1 the 2005 Hurricane Season – a Sign of Climate Change? by Nancy Chen

Total Page:16

File Type:pdf, Size:1020Kb

1 the 2005 Hurricane Season – a Sign of Climate Change? by Nancy Chen The 2005 hurricane season – a sign of climate change? By Nancy Chen, intern at the RC/RC Climate Centre I. Background: Katrina and the trend in Atlantic hurricanes On Aug. 24, 2005, tropical Depression 12 strengthened into Tropical Storm Katrina over the Central Bahamas, and a hurricane warning was issued for the Southeastern Florida coast. Katrina passed Miami as a weak hurricane, rating as only a category 1 hurricane on a scale from 1 to 5. But within days, warnings from forecasters warmed that the worst might be yet to come. The storm sucked energy from warm Gulf of Mexico waters as it moved west, swelling into a category 5 monster and then weakening only slightly before it slammed into the Mississippi shore as a category 4 hurricane. Abundant rain and a surge of ocean water overwhelmed flood-control measures and broke levees at nearby Lake Pontchartrain, deluging New Orleans with up to 20 feet of water and plunging the city into mayhem. Katrina pushed the death toll in New Orleans alone as much as "Minimum, hundreds. Most likely, thousands1" and caused the economic loss with subsequent flooding in New Orleans expected to exceed $100 billion2, breaking the records of Hurricane Andrew in 1992. In the remainder of the season, the US was also hit by hurricanes Rita, and Wilma, the most intense hurricane ever recorded. In the meantime, further south, hurricane Stan created havoc in Central America. After Wilma, there were no names left for the next tropical storm, which became alpha, shortly followed by hurricane beta, which made landfall on the coast of Nicaragua. With another month remaining, the 2005 hurricane season had already set new records for the most named storms and hurricanes in a single year. The year before, 2004, had been very intense as well, with the second largest annual damages (after 2005). And these two subsequent harsh seasons seem to fit a trend: the frequency and particularly intensity of tropical cyclones in the Atlantic has been on the rise since 1995. II. Scientific debate: a link to climate change? Triggered by the devastation caused by Katrina, but also in the light of the harsh 2004 and 2005 hurricane seasons, many people have been asking whether these hurricanes arose by mere chance or whether something more long lasting might be at play—global warming/ climate change. The scientific debate on these linkages is currently ongoing. All scientists agree that the main cause of the upswing in hurricanes is a natural, cyclic phenomenon that affects ocean currents and atmospheric temperature, which yields decade-to-decade swings in total hurricane numbers that have nothing to do with global warming. 1 According to New Orleans Mayor Ray Nagin 2 Risk Management Solutions, a US firm. 1 In a recent study in Nature3, Kerry Emanuel of the Massachusetts Institute of Technology found an increase in the duration and power of hurricanes in the North Atlantic and North Pacific. Another scientific study in the September 16 issue of Science4 notes that the number of large hurricanes appears to have increased since 1970, while smaller hurricanes have become less common. Co-author Greg Holland of the National Center for Atmospheric Research comments: "What we've done is show that there's actually an increase in the number of intense storms”. To count the hurricanes world-wide in each category of storm intensity, Holland and his colleagues used satellite data collected by scientists since about 1970. They found that the number of storms in categories 4 and 5 doubled during the past 35 years, while storms in categories 1 to 3 dropped off. Overall, he says, the larger storms now occur 20 to 35 percent more often than smaller storms do. Peter Webster, a coauthor of the report, says, "The intensity of Katrina is consistent with the type of storms we've been finding, [which are] increasing in intensity globally." Some of these climate scientists are also pointing to global warming as a culprit for at least part of the increasingly ferocious hurricanes worldwide. Both scientific theory and computer modeling predict that as human activities heat the atmosphere, warmer sea- surface temperatures will fuel hurricanes, increasing wind speeds and rainfall. In a paper in Science on 17th June5 2005, Kevin Trenberth, Head of the Climate Analysis Section at the National Centre for Atmospheric Research6 explains that the observational hurricane record reveals large natural variability from El Niño and on multi-decadal time scales, and that any additional trends due to climate change would be relatively small. However, he also points out that we do know that sea surface temperatures are rising and atmospheric water vapour is increasing. These factors are potentially enhancing tropical convection, including thunderstorms, and the development of tropical storms. Over the coming decades, these changes are expected to increase hurricane intensity and rainfall. At the same time however, the effect on hurricane numbers and tracks remains unclear: "there is no sound theoretical basis for drawing any conclusions about how anthropogenic change affects hurricane numbers or tracks, and thus how many hit land." III. The response Regardless of the scientific debate on the involvement of global warming in the current hurricane season and hurricane Katrina, there is a very important underlying issue: our vulnerability is rising dramatically. "[Katrina] should be a wake-up call for us to carefully look at our vulnerabilities," says Roger Pielke of the University of Colorado at Boulder, "Global warming is an important topic—I definitely think we should be responding to it— but we shouldn't confuse our responses to global warming with disaster mitigation." In fact, this is a key message for all extreme events (including floods, droughts, and heat waves, which are already becoming more frequent due to global climate change): we need to address the rising risks not only by mitigating climate change, but also by better 3 Emanuel, K (2005), Increasing destructiveness of tropical cyclones over the past 30 years, Nature, 436, 686- 688. 4 Webster, P.J., G. J. Holland, J.A. Curry, and H.-R. Chang (2005), Changes in Tropical Cyclone Number, Duration and Intensity in a Warming Environment, Science, 309, 1844-1846. 5 Trenberth K. (2005), Uncertainty in Hurricanes and Global Warming, Science, 308, 1753-1754. 2 disaster risk reduction. Increasing disaster preparedness and integrating disaster risk reduction into development planning are crucial to mitigate the impacts of hurricanes like Katrina, and reduce the massive losses and human suffering we’ve seen in the 2005 hurricane season. 3.
Recommended publications
  • Central America: Hurricane Stan "Tropical Storm "Stan" Turned Into a Hurricane (Category OCHA Situation Report No
    Central America: Hurricane Stan "Tropical storm "Stan" turned into a hurricane (Category OCHA Situation Report No. 2 One, Saffir-Simpson scale) on 4 October 2005 and is Issued 7 October 2005 affecting Mexico and Central America." GLIDE: TC-2005-000173-SLV International Boundary SITUATION Neighouring Country Floods and landslides: Affected Country Heavy rains caused flooding, deadly mud- and rockslides. National Capital People evacuated to shelters or relatives', friends' houses. Wind (mph) 50-100 Damage to crops. Roads in main cities closed due to 25-50 Gulf of Mexico landslides. Rains expected in the next 48 hours. Volcanic activity: Largest volcano in El Salvador, Ilamatepec, erupted on 1st and 3rd Oct., emitting gases, smoke and ash. 13 tremors registered in last 3 days. Potential mudflows. 3 Oct 4 Oct ACTION Government announced USD 11.7 million to cover the emergency requirements and is negotiating the reorientation 2 Oct of USD 43 million loan. Mexico 1 Oct Following the request of the Government, UN-OCHA released USD 30,000 from its Emergency Grant Reserve and USD 30,000 from the Norwegian Grant Reserve in MMEEXXIICCOO 5 Oct OCHA Trust Fund for Disaster Relief. Joint UN Inter-agency appeal of USD 7,895,913 issued. E Z El I Salvador 49L killed Geog raph ic Co ord in ate System s: WG S 19 84. E Ma p data so urce: U N Ca rtographic Se ction, UNISYS. 32B ,045 evacuated 309 shelters Cod e: OC HA/GVA - 200 5/015 1 66,320 population at risk from mudslides (13,543 rural, 288 urban families) GGUUAATTEEMMAALLAA 94,165 population at risk from flooding (13,438 rural, 5,395 urban families) Guatemala HONDURAS EELL S SAALL V VAADDOORR PACIFIC OCEAN Ilamatepec volcano San Salvador NICARAGUA 5 killed 4,000 evacuated 0 100 200 300 400 Km Created by the ReliefWeb Map Centre Office for the Coordination of H um anitarian Affairs The names shown and the designations used on this map do not imply official endorsement or acceptance by the United Nations.
    [Show full text]
  • Floods from Hurricane Stan; Appeal No
    CENTRAL AMERICA, MEXICO AND HAITI: FLOODS FROM 23 December 2005 HURRICANE STAN The Federation’s mission is to improve the lives of vulnerable people by mobilizing the power of humanity. It is the world’s largest humanitarian organization and its millions of volunteers are active in over 181 countries. In Brief Appeal No. 05EA021; Operations Update no. 03; Period covered: 17 October to 23 December, 2005; Appeal coverage: 79.2%. Click here to go directly to the attached Contributions List, also available on the website). Appeal history: • Launched on 7 October 2005 CHF 1,568,000 (USD 1,230,694 OR EUR 1,012,648) for 6 months to assist 10,250 families (51,250 beneficiaries). • A revised Emergency Appeal was issued on 17 October 2005, seeking CHF 6,175,760 (USD 4,780,996 or EUR 3,974,564) in cash, kind, or services to assist 10,050 families (50,250 beneficiaries) for 6 months. • Disaster Relief Emergency Funds (DREF) allocated: CHF 280,000 Outstanding needs: CHF 1,285,365 (USD 979,736 or EUR 825,457) Related Emergency or Annual Appeals: El Salvador: Floods and Volcanic Activity (Appeal 05EA020); Haiti: Floods (Appeal 22/2004); Bahamas, Cuba and Mexico: Hurricane Wilma (Appeal 05EA024); Central America: Annual Appeal (Appeal 05AA043); Pan American Disaster Response Unit: Annual Appeal (Appeal 05AA040) Operational Summary: Since the onset of the disaster, Costa Rican, Guatemalan, Honduran, Mexican, Nicaraguan and Haitian Red Cross Societies have been working untiringly to respond to the needs of the most affected families. Although many families have now been able to return to their homes, many of those affected remain in shelters or are staying in the homes of friends or relatives.
    [Show full text]
  • ANNUAL SUMMARY Atlantic Hurricane Season of 2005
    MARCH 2008 ANNUAL SUMMARY 1109 ANNUAL SUMMARY Atlantic Hurricane Season of 2005 JOHN L. BEVEN II, LIXION A. AVILA,ERIC S. BLAKE,DANIEL P. BROWN,JAMES L. FRANKLIN, RICHARD D. KNABB,RICHARD J. PASCH,JAMIE R. RHOME, AND STACY R. STEWART Tropical Prediction Center, NOAA/NWS/National Hurricane Center, Miami, Florida (Manuscript received 2 November 2006, in final form 30 April 2007) ABSTRACT The 2005 Atlantic hurricane season was the most active of record. Twenty-eight storms occurred, includ- ing 27 tropical storms and one subtropical storm. Fifteen of the storms became hurricanes, and seven of these became major hurricanes. Additionally, there were two tropical depressions and one subtropical depression. Numerous records for single-season activity were set, including most storms, most hurricanes, and highest accumulated cyclone energy index. Five hurricanes and two tropical storms made landfall in the United States, including four major hurricanes. Eight other cyclones made landfall elsewhere in the basin, and five systems that did not make landfall nonetheless impacted land areas. The 2005 storms directly caused nearly 1700 deaths. This includes approximately 1500 in the United States from Hurricane Katrina— the deadliest U.S. hurricane since 1928. The storms also caused well over $100 billion in damages in the United States alone, making 2005 the costliest hurricane season of record. 1. Introduction intervals for all tropical and subtropical cyclones with intensities of 34 kt or greater; Bell et al. 2000), the 2005 By almost all standards of measure, the 2005 Atlantic season had a record value of about 256% of the long- hurricane season was the most active of record.
    [Show full text]
  • Syndromes of Sustainability of Development for Assessing the Vulnerability of Coupled Human–Environmental Systems
    ARTICLE IN PRESS Global Environmental Change 17 (2007) 207–217 www.elsevier.com/locate/gloenvcha Syndromes of sustainability of development for assessing the vulnerability of coupled human–environmental systems. The case of hydrometeorological disasters in Central America and the Caribbean David Manuel-NavarreteÃ, Jose´Javier Go´mez, Gilberto Gallopı´n Division of Sustainable Development and Human Settlements, Economic Commission for Latin America and the Caribbean, Casilla 179-D, Santiago de Chile, Chile Received 27 March 2006; received in revised form 4 July 2006; accepted 18 July 2006 Abstract Syndrome analysis seeks to capture socio-ecological dynamics of interaction by addressing clusters of symptoms rather than isolated variables. This paper identifies the main symptoms of vulnerability to hydrometeorological disasters in Central America and the Caribbean by building on the results of 14 postdisaster assessments. A syndrome representation for this region is proposed, including 13 symptoms and their causal interrelations. These symptoms are manifested in the spheres of biology, hydrology, soil, population, economy, social organization, and knowledge. The linkages of this syndrome representation to other syndromes, its degree of generality across places, and its causal loops are analyzed and discussed. Three vicious circles increasing vulnerability to hydrometeorological disasters in the region are identified. Two of them point to the importance of breaking urbanization cycles marked by the absence of effective land-use planning which lead to the occupation of hazardous areas by poor people. The third causal loop goes far beyond the urban context and establishes ecosystem degradation and conversion as its main driving force. This latter vicious circle supports the notion that vulnerability should be understood in the context of human–environmental interactions.
    [Show full text]
  • Natural Disasters in Latin America and the Caribbean
    NATURAL DISASTERS IN LATIN AMERICA AND THE CARIBBEAN 2000 - 2019 1 Latin America and the Caribbean (LAC) is the second most disaster-prone region in the world 152 million affected by 1,205 disasters (2000-2019)* Floods are the most common disaster in the region. Brazil ranks among the 15 548 On 12 occasions since 2000, floods in the region have caused more than FLOODS S1 in total damages. An average of 17 23 C 5 (2000-2019). The 2017 hurricane season is the thir ecord in terms of number of disasters and countries affected as well as the magnitude of damage. 330 In 2019, Hurricane Dorian became the str A on STORMS record to directly impact a landmass. 25 per cent of earthquakes magnitude 8.0 or higher hav S America Since 2000, there have been 20 -70 thquakes 75 in the region The 2010 Haiti earthquake ranks among the top 10 EARTHQUAKES earthquak ory. Drought is the disaster which affects the highest number of people in the region. Crop yield reductions of 50-75 per cent in central and eastern Guatemala, southern Honduras, eastern El Salvador and parts of Nicaragua. 74 In these countries (known as the Dry Corridor), 8 10 in the DROUGHTS communities most affected by drought resort to crisis coping mechanisms. 66 50 38 24 EXTREME VOLCANIC LANDSLIDES TEMPERATURE EVENTS WILDFIRES * All data on number of occurrences of natural disasters, people affected, injuries and total damages are from CRED ME-DAT, unless otherwise specified. 2 Cyclical Nature of Disasters Although many hazards are cyclical in nature, the hazards most likely to trigger a major humanitarian response in the region are sudden onset hazards such as earthquakes, hurricanes and flash floods.
    [Show full text]
  • MASARYK UNIVERSITY BRNO Diploma Thesis
    MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.
    [Show full text]
  • Spring 2006 (PDF)
    SKYWARNEWS National Weather Service State College, PA - Spring 2006 “Working Together To Save Lives” New Radar Displays on mosaics are available from the dark blue left-hand menu common to all of our the Webpage! pages. The mosaics are a really nice By Michael Dangelo, NWS CTP feature, as the radar echoes from all the Webmaster radars in a wide area are combined into one picture. The regional mosaics cover Many of you have been to our website about a dozen states each, and the (http://weather.gov/statecollege), and national one covers the lower 48 states. lots of you have mentioned the new These mosaic images can also be radar displays. Thank you for all of your looped! There are even two different comments and suggestions. I will pass sizes/resolutions of the national mosaic them along to the headquarters folks and loops. who create those displays. There is both an “Enhanced” version of There are many new features available, the individual radar displays, and a and I thought I could highlight some of “Standard” version of the displays. The them. Enhanced displays are for those with high-bandwidth internet connections “KCCX” is the identifier for the Central (cable/DSL), while the Standard displays PA WSR-88D Radar. KCCX is located are better for low-bandwidth (dial-up) in northern Centre County near Black users. Moshannon State Park, and operated and maintained by the staff at WFO CTP. The Enhanced display allows you to See our “All Local Radars” page toggle on and off some useful overlays (http://www.erh.noaa.gov/ctp/radar.php) of local warnings, a topographic for more info on the 88D and some background image, a legend, and various pictures of the site (from a tour that was maps.
    [Show full text]
  • Hurricane Stan 1-5 October 2005
    Tropical Cyclone Report Hurricane Stan 1-5 October 2005 Richard J. Pasch and David P. Roberts National Hurricane Center 14 February 2006 Stan was associated with disastrous inland flooding across portions of Central America and Mexico, and some estimates of the death toll are as high as 2000. However, not all of these deaths can be directly attributed to Stan. a. Synoptic History A tropical wave that moved off the coast of Africa on 17 September was the likely precursor to Stan. This wave showed little distinction as it moved over the eastern and central tropical Atlantic for several days. Cloudiness and showers associated with the system began to increase the wave neared 50°W longitude on 22 September, but north-northeasterly shear created an environment that was not favorable for tropical cyclone formation. The wave moved into the eastern Caribbean Sea on 25 September, while shear over the system diminished. By 27 September, deep convection associated with the wave became more consolidated over the central Caribbean Sea. Over the next several days, organization of the system waxed and waned as it moved into the western Caribbean Sea. It was not until early on 1 October, when the system neared the eastern coast of the Yucatan peninsula, that development began in earnest. Based on the extent and organization of deep convection as well as surface observations, it is estimated that a tropical depression formed around 1200 UTC 1 October centered about 115 n mi southeast of Cozumel. Figure 1 is a “best track” chart of the tropical cyclone’s path.
    [Show full text]
  • Hurricane Stan "Affected Areas Include the Coast of the Gulf of Mexico, OCHA Situation Report No
    Mexico: Hurricane Stan "Affected areas include the coast of the Gulf of Mexico, OCHA Situation Report No. 1 particularly the South of Veracruz as well... the Central-South Issued 11 October 2005 part of the country." GLIDE: TC-2005-000173-SLV Saltillo SITUATION Gulf of Mexico Hurricane Stan caused floods in Mexico, damaging crops, roads and communication infrastructure, leaving some areas VERACRUZ Ciudad Victoria Cazones isolated. 150 evacuated Emiliano Zapata ACTION Partially isolated Zacatecas Medellín National System of Civil Protection, DN-3 emergency plan, Shelter set up State departments and local civil protection organizations Assistance provided Tampico responding to the emergency. San Luis Potosi Saltabarranca Aguascalientes Estanzuela Warehouse to store water and food supplies established in 448 families affected Chiapas; Secretariat of Health has also opened a Estanzuela Texistepec Two shelters set up warehouse. 3 Oct Merida Guanajuato V Cazones Government has not requested international support though Queretaro E R HIDALGO A 4 Oct several offers have been made. C Pachuca R U Emiliano Zapata Z Geog raph ic Co ord in ate System s: WG S 19 84. Jalapa Campeche Ma p data so urce: U N Ca rtographic Se ction, Arcworld, UNISYS, Ciesin, GN S. Morelia Mexico Cod e: OC HA/GVA - 200 5/016 1 Toluca Tlaxcala Rinconada Veracruz MEXICO Medellin MEXICO Puebla International Boundary Cuernavaca Xoxocotla Huitzila Tlalixcoyan Atlahuilco Saltabarranca Neighouring Country PUEBLA Affected Country Villahermosa Chilpancingo Affected State De Los Bravo
    [Show full text]
  • What Is Really Responsible for the Extreme Waves Regime in the Colombian Caribbean Coastal Region?
    Nat. Hazards Earth Syst. Sci., 16, 391–401, 2016 www.nat-hazards-earth-syst-sci.net/16/391/2016/ doi:10.5194/nhess-16-391-2016 © Author(s) 2016. CC Attribution 3.0 License. Storms or cold fronts: what is really responsible for the extreme waves regime in the Colombian Caribbean coastal region? L. J. Otero, J. C. Ortiz-Royero, J. K. Ruiz-Merchan, A. E. Higgins, and S. A. Henriquez Applied Physics Group – Ocean and Atmosphere Area – Physics Department, Universidad del Norte, Barranquilla, Colombia Correspondence to: L. J. Otero ([email protected]) Received: 9 April 2015 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 4 May 2015 Revised: 28 December 2015 – Accepted: 4 January 2016 – Published: 8 February 2016 Abstract. The aim of this study is to determine the contri- that in the continental area due to their geographic location. bution and importance of cold fronts and storms to extreme The wave heights in the extreme regime are similar in mag- waves in different areas of the Colombian Caribbean in an nitude to those found in Alta Guajira, but the extreme waves attempt to determine the extent of the threat posed by the associated with the passage of cold fronts in this region have flood processes to which these coastal populations are ex- lower return periods than those associated with the hurricane posed. Furthermore, the study wishes to establish the actions season. to which coastal engineering constructions should be sub- ject. In the calculation of maritime constructions, the most important parameter is the height of the wave. For this rea- son, it is necessary to establish the design wave height to which a coastal engineering structure should be resistant.
    [Show full text]
  • The Impact of Hurricane Beta on the Forests Of
    http://www.icn.unal.edu.co/ Caldasia 32(2):425-434.Ruiz & Fandiño 2010 THE IMPACT OF HURRICANE BETA ON THE FORESTS OF PROVIDENCIA ISLAND, COLOMBIA, SOUTHWEST CARIBBEAN El impacto del huracán Beta en los bosques de la isla Providencia, Colombia, Suroccidente caribeño JORGE RUIZ Escuela de Ciencias Sociales; Convenio Uptc-IGAC. Universidad Pedagógica y Tecnológica de Colombia (Uptc). Bogotá, D.C. Colombia. [email protected] MARÍA C. FANDIÑO Patrimonio Natural Fondo para la Biodiversidad y Áreas Protegidas, Programa Incentivos a la Conservación. Bogotá, D.C. Colombia. [email protected] ABSTRACT One of the consequences of global warming in the Caribbean is an increase in the frequency and intensity of hurricanes. Little is known on the impact of this natural phenomenon on forests, particularly for dry tropical forests. Understanding this impact in terms of structure and species richness is important for forest management. Slow moving Hurricane Beta, a category 1, struck Old Providence island, Colombia, in October 29, 2005. Before Beta woody vegetation was characterized by 88 2 x 50 m plots (0.01 ha) established throughout the island following the protocol by Gentry (1982); 59 plots were studied fi ve years earlier and 29 plots four to fi ve months earlier. The impact of hurricane Beta was assessed within 11 plots located in the Dry Tropical Forests of Old Providence, six months after the hurricane. The These plots were measured in species composition, diameter at breast height (DBH), and height were measured within these plots. There was a considerable reduction in the number of individuals, stems, height, basal areas, and there was no signifi cant difference between DBH.
    [Show full text]
  • The Story of a Hurricane: Local Government, Ngos, and Post‐Disaster Assistance
    CDEP‐CGEG WORKING PAPER SERIES CDEP‐CGEG WP No. 86 The Story of a Hurricane: Local Government, NGOs, and Post‐Disaster Assistance Ben Fitch‐Fleischmann and Evan Plous Kresch June 2020 The Story of a Hurricane: Local Government, NGOs, and Post-Disaster Assistance∗ Ben Fitch-Fleischmann Evan Plous Kresch Abstract After catastrophes, international donors offering assistance must decide whether to channel their resources via the local government or non-governmental organizations (NGOs). We examine how these channels differ in the timing, locations, and popula- tions that they assist by combining data on aid received by Nicaraguan households over ten years with municipal election results and an exogenous measure of a catastrophe (Hurricane Mitch). In the short term (0-3 years post), NGOs provided aid accord- ing to hurricane severity with no evidence of political influence, while government aid allocations were unrelated to hurricane severity. Instead, the evidence suggests that short-term government aid was distributed along political lines, though in a nuanced way. The catastrophe also had long-term effects on aid, with households in the disaster area receiving significantly more aid than households in other areas|from both NGOs and the government|in the period 3 to 7 years after the hurricane. Keywords: development aid, non-governmental organizations, climate change, hurricane, Nicaragua JEL classification: Q01, Q54, O12 ∗Fitch-Fleischmann is an energy supply planning manager at NorthWestern Energy; Kresch is an assistant professor of Economics at Oberlin College. Corresponding author: Kresch ([email protected]). We are grateful to Alfredo Burlando, Trudy Cameron, Amy Damon, and Glen Waddell for helpful comments.
    [Show full text]