed the storm at 16:08 UTC on April 22, 2006 (1:38 a.m., April 23, Australian CST). The Category 5 cyclone hit along the sparsely populated coastline of the Northern Territory, sparing the city of Darwin. Just 12 hours after landfall the system had weakened to below cyclone intensity, and passed to the north of Darwin as a tropical low during the afternoon of 25 April.All times in UTC - add 10 hours to convert to EST and 9.5 hours to convert to CST.Figure 1. At one point, Nargis was a Category 4 cyclone, with sustained winds of 210 kilometers per hour (130 miles per hour).

The system weakened over land, before entering the Gulf of Carpentaria as a weak cyclone early the following day.Increasing shear and being over land contributed to the weakening process but it appears the entrainment of mid-level dry air was the most important factor. Monica originated in the Coral Sea below the southeastern tip of Papua New Guinea, becoming a minimal tropical storm on April 17, 2006. The storm tracked due west towards the Cape York Peninsula in Queensland, where it came ashore just south of Lockart River on the afternoon of April 19 as a Category 3 cyclone. Monica weakened as it crossed the peninsula, but when it reached the warm waters of the Gulf of Carpentaria on the other side, it re-organized and re-intensified.The image above shows Cyclone Monica during this re-intensification. tropical cyclone.

With an active radar and a passive microwave sensor, TRMM can peer into the core of these storms and relay details on storm structure and location to forecasters.Tropical Cyclone Monica formed off the northeastern coast of Australia on April 17, 2006. The cyclone tracked westward, skirting the northern coastline of Australia before coming ashore west of Maningrida in the Northern Territory just after 8 p.m. local time. The storm quickly lost strength as it moved inland and passed by the main population center of Darwin.TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Gove radar at 9:20pm CST on 23 April 2006. Monica originated in the Coral Sea below the southeastern tip of Papua New Guinea, becoming a minimal tropical storm on April 17, 2006. Cyclone Monica became the strongest storm of the 2006 Australian cyclone season with wind gusts reaching 350 kilometers per hour (215 miles per hour) as reported by the Australian Bureau of Meteorology’s Cyclone Warning Centre. Soon after these images were taken, Monica reached Category 5 status with sustained winds estimated at 285 km/hr (178 mph).

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