Mitigating Impacts of Natural Hazards on Fishery Ecosystems

Abstract.—On 29 August 2005, Hurricane Katrina came ashore devastating coastal communities in the northern Gulf of Mexico. This paper examines the impacts of Hurricane Katrina on two fishing communities in Louisiana: Grand Isle and the Empire- Venice area. Both of these areas were heavily involved in the commercial fishing industry before the hurricane hit. Empire-Venice is one of the top commercial fishing ports by volume of landings in the country. As the storm crossed the wetlands south of New Orleans, boats were sunk, houses and businesses were destroyed, and lives were changed, in some cases, perhaps, forever.

2015 ◽  
Vol 45 (12) ◽  
pp. 3137-3154 ◽  
Author(s):  
Zhao Jing ◽  
Ping Chang ◽  
Steven F. DiMarco ◽  
Lixin Wu

AbstractMoored ADCP data collected in the northern Gulf of Mexico are analyzed to examine near-inertial internal waves and their contribution to subthermocline diapycnal mixing based on a finescale parameterization of deep ocean mixing. The focus of the study is on the impact of near-inertial internal waves generated by an extreme weather event—that is, Hurricane Katrina—and by month-to-month variation in weather patterns on the diapycnal mixing. The inferred subthermocline diapycnal mixing exhibits pronounced elevation in the wake of Katrina. Both the increased near-inertial (0.8–1.8f, where f is the Coriolis frequency) and superinertial (>1.8f) shear variances contribute to the elevated diapycnal mixing, but the former plays a more dominant role. The intense wind work on near-inertial motions by the hurricane is largely responsible for the energetic near-inertial shear variance. Energy transfer from near-inertial to superinertial internal waves, however, appears to play an important role in elevating the superinertial shear variance. The inferred subthermocline diapycnal mixing in the region also exhibits significant month-to-month variation with the estimated diffusivity in January 2006 about 3 times the values in November and December 2005. The subseasonal change in the diapycnal mixing mainly results from the subseasonal variation of the near-inertial wind work that causes intensification of the near-inertial shear in January 2006.


2019 ◽  
Vol 10 (4) ◽  
pp. 478-492 ◽  
Author(s):  
Claire McConnell ◽  
Chiara Bertolin

AbstractThe increasing risk and exposure of people and assets to natural hazards and disasters suggests an increasing need for temporary housing following disasters. Resilience to natural hazards is dependent on the resources available to families or communities to prepare for and mitigate risk, influenced by social vulnerability. This study seeks to quantify the total environmental impact of temporary housing deployment in New Orleans, using the catastrophic impact of Hurricane Katrina in southern Louisiana in August 2005 as a case example. We employ a novel approach to estimate displacement period and take into account social vulnerability across New Orleans neighborhoods to better understand the scale of post-disaster relief and its global warming potential. The methodology implemented in this study comprises three steps: a risk assessment, a life cycle assessment, and a resulting total impact assessment. We demonstrate the considerable risk of greenhouse gas emissions and energy impacts from temporary housing deployment linked to hurricane hazard. Furthermore, we show that environmental impact is highly sensitive to displacement period and find the current methodology of anticipating temporary housing use by hazard alone to be inadequate. Additionally, the approach presented in this article provides tools to politicians and disaster risk professionals that allow for resource investment planning to decrease social vulnerability, thus enhancing resilience and adaptive capacity in a more homogeneous way at the urban scale.


2008 ◽  
Vol 14 ◽  
pp. 287-294 ◽  
Author(s):  
M. H. Glantz

Abstract. By American standards, New Orleans is a very old, very popular city in the southern part of the United States. It is located in Louisiana at the mouth of the Mississippi River, a river which drains about 40% of the Continental United States, making New Orleans a major port city. It is also located in an area of major oil reserves onshore, as well as offshore, in the Gulf of Mexico. Most people know New Orleans as a tourist hotspot; especially well-known is the Mardi Gras season at the beginning of Lent. People refer to the city as the "Big Easy". A recent biography of the city refers to it as the place where the emergence of modern tourism began. A multicultural city with a heavy French influence, it was part of the Louisiana Purchase from France in early 1803, when the United States bought it, doubling the size of the United States at that time. Today, in the year 2007, New Orleans is now known for the devastating impacts it withstood during the onslaught of Hurricane Katrina in late August 2005. Eighty percent of the city was submerged under flood waters. Almost two years have passed, and many individuals and government agencies are still coping with the hurricane's consequences. And insurance companies have been withdrawing their coverage for the region. The 2005 hurricane season set a record, in the sense that there were 28 named storms that calendar year. For the first time in hurricane forecast history, hurricane forecasters had to resort to the use of Greek letters to name tropical storms in the Atlantic and Gulf (Fig.~1). Hurricane Katrina was a Category 5 hurricane when it was in the middle of the Gulf of Mexico, after having passed across southern Florida. At landfall, Katrina's winds decreased in speed and it was relabeled as a Category 4. It devolved into a Category 3 hurricane as it passed inland when it did most of its damage. Large expanses of the city were inundated, many parts under water on the order of 20 feet or so. The Ninth Ward, heavily populated by African Americans, was the site of major destruction, along with several locations along the Gulf coasts of the states of Mississippi and Alabama, as well as other parts of Louisiana coastal areas (Brinkley, 2006). The number of deaths officially attributed to Hurricane Katrina was on the order of 1800 to 2000 people. The cost of the hurricane in terms of physical damage has been estimated at about US $250 billion, the costliest natural disaster in American history. It far surpassed the cost of Hurricane Andrew in 1992, the impacts of which were estimated to be about $20 billion. It also surpassed the drought in the US Midwest in 1988, which was estimated to have cost the country $40 billion, but no lives were lost. Some people have referred to Katrina as a "superstorm". It was truly a superstorm in terms of the damage it caused and the havoc it caused long after the hurricane's winds and rains had subsided. The effects of Katrina are sure to be remembered for generations to come, as were the societal and environmental impacts of the severe droughts and Dust Bowl days of the 1930s in the US Great Plains. It is highly likely that the metropolitan area of New Orleans which people had come to know in the last half of the 20th century will no longer exist, and a new city will likely replace it (one with a different culture). Given the likelihood of sea level rise on the order of tens of centimeters associated with the human-induced global warming of the atmosphere, many people wonder whether New Orleans will be able to survive throughout the 21st century without being plagued by several more tropical storms (Gill, 2005). Some (e.g., Speaker of the US House of Representatives Hastert) have even questioned whether the city should be restored in light of the potential impacts of global warming and the city's geographic vulnerability to tropical storms.


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