The assessment of standardized training programs in public health preparedness

The Texas Bioterrorism Continuing Education Consortium (BCE) provided National Disaster Life Support (NDLS) training courses throughout the state of Texas in 2005, to help improve knowledge and skills pertaining to bioterrorism and other public health emergencies. The NDLS training courses include curriculum in Basic Disaster Life Support (BDLS) and Core Disaster Life Support (CDLS). A course evaluation which included items assessing ability and willingness of training participants, role of responders, and other variables was mailed to all NDLS participants who provided contact information. An analysis was conducted to determine whether the survey respondents participated in the Hurricanes Katrina and/or Rita relief efforts, as well as to evaluate the impact of the NDLS training courses on the participant's ability and willingness to respond during a disaster. The study population (n = 2150) consisted mostly of nurses (50%) (n=1074). A chi-square test of analysis indicated the following results. Among the survey respondents who took the CDLS course, there was no statically significant difference by occupation pertaining to ability or willingness to respond (x2 [df = 5] = 4.02, p= 0.546); (x2 [df = 5] = 2.45, p = .783). However, there was a statistically significant difference among those respondents who took the BDLS course with respect to ability, and a slightly significant difference with respect to willingness (x2 [df = 5] = 13.35, p = .020 and (x2 = [df = 5] = 10.299, p = .067). These findings are similar to previous studies assessing willingness to respond to a disaster.^ A second analysis was conducted with these survey data to evaluate the implications for disaster response training for the NDLS courses. Results indicated that the majority of disaster responders served in the role for which they were professionally trained (Physicians=68%; Nurses = 50.4%). Nurses, EMT, and Fire professionals served in multiple roles. These results suggest the importance of developing training programs that will prepare professionals to serve in multiple roles. The development of standardized evaluation methods would fill an important gap in assessing impact of national training programs. ^

Electron spin resonance (ESR) and 14C dating in sediments of Bonaire, Leeward Antilles

The coastal deposits of Bonaire, Leeward Antilles, are among the most studied archives for extreme-wave events (EWEs) in the Caribbean. Here we present more than 400 electron spin resonance (ESR) and radiocarbon data on coarse-clast deposits from Bonaire's eastern and western coasts. The chronological data are compared to the occurrence and age of fine-grained extreme-wave deposits detected in lagoons and floodplains. Both approaches are aimed at the identification of EWEs, the differentiation between extraordinary storms and tsunamis, improving reconstructions of the coastal evolution, and establishing a geochronological framework for the events. Although the combination of different methods and archives contributes to a better understanding of the interplay of coastal and archive-related processes, insufficient separation, superimposition or burying of coarse-clast deposits and restricted dating accuracy limit the use of both fine-grained and coarse-clast geoarchives to unravel decadal- to centennial-scale events. At several locations, distinct landforms are attributed to different coastal flooding events interpreted to be of tsunamigenic origin. Coastal landforms on the western coast have significantly been influenced by (sub)-recent hurricanes, indicating that formation of the coarse-clast deposits on the eastern coast is likely to be related to past events of higher energy.

Monthly Bonaire coral Sr/Ca and oxygen isotope data from 118 kyr ago (coral BON-5-D)

The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and d18O records. We find that temperature seasonality was similar to today, which is consistent with the orbital insolation forcing. Our coral and climate model results suggest that temperature seasonality of the tropical surface ocean is controlled mainly by orbital insolation changes during interglacials.

Meteocean Influence on Inland and Coastal Floods in the East of Spain

The Santa Irene flood, at the end of October 1982, is one of the most dramatically and widely reported flood events in Spain. Its renown is mainly attributable to the collapse of the Tous dam, but its main message is to be the paradigm of the incidence of the maritime/littoral weather and its temporal sea-level rise on the coastal plains inland floods. The Santa Irene flood was attributable to a meteorological phenomenon known as gota fría (cold drop), a relatively frequent and intense rainy phenomenon on the Iberian Peninsula, particularly on the Spanish E to SE inlands and coasts. There are some circumstances that can easily come together to unleash the cold drop there: cold and dry polar air masses coming onto the whole Iberian Peninsula and the north of Africa, high sea-water temperatures, and low atmospheric pressure (cyclone) areas in the western Mediterranean basin; these circumstances are quite common during the autumn and, as it happens, in other places around the world (E/SE Africa). Their occurrence, however, shows a great space-temporal variability (in a similar way to hurricanes on Caribbean and western North Atlantic areas or also in a similar way to typhoons). In fact, all of these are equivalent, although different, phenomena, able to have a different magnitude each time. This paper describes the results of a detailed analysis and reflection about this cold drop phenomenon as a whole, on the generation of its rains, and on the different natures and consequences of its flood. This paper also explains the ways in which the nearby maritime weather and the consequential sea level govern floods on different zones of any hydrographical basin. The Santa Irene case can be considered as a paradigm to explain the influence of nearby maritime climatic conditions on flooding phenomena not only in coastal but also in upward inland areas.

Consideración de los huracanes en el diseño de las estructuras en la República Dominicana

La gestión de riesgo, es un mecanismo de protección, que mediante la identificación anticipada de las acciones generadas por un evento catastrófico, ayuda a reducir de la vulnerabilidad y a identificar las medidas a tomarse para evitar o mitigar los impactos de estos eventos o desastres. A sabiendas de que la seguridad absoluta no existe, surge la necesidad de que las construcciones de hoy día deben ser adaptadas en función de las características de su entorno y los peligros que se presentan en el mismo. La sociedad moderna identifica su exposición al riesgo y exige que estos sean tratados de manera adecuada garantizando que la obra no suponga ningún tipo de amenaza. Este Trabajo de Fin de Máster está guiado a la identificación de aquellas acciones e influencias que representan un peligro para las estructuras de la República Dominicana por el paso de los huracanes. Con esta información será posible la creación de un catálogo de Riesgos y Soluciones, cuya finalidad sea reducir la exposición y vulnerabilidad de las construcciones frente a un evento catastrófico como lo es paso de un huracán. Para realizar la investigación se ha utilizado el “Método LOGRO”, el cual trabaja bajo tres distintos métodos de investigación, los cuales son la: La revisión de documentación, una sesión de tormenta de ideas y encuestas a expertos (Método Delphi). Ya realizada la investigación e identificados los riesgos, se han realizado una serie de catálogos de Riesgos y Soluciones, que faciliten la creación de un plan de gestión de riesgos, para garantizar un diseño estructural resiliente, en las zonas expuestas al paso de los huracanes en la República Dominicana. Risk management is a protective mechanism, which by the early identification of actions generated by a catastrophic event, helps reduce vulnerability and to identify the measures taken to prevent or mitigate the impacts of these events or disasters. Knowing that there is no absolute security, there is the need for the construction of today must be adapted according to the characteristics of their environment and the dangers presented herein. Modern society identifies their exposure to risk and requires that these are adequately addressed by ensuring that the work does not pose any threat. This Final Project Master is guided to the identification of those actions and influences that pose a threat to the structures of the Dominican Republic by the hurricanes. With this information it is possible to create a catalog of risks, and solutions aimed at reducing the exposure and vulnerability of the buildings facing a catastrophic event as it is a hurricane. To make research has used the "LOGRO method", which works low three different research methods, which include: The review of documentation, a session of brainstorming and expert surveys (Delphi method). And conducted research and identified the risks, there have been a number of catalogs and Risk Solutions that facilitate the creation of a risk management plan to ensure a structural design resilient in areas prone to hurricanes in the Dominican Republic

Assessing climate impacts

Assessing climate impacts involves identifying sources and characteristics of climate variability, and mitigating potential negative impacts of that variability. Associated research focuses on climate driving mechanisms, biosphere–hydrosphere responses and mediation, and human responses. Examples of climate impacts come from 1998 flooding in the Yangtze River Basin and hurricanes in the Caribbean and Central America. Although we have limited understanding of the fundamental driving-response interactions associated with climate variability, increasingly powerful measurement and modeling techniques make assessing climate impacts a rapidly developing frontier of science.

Posthurricane survey of experimental dunes on Padre Island, Texas /

This report summarizes the impact of Hurricane Allen (August 1980) on dune configuration, sand accretion or erosion, and changes in the vegetation on north Padre Island. Four experimental foredunes, the result of grass plantings from 1969 to 1973, and an unplanted control section were monitored in 1975-1977 and also in 1981. The 1981 posthurricane data were compared where possilbe, with the previous studies. Foredune elevation surveys were completed in March 1981; accompanying vegetation transects were made in July 1981. Hurrican Allen causes erosion of the dune face of all the experimental dunes, but caused a breach in only one dune. The beach elevations had returned to approximately prehurricane heights by the time the area was resurveyed. The unplanted control dune provided little resistance to waves generated by the storm and a large quantity of sand was deposited inland.

The benthic fauna and sediments of the nearshore zone off Panama City Beach, Florida /

"August 1976."

Hurricane Gilbert storm surge data /

At head of title: Coastal Field Data Collection Program.

Hindcast hurricane swell for the coast of Southern California /

"November 1990."

Hurricane surge frequency estimated for the Gulf Coast of Texas /

"February 1969."

Storm surge on the open coast : fundamentals and simplified prediction /

"May 1971."

An analysis of drag coefficient at hurricane windspeeds from a numerical simulation of dynamical water level changes in Lake Okeechobee, Florida /

"October 1975."

Verification study of a bathystrophic storm surge model /

"May 1975."

The statistical anatomy of ocean wave spectra /

"July 1976."