Early in its duration while it was still in the Australian basin, the cyclone produced high waves near Christmas Island, forcing a boat of about 500 refugees to be escorted to port. Partial funding from the South African government Innovation Fund is gratefully acknowledged. Soc., 141–174. (a)–(h) Daily interpolated outgoing longwave radiation (contour interval 30 W m−2) from NCEP–NCAR for various days between 22 Feb and 1 Mar. 0000003460 00000 n Less than 5% of southwest Indian Ocean tropical cyclones actually make landfall on the east coast of southern Africa and even fewer significantly penetrate into the interior, because of the relatively dry 1–1.5-km-high interior plateau that covers most of the region. While crossing the Mozambique, Idai weakened to a tropical storm and entered Zimbabwe. Such underestimations of heavy rain by the Eta model, particularly near the escarpment, are common; for example, similar errors occurred for the early February 2000 tropical low case (Dyson and van Heerden 2001) and for a previous flooding event in 1996 (De Coning et al. width: 100%; The previous major cyclone, Cyclone Eline of February 2000, had a slightly different track but still coming in through the central Eastern Highlands and then moving right across Zimbabwe weakening as it did so and finally reaching Namibia as a minor depression. 334 0 obj << /Linearized 1 /O 336 /H [ 947 1137 ] /L 543003 /E 39774 /N 88 /T 536204 >> endobj xref 334 26 0000000016 00000 n height: 4px; Over the mainland, almost all countries do not have any NWP capacity, and the challenges and potential solutions for improved forecasting for the region are discussed. Using the definition of forecast skill as (CLIPER DPE − UKMO DPE)/CLIPER DPE × 100%, where DPE is the direct positional error between the model and observed center, the skill scores were 23%, 36%, and 51% for the 24-, 48-, and 72-h forecasts. If a westward steering current existed, then warm SSTs in the SWIO were found by these authors to further promote landfall. Although inland penetration is highly unusual, there were in fact three large-scale precursor features in existence over the region that have previously been identified as favoring a westward track of TCs (Olivier 1993). Further research is needed, but this suggests that improved TC predictability could result if a (Tropical Atmosphere Ocean) TAO-type monitoring array is established in the tropical SWIO. 1 shows the wind speeds associated with south Indian Ocean storm categories. Cyclone Idai, which devastated Zimbabwe’s eastern border districts of Chimanimani and Chipinge in mid March after drowning Mozambique’s second largest city of Beira, has been described by the United Nations’ World Food Programme (WFP) Executive Director David Beasley as the biggest natural disaster to hit the region in living memory. Zimbabwe floods: No lessons learnt. Less known is that ex-Eline tracked about 2000 km across southern Africa toward the Atlantic (Fig. In Mozambique, an … 4a,b) helped sustain the landfalling Eline as it tracked farther west (e.g., Jury and Pathack 1991). 5f–h) existed over the region from Botswana east to the SWIO during 24–29 February, thereby continuing to steer the storm westward to Namibia. Cyclone has left a trail of destruction and now UNICEF says it needs about 30 million U.S. dollars to restore the three affected countries. Less well known is that one of the weather systems that contributed to these floods (ex-Tropical Cyclone Eline) … Rep. 342, 14 pp. Although there were some errors in the predicted speed and intensity of Eline, La Réunion forecasts were generally quite accurate regarding track and landfall position. At 0600 UTC 22 February, the bulletin noted that the eye was on the Mozambique coast and forecast that Eline would track into Zimbabwe within 36–48 h. ENSO and climatic signals across the Indian Ocean basin in the global context. At 0600 UTC 21 February, a storm warning was issued along with advice that Eline might intensify steadily during the next day. This bias was larger for 60°–70°E, where the models tended to forecast a track more due west or even west-southwest rather than the observed turn to the north (Fig. La Niña conditions strengthened again during early 2000 after a lull in mid-1999 and warm SST anomalies evolved near Mozambique (Fig. The tropical storm, named Cyclone … display: flex; These authors present evidence that years with deeper-than-average thermocline depth in the 8°–12°S, 50°–70°E region tend to have more TC in the SWIO than those with shallower thermocline depths. Bulletin of the American Meteorological Society, Journal of Applied Meteorology and Climatology, Journal of Atmospheric and Oceanic Technology, An Analysis of Subdaily Severe Thunderstorm Probabilities for the United States, Subseasonal Forecast Skill of Snow Water Equivalent and Its Link with Temperature in Selected SubX Models, Configuration of Statistical Postprocessing Techniques for Improved Low-Level Wind Speed Forecasts in West Texas, Topographic Rainfall of Tropical Cyclones past a Mountain Range as Categorized by Idealized Simulations, https://doi.org/10.1175/1520-0434(2004)019<0789:TCEAIU>2.0.CO;2, 10.1175/1520-0434(2004)019<0789:TCEAIU>2.0.CO;2. 8c) corresponds to the second major wet spell of the summer over southern Namibia, including its wettest day (29 February), and shows some similarities in moisture flux with pentad 1 over the mainland. Each southern African country has its own meteorological service but only the South African Weather Service runs a regional NWP model (Eta). 11c. Other satellite products, available to La Réunion after the 1998/99 season, are from research-type platforms (Special Sensor Microwave Imager, Tropical Rainfall Measurement Mission, Advanced Microwave Sounding Unit) and have led to improvements in TC forecast accuracy (RSMC La Réunion 2002). J. However, the intensity of the system was underforecast during this period, and the forward track speed was overforecast. We thank Dr. Warren Tennant, SAWS, for helpful discussions. 0000024810 00000 n Second, a trough aligned northwest–southeast across the southern African interior existed on 21–24 February (Fig. 9b,c), discouraging a track farther south into the SWIO as is usual. 1, 2a). Waters immediately southeast of Madagascar were 0.5°–2°C cooler than average during both months (Figs. During El Niño, TC tracks tend to concentrate in the 50°–70°E band just east of Madagascar since the high pressure anomalies centered over the eastern Indian/ Australasian sector are unfavorable for TCs farther east. In 2000, Cyclone Eline devastated parts of the country, claiming 136 lives and destroying tens of thousands of houses. While crossing the Mozambique, Idai weakened to a tropical storm and entered Zimbabwe. At 0600 UTC 22 February, the bulletin noted that the eye was on the Mozambique coast and forecast that Eline would track into Zimbabwe within 36–48 h. Instead, the system moved considerably faster than expected and reached eastern Zimbabwe within 12–18 h. The next three forecasts issued between 1200 UTC 22 February and 0000 UTC 23 February predicted a more rapid weakening of ex-Eline than was observed. This may be something that could be implemented by forecast offices with more resources, for example, RSMC La Réunion. Zimbabwe and Malawi. The enhanced vegetation and soil moisture over much of southern Africa implies increased latent heat flux into the atmosphere, which is conducive to local intensification of weather systems. Information brochure, Météo France, La Réunion, 12 pp. These areas included the track of ex-TC Eline across southern Africa, implying that the precursor surface conditions over the land were considerably moister than average. Two important statistics are the mean position errors in the along-track (AT) and cross-track (CT) directions. Eline also killed 12 people in Zimbabwe and 21 people in South Africa. 1) and contributed significantly to the semidesert region of Real-time advisory positions produced by La Réunion were used to verify observations of the location of the system. 2) and its associated low-level moisture convergence and convection (Figs. Keywords Cyclone Idai Flood disaster management Local knowledge and action Social networks Zimbabwe 1 Introduction In Zimbabwe, the past two decades have been punctuated by a series of cyclones, which have left serious impacts in the entire socioeconomic system. 9), favoring local intensification and landfall of tropical systems. The associated convection over southern Namibia on 29 February produced the greatest daily falls of the entire summer (40–60 mm at several stations). During 24–27 February, the storm moved over northeastern Botswana toward Namibia (Figs. Note that UKMO statistics are computed over the full ocean track of the storm (4–23 February) whereas the La Réunion results are only for 8–21 February (24-h forecast) or 8–19 February (48-h forecast). 2002) show positive anomalies of 30%–100% across much of southern Africa in December 1999 and January 2000, indicating that the vegetation was substantially greener than average. 0000035209 00000 n Elita Chikwati Senior Reporter The potential cyclone threat to Zimbabwe in around a week’s time is still a tropical depression north east of Mauritius and heading towards northern Madagascar, which may well have 100mm to 200mm of rain over this weekend. 0000025096 00000 n 4b–e, 6). The NCEP/NCAR 40-Year Reanalysis Project. S. Afr. By 1200 UTC 23 February the storm was centered near 30°E, with severe flooding resulting in southeastern Zimbabwe. Email: cjr@egs.uct.ac.za. 0000015934 00000 n Heming, J. T., 1994: Keeping an eye on the hurricane—Verification of tropical cyclone forecast tracks at the Met Office. We thank two anonymous reviewers for their comments, which helped to improve the paper. During La Niña, TC tracks in the tropical south Indian Ocean are relatively spread out, with more occurring in the Mozambique Channel. J. Atmos. Over southern Namibia, the February and March rainfall were each over two standard deviations above average and JFM 2000 represented by far the wettest season since 1976. The worst affected areas stretched along the border with van Heerden, J., , and Taljaard J. J. , 1988: Africa and surrounding waters. Shading denotes values less than or equal to 240 W m−2 or areas where convection is likely, (a)–(h) Zonal wind (contour interval 5 m s−1) at the 500-hPa level from NCEP reanalyses for various days during 18–28 Feb. 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