Emergency Humanitarian Aid for Populations Affected by Cyclone Indlala
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Preparatory Survey Report on the Mauritius Meteorological Services Project in the Republic of Mauritius
Mauritius Meteorological Services The Republic of Mauritius PREPARATORY SURVEY REPORT ON THE MAURITIUS METEOROLOGICAL SERVICES PROJECT IN THE REPUBLIC OF MAURITIUS November 2012 JAPAN INTERNATIONAL COOPERATION AGENCY JAPAN WEATHER ASSOCIATION INTERNATIONAL METEOROLOGICAL CONSULTANT INC. GE JR 12-143 Summary Summary Mauritius, a country consisting of small islands, is located in the cyclone-prone area of the Southwest Indian Ocean and is often affected by natural disasters such as heavy storms, tidal waves and floods caused by tropical cyclones, landslides and so on. Recently, climate change caused by global warming has posed a serious problem for Mauritius as it is predicted to have significant negative impacts on small island nations which are particularly vulnerable to a change in the natural environment. In addition, it is said that climate change has a potential to become the greatest threat to the sustainability of the very foundations of human survival. Thus, it is a significant global issue which developed and developing countries alike must deal with in mutually beneficial cooperation. In line with increasing global concerns on the intensification of disasters caused by climate change, the establishment of effective countermeasures against disasters such as severe storms, storm surges, and floods caused by tropical cyclones, rising sea level, tsunami, etc. has been an urgent task in Mauritius as well as in other countries in the Southwest Indian Ocean. In order for Mauritius to contribute to the alleviation of natural disasters in the Southwest Indian Ocean, the following are required and strongly desired: 1) An efficient meteorological observation system; and, 2) An Exchange of meteorological observation data and information about cyclones with neighboring countries in the Southwest Indian Ocean on a timely basis. -
CULTURES DE RENTE ET REDUCTION DES RISQUES DE CATASTROPHE, Cas Du District D’Antalaha
Université d’Antananarivo Faculté de Droit d’Economie de Gestion et de Sociologie Département Economie - Troisième Cycle Diplôme d’études supérieures spécialisées Multidisciplinaire en Gestion des Risques et des Catastrophes DMGRC Mémoire de fin d’études pour l’obtention du Diplôme d’études supérieures spécialisées Multidisciplinaire en Gestion des Risques et des Catastrophes CULTURES DE RENTE ET REDUCTION DES RISQUES DE CATASTROPHE, Cas du district d’Antalaha Présenté par : RAZAKANDRAINY Mandimby Encadreur pédagogique : Mr ANDRIANANJA Heriniaina Rakotovao. Date de soutenance : 30 Août 2011 Université d’Antananarivo Faculté de Droit d’Economie de Gestion et de Sociologie Département Economie - Troisième Cycle Diplôme d’études supérieures spécialisées Multidisciplinaire en Gestion des Risques et des Catastrophes DMGRC Mémoire de fin d’études pour l’obtention du Diplôme d’études supérieures spécialisées Multidisciplinaire en Gestion des Risques et des Catastrophes CULTURES DE RENTE ET REDUCTION DES RISQUES DE CATASTROPHE, Cas du district d’Antalaha Présenté par : RAZAKANDRAINY Mandimby Encadreur pédagogique : Mr ANDRIANANJA Heriniaina Rakotovao. Août 2011 REMERCIEMENTS Avant tout, nous rendons grâce à DIEU tout puissant, de nous avoir accordé la force, l’intelligence et la bonne santé durant les années de formation et la période de stage. Nous exprimons ici nos sincères remerciements à : - Monsieur RANDRIANALIJAONA Tiana Mahefasoa, Directeur de la formation DMGRC, d’avoir sacrifié son temps et ses efforts pour le bien de notre formation -
ECHOMDGBUD200701000 Dec
EUROPEAN COMMISSION DIRECTORATE-GENERAL FOR HUMANITARIAN AID - ECHO Emergency Humanitarian Aid Decision 23 02 01 Title: Humanitarian aid for the victims of flooding in Madagascar Location of operation: Madagascar Amount of Decision: EUR 1,500,000 Decision reference number: ECHO/MDG/BUD/2007/01000 Explanatory Memorandum 1 - Rationale, needs and target population. 1.1. - Rationale: Madagascar, an island off the southeast coast of Africa, east of Mozambique, suffers periodically the impact of cyclones while the southern part of the island is regularly affected by drought. The climate of Madagascar is tropical along the coast, temperate inland, and arid in the south. The weather is dominated by the southeastern winds that originate in the Indian Ocean anticyclone, a center of high atmospheric pressure that seasonally changes its position over the ocean. The east coast, being most directly exposed to the winds, is notorious for the destructive cyclones that occur during the rainy season, from November to April. Since December 2006, various regions of Madagascar were hit by cyclone Bondo, tropical storms Clovis, Enok, Favio and cyclone Gamede, which caused an exceptionally heavy rainfall affecting, in particular, the infrastructures of communication, health and agriculture. In the meantime, this year's rainy season has brought exceptional rains to most of the island. These conditions have contributed to heavy flooding in large, populated and cultivated areas throughout the country, resulting in over 90,000 hectares of agricultural land affected1, over 85,000 metric tones (MT) of rice harvest lost (against an annual production of approximately 3,600,000 MT) and at least 33,000 displaced people. -
Seychelles Post Disaster Needs Assessment Tropical Cyclone Fantala
Seychelles Post Disaster Needs Assessment Tropical Cyclone Fantala April 2016 A Report by the Government of Seychelles With support from the European Union, the United Nations, and the World Bank A report prepared by the Government of Seychelles, with technical and financial support from the European Union (EU), the World Bank (WB), the Global Facility for Disaster Reduction and Recovery (GFDRR) and the United Nations (UN). Photos: Courtesy of: Government of Seychelles, Virgine Duvat, Adrian Skerrett, and Doekle Wielinga. Disclaimer: (PDNA) Report. The Boundaries, colors, denominations and any other information shown on this map do not imply, on the part of the World Bank Group, any judgement on the legal status of any territory, or any endorsement of acceptance of such boundaries. © 2016 Seychelles Post Disaster Needs Assessment Tropical Cyclone Fantala April 2016 A Report by the Government of Seychelles With support from the European Union, the United Nations, and the World Bank FOREWORD The tropical cyclone, Fantala, formed over the southwestern Indian Ocean on 11 April, 2016. It passed near Farquhar Atoll on April 17, with maximum sustained wind speeds of 241 km/h. On April 19, it sustained maximum wind speeds of 157 km/h, causing widespread damage. Tropical cyclone Fantala made landfall on the evening of Sunday 17 with winds up to 350 km/h. Significant damage was reported on Farquhar Island's environment, physical infrastructure, and coconut palm tree groves. On April 20, the Government of Seychelles declared the Farquhar group area, including Providence Atoll and St. Pierre a disaster area. The government is grateful that no one was killed or seriously injured from this disaster, thanks to adequate preparedness measures taken by the Government and the Islands Development Company. -
Université D Faculté Des Lettres Départemen
UNIVERSITÉ D’ANTANANARIVO FACULTÉ DES LETTRES ET SCIENCES HUMAINES DÉPARTEMENT DE GÉOGRAPHIE Filière Spécialisée en Environnement et Aménagement du Territoire (F.S.E.A.T) MÉMOIRE POUR L’OBTENTION DU DIPLÔME DE MAITRISE « VULNERABILITE DE LA VILLE COTIERE FACE AUX CYCLONES : CAS DE LA COMMUNE URBAINE D’ANTALAHA REGION SAVA » Présenté par : BE MELSON Evrald Angelo Sous la direction de : Madame Simone RATSIVALAKA, Professeur Titulaire au Département de Géographie Date de soutenance : 1O Octobre 2014 Octobre 2014 UNIVERSITÉ D’ANTANANARIVO FACULTÉ DES LETTRES ET SCIENCES HUMAINES DÉPARTEMENT DE GÉOGRAPHIE Filière Spécialisée en Environnement et Aménagement du Territoire (F.S.E.A.T) MÉMOIRE POUR L’OBTENTION DU DIPLÔME DE MAITRISE « VULNERABILITE DE LA VILLE COTIERE FACE AUX CYCLONES : CAS DE LA COMMUNE URBAINE D’ANTALAHA REGION SAVA » Présenté par : BE MELSON Evrald Angelo Président du jury : James RAVALISON, Professeur Rapporteur : Simone RATSIVALAKA, Professeur Titulaire Juge : Mparany ANDRIAMIHAMINA, Maitre de conférences Octobre 2014 REMERCIEMENTS Ce mémoire de Maitrise n’aurait pas été ce qu’il est aujourd’hui, sans le concours de plusieurs personnes, à qui nous aimerons témoigner notre plus profonde reconnaissance. Tout d’abord, nous remercions de tout profond de notre cœur le Dieu Tout Puissant de nous avoir donné encore la vie et l’opportunité d’avoir pu mener à terme ce travail de recherche. Aussi, Monsieur James RAVALISON, Professeur pour avoir accepté de présider notre soutenance ; Monsieur Mparany ANDRIAMIHAMINA, Maître de conférences pour avoir accepté de juger notre soutenance ; Madame Simone RATSIVALAKA, notre Directeur de mémoire pour sa constante dévotion à notre travail malgré ses multiples occupations. -
GROWING SEASON STATUS Rainfall, Vegetation and Crop Monitoring
REGIONAL FOOD SECURITY PROGRAMME GROWING SEASON STATUS Rainfall, Vegetation and Crop Monitoring 2006/2007 Issue 5 March 2007 Release date: 24 April 2007 Highlights Contents • Good rainfall performance in the northern half of the SADC region, but poor rains in the southern parts by the end of March Rainfall Performance … Pg. 1 2007. Vegetation Pg. 2 Performance… • The prolonged dry spells develop into drought affecting Regional Dry Spells, Pg. 2 Botswana, Lesotho, Namibia, Swaziland, southern Mozambique Floods & Cyclones … and southern Zimbabwe. Water Requirement Pg. 2 Satisfaction Index … • Food security prospects at both (some) national and regional level uncertain as drought sets in. FAO/WFP Crop and Food Rainfall Estimates … Pg. 3 Supply Assessments to take place in some of the drought affected countries Vegetation Maps … Pg. 4 • Persistent heavy rains resulted in widespread floods in Zambia, Rainfall Time Series + Madagascar and central Mozambique. Country Updates Pg. 6 January to March 2007 rainfall totals as Rainfall Performance percentage of average Cumulative rainfall analysis (Figure 1) shows that the southern half of the region has had a poor second half of the rainfall season. January to March rainfall totals have been below average for Botswana, Lesotho, eastern Namibia, Swaziland, South Africa and southern Zimbabwe. On the other hand, the northern parts of the region, including Malawi, northern Mozambique, Tanzania, Zambia, and parts of northern Zimbabwe, have had good accumulations of rainfall, conducive to good crop development and good pasture. However, in some of these areas excess rainfall has been detrimental to crop growth, and has caused widespread flooding in some of the main river basins of the region, particularly the Zambezi river basin. -
CIRENE Air–Sea Interactions in the Seychelles–Chagos Thermocline Ridge Region*
CIRENE Air–Sea Interactions in the Seychelles–Chagos Thermocline Ridge Region* BY J. VIALARD,+ J. P. DUVEL, M. J. MCPHADEN, P. BOURUET-AUBERTOT, B. WARD, # E. KEY, D. BOURRAS, R. WELLER, P. MINNETT, A. WEILL, C. CASSOU, L. EYMARD, T. FRISTEDT, C. BASDEVANT, Y. DANDONNEAU, O. DUTEIL, T. IZUMO, C. DE BOYER MONTÉGUT, S. MASSON, F. MARSAC, C. MENKES, AND S. KENNAN !"#$%&'"%()%*$+%,-"$,"-.%"/01-.2%/-%*," 3,'$4,"56%4,")*07$'%/",%2"$,/$8.-/"$,-0" 06%4,94-+0/).%*%"$,-%*46-$0,/"$,"4":%;" 6&$+4-$6"*%8$0,< hile easterly trade winds blow year-round over the southern Indian Ocean, surface W winds experience a striking reversal north of 10°S. During boreal summer, the low-level easterly flow penetrates northward, is deflected when crossing the equator, and forms the strong Indian monsoon jet. During boreal winter, north- easterly winds also bend while crossing the equa- tor southward and form a weak low-level westerly jet between the equator and 10°S (Fig. 1a). The cyclonic circulation at the meeting point of these two wind regimes is responsible for the formation of a peculiar oceanic structure: the “Seychelles Chagos thermocline ridge” (SCTR; Hermes and Reason 2008; see the “Seychelles–Chagos thermocline ridge” sidebar for a more complete explanation of the formation of this feature). This region has attracted attention because it is home to distinct oceanic and atmospheric vari- ability at multiple time scales, each time with sig- nificant climatic consequences. Anomalously warm sea surface temperature (SST) in the SCTR region is associated with increased ! =,'%*24-%*").0-08*4)." 0#"!>3?<">%%"@A.%"!$*9>%4" 3,-%*46-$0,")*0#$&%*” /$'%B4*" *Pacific Marine Environment Laboratory Publication Number 3179 #0*"+0*%"$,#0*+4-$0,< cyclonic activity near Madagascar and La Réunion Continent (Annamalai et al. -
CIRENE Air–Sea Interactions in the Seychelles–Chagos Thermocline Ridge Region*
CIRENE Air–Sea Interactions in the Seychelles–Chagos Thermocline Ridge Region* BY J. VIALARD,+ J. P. DUVEL, M. J. MCPHADEN, P. B OURUET-AUBERTOT, B. WARD, # E. KEY, D. BOURRAS, R. WELLER, P. MINNETT, A. WEILL, C. CASSOU, L. EYMARD, T. FRISTEDT, C. BASDEVANT, Y. DANDONNEAU, O. DUTEIL, T. IZUMO, C. DE BOYER MONTÉGUT, S. MASSON, F. MARSAC, C. MENKES, AND S. KENNAN A field experiment in the southwestern Indian Ocean provides new insights into ocean–atmosphere interactions in a key climatic region. hile easterly trade winds blow year-round W over the southern Indian Ocean, surface winds experience a striking reversal north of 10°S. During boreal summer, the low-level easterly flow penetrates northward, is deflected when crossing the equator, and forms the strong Indian monsoon jet. During boreal winter, north- easterly winds also bend while crossing the equa- tor southward and form a weak low-level westerly jet between the equator and 10°S (Fig. 1a). The cyclonic circulation at the meeting point of these two wind regimes is responsible for the formation of a peculiar oceanic structure: the “Seychelles Chagos thermocline ridge” (SCTR; Hermes and Reason 2008; see the “Seychelles–Chagos thermocline ridge” sidebar for a more complete explanation of the formation of this feature). This region has attracted attention because it is home to distinct oceanic and atmospheric vari- ability at multiple time scales, each time with sig- nificant climatic consequences. Anomalously warm sea surface temperature (SST) in the SCTR region is associated with increased X Underwater photograph of ASIP. See “The Air–Sea Interaction profiler” sidebar *Pacific Marine Environment Laboratory Publication Number 3179 for more information. -
FULL REPORT Data Collected in August/September 2010
Comprehensive Food and Nutrition Security and Vulnerability Analysis (CFSVA+N) RURAL MADAGASCAR FULL REPORT Data collected in August/September 2010 In partnership with: Office National de Nutrition VPM/Santé Publique The Gates Foundation IFAD UNDP Institut National de la Statistique Direction Générale de la Météorologie DSEC/Statistique Agricole Rural Madagascar Comprehensive Food and Nutrition Security and Vulnerability Analysis November 2011 Experts from different organizations have contributed to the drafting of this report; Maherisoa Rakotonirainy (VAM Officer, WFP), Isabelle Nirina (Data Analyst, WFP), Chiara Brunelli (Food Security Analyst, WFP), Rijasoa Rakotoarinoro (M&E/GIS, WFP), Amal Tucker Brown (Nutrition Specialist, UNICEF ), Paola Valenti (Nutrition Manager UNICEF) The report has been reviewed and cleared by the nutrition cluster and the food security and livelihood cluster. The study was funded by UNICEF and WFP with financial support from the Bill and Melinda Gates Foundation, IFAD and UNDP. The views expressed herein can in no way be taken to reflect the official opinion of the donor. For information about Food Security Analysis, visit www.wfp.org/food‐security For information about nutrition security, visit http://www.unicef.org/nutrition/index_4050.html For questions or comments concerning any aspect of the survey and this report, please contact: WFP Madagascar Mr Maherisoa Rakotonirainy [email protected] Ms Isabelle Nirina [email protected] Ms Katy Elliott [email protected] UNICEF Madagascar -
WTO Documents Online
WORLD TRADE G/AG/N/EU/2 16 February 2012 ORGANIZATION (12-0913) Committee on Agriculture Original: English NOTIFICATION The following submission, dated 16 November 2011, is being circulated at the request of the Delegation of the European Union. The notification concerns actions taken within the framework of the Decision on Measures Concerning the Possible Negative Effects of the Reform Programme on Least-Developed and Net Food-Importing Developing Countries (Table NF:1) during the calendar year 2007. G/AG/N/EU/2 Page 2 NOTIFICATION UNDER ARTICLE 16:2 OF THE AGREEMENT: MONITORING OF THE FOLLOW-UP TO THE DECISION ON MEASURES CONCERNING THE POSSIBLE EFFECTS OF THE REFORM PROGRAMME ON LEAST-DEVELOPED AND NET FOOD-IMPORTING DEVELOPING COUNTRIES: European Union REPORTING PERIOD: calendar year 2007 (1) Quantity of food aid provided to least-developed and net food-importing developing countries: 1. The contribution by the European Union (EU) for food aid and support operations in 2007 was €308 million. It was spent on products mobilized under the Food Aid Convention (FAC) and on contract aid provided by European Commission Directorate General for Humanitarian Aid and Civil Protection (DG ECHO). The contract aid was spent on products, support operations and transport, distribution, flanking measures and measures to monitor implementation. A substantial contribution to food aid and supporting operations was also delivered by Directorate General for Development and Relations with African, Caribbean and Pacific Countries (DG DEV) as part of Official Development Assistance delivered by the European Commission. 2. As a result of reorganization of instruments under the EU's Financial Perspectives exercise for 2007-2013, the responsibility for the management of humanitarian food aid budget line was transferred from the European Commission Directorate General EuropeAid Cooperation Office (DG AIDCO) to DG ECHO with effect from January 2007. -
Africa Weather Hazards Benefits Assessment
The USAID FEWS-NET Africa Weather Hazards Benefits Assessment for December 21 – 27, 2006 Weekly Introduction: Greater Horn of Africa Outlook The four month lead in the Greater Horn shows a slight tilt in the odds towards above normal precipitation in northern Somalia and nearby portions of Djibouti and Ethiopia. Certain parts of western Sudan have a slight tilt in the odds towards below normal precipitation. This area is near, although not part of, West Darfur. Further south there is a slight tilt in the odds favoring above normal precipitation in part of southern Somalia and across central and southern Tanzania. Weather Hazards Assessment Graphic: 2 Weather Hazards Text Explanation: 1) Poor rainfall totals across central and southern Mozambique has led to a delayed start of the season. Although there has been some improvement in the south, with the season already facing deficits has high as 50 percent of normal additional rainfall is needed. Central Mozambique meanwhile still has not seen a start to its season, which is already four dekads late and it is unlikely that a start to the season will occur during the coming period. 2) Positive ENSO conditions are occurring and are expected to continue through early 2007. Sea surface temperatures in the main index area of the Pacific Ocean are running 1.5 degrees Celsius above normal. Other areas are seeing anomalies as high as 2 degrees Celsius above normal. Therefore moderate El Nino conditions are currently being experienced. Based on climatological patterns in southern Africa during El Nino seasons, there is a link between positive ENSO conditions and dryness in Zambia, Zimbabwe, Botswana, Namibia, South Africa, Mozambique and Madagascar during the January to March portion of the wet season. -
Floods in the Northern Part of the Country and Drought in the South Resulted in Nearly 500,000 People in Need of Assistance
ANNUAL REPORT OF THE HUMANITARIAN / RESIDENT COORDINATOR ON THE USE OF CERF GRANTS Country Madagascar Humanitarian / Resident Coordinator Mr. Xavier Leus Reporting Period 1 January 2007- 12 August 2007 I. Executive Summary On the 20 February 2007, the Malagasy Government declared a national state of emergency in Madagascar after a succession of particularly severe storms – including Bondo, Clovis, Favio and Gamede – had battered the island since December. By the end of March, the combined effects of extensive floods in the northern part of the country and drought in the south resulted in nearly 500,000 people in need of assistance. Against this backdrop, a new cyclone, Indlala, struck the north-eastern coast of Madagascar on 15th March, with winds of more than 230 km/h. Even after moving inland, it still registered gusts up to 125 km/h. The storm also continued to unleash torrential rains. Floods washed away villages in the northeast of the country, silted paddy fields and other large agricultural areas, damaged road infrastructure, washed away bridges and made it impossible to reach a number of remote villages where communities remained in dire need of immediate relief aid. These conditions contributed to extensive flooding in heavily populated and cultivated areas throughout the country, including the capital region, the northwest, the northeast, and the southeast. The food security situation deteriorated dramatically, and the risk of maternal and child mortality linked to lack of access to services, and water- and vector-borne diseases, increased. The situation threatened to deteriorate further were timely assistance not provided to address immediate needs and restore agricultural production and livelihoods before the next cyclone season.