Hurricane Harvey's Aftermath

Author(s):  
Kevin M. Fitzpatrick ◽  
Matthew L. Spialek

Early June begins the Southern Hemisphere hurricane season. Stretching into November, it can often be a time of weary waiting and cautious optimism for coastal residents. Clear skies and calm seas can quickly give way to disaster. On August 27, 2017, a Category 4 hurricane (Harvey), targeting the Texas Gulf Coast and packing winds of over 130 miles per hour, wreaked havoc and created a path of destruction with bands of rain that seemingly went on forever. Lives were lost, neighborhoods devastated, resiliency cracked; yet people continued helping each other, and the recovery process began. Fitzpatrick and Spialek tell a complicated story of heartache, destruction, resiliency, recovery, and hope. Through over 300 interviews from Hurricane Harvey survivors living along the Texas Gulf Coast, their stories tell an all-too-familiar tale. Interviewing survivors with diverse displacement experiences, the authors create a narrative around who, what, where, and why residents sought refuge in shelters, hotels, and other alternative locations. Some residents have since moved back. Others have been rebuilding for months and even years. And there are some residents who will never return home. Their stories, circumstances, and insight into the recovery processes are all very different, yet intimately tied together through an understanding of how race and place come to define their experiences. This book tells survivors’ stories while emphasizing that who those survivors were and where they lived had a major impact on these tales of destruction, resiliency, and recovery.

2014 ◽  
Vol 2014 ◽  
pp. 1-7 ◽  
Author(s):  
W. James Grichar ◽  
Stephen P. Biles

Soybeans (Glycine maxL.) can be planted along the upper Texas Gulf Coast from mid-March through May to take advantage of early season rains and to complete harvest before hurricane season and fall rains become a problem. However, in the Calhoun County area (28.5° north latitude), these planting dates have resulted in below average yields and reasons for these yield reductions are not clear. To determine if earlier planting dates could be an option to eliminate the low yields, field studies were conducted from 2005 through 2010 in Calhoun County, Texas, to determine soybean cultivar response to planting dates which ranged from mid-February through the last of April. Typically, soil temperatures in this area are above 18°C in mid-February and depending on weather patterns may not fall much lower during any time in the early portion of the growing season. The greatest yield was obtained with the mid-February and mid-March planting dates compared with early- or late-April planting dates. Typically, as planting date was delayed, the interval between planting and harvest decreased.


2011 ◽  
Vol 2011 ◽  
pp. 1-14 ◽  
Author(s):  
W. J. Grichar ◽  
S. Biles ◽  
J. D. Janak ◽  
P. McGuill

Soybeans (Glycine max) can be planted along the upper Texas Gulf Coast from mid-March through May to take advantage of early season rains and to complete harvest before hurricane season and fall rains become a problem. When average to above average rainfall was received in May through July, yields were greater with the early April to mid-April planting; however, under high rainfall conditions throughout the season, the mid-April to early May planting produced the highest yields, with yields of over 4000 kg/ha. When rainfall was below normal, late March to early April plantings produced the greatest yields. When rainfall was above average, soybeans took longer to reach harvestability regardless of cultivar or plant dates, while under drought conditions the interval between planting and harvest was reduced. However, when planting was delayed, there was a greater risk of detrimental late-season effects from southern green stink bug (Nezara viridula) or the brown stink bug (Euschistus heros).


Author(s):  
Kevin M. Fitzpatrick ◽  
Matthew L. Spialek

Chapter one introduces how race and place intersect in such a way as to impact the response and recovery of residents living along the Texas Gulf Coast that were affected by Hurricane Harvey. Harvey was a special storm: it dumped rain like none other in the history of the continental United States, and was one of the costliest storms on record. Providing background and context to the storm, to the study, and to the overall framework of the book is the central focus of chapter one. In addition, the authors discuss the unique circumstances of 2017 as an unprecedented year of disasters for the US, and that uniqueness had specific ramifications for the coastal towns of southeastern Texas.


1994 ◽  
Vol 31 (6) ◽  
pp. 648-653 ◽  
Author(s):  
D. F. Cowan

The thymus glands of 10 bottlenose dolphins, Tursiops truncatus, collected along the Texas Gulf coast were examined using standard histologic and immunocytochemical methods. The thymus gland of Tursiops persists into adult life, represented by medulla and progressively thinning cortex. A network of epithelial cells, including Hassal bodies, is demonstrable using polyclonal anti-cytokeratin antibody. The network condenses, with loss of lymphoid cells as involution progresses. Cysts arise within the condensed network. These cysts, found in eight of 10 animals, increase in number and size with increasing body size. Body size tends to reflect age. Thymic cysts typically have an irregular shape when small but tend to become spherical as they enlarge. Theey may be lined by squamous epithelium of variable thickness. Eventually, the cysts become macroscopic and filled with a colloidlike material and may largely replace the thymus, which may be identified by noncystic remnants adjacent to the cysts.


2017 ◽  
Author(s):  
Hannah M. Horowitz ◽  
Daniel J. Jacob ◽  
Yanxu Zhang ◽  
Theodore S. Dibble ◽  
Franz Slemr ◽  
...  

Abstract. Mercury (Hg) is emitted to the atmosphere mainly as volatile elemental Hg0. Oxidation to water-soluble HgII controls Hg deposition to ecosystems. Here we implement a new mechanism for atmospheric Hg0 / HgII redox chemistry in the GEOS-Chem global model and examine the implications for the global atmospheric Hg budget and deposition patterns. Our simulation includes a new coupling of GEOS-Chem to an ocean general circulation model (MITgcm), enabling a global 3-D representation of atmosphere-ocean Hg0 / HgII cycling. We find that atomic bromine (Br) of marine organobromine origin is the main atmospheric Hg0 oxidant, and that second-stage HgBr oxidation is mainly by the NO2 and HO2 radicals. The resulting lifetime of tropospheric Hg0 against oxidation is 2.7 months, shorter than in previous models. Fast HgII atmospheric reduction must occur in order to match the ~ 6-month lifetime of Hg against deposition implied by the observed atmospheric variability of total gaseous mercury (TGM ≡ Hg0 + HgII(g)). We implement this reduction in GEOS-Chem as photolysis of aqueous-phase HgII-organic complexes in aerosols and clouds, resulting in a TGM lifetime of 5.2 months against deposition and matching both mean observed TGM and its variability. Model sensitivity analysis shows that the interhemispheric gradient of TGM, previously used to infer a longer Hg lifetime against deposition, is misleading because southern hemisphere Hg mainly originates from oceanic emissions rather than transport from the northern hemisphere. The model reproduces the observed seasonal TGM variation at northern mid-latitudes (maximum in February, minimum in September) driven by chemistry and oceanic evasion, but does not reproduce the lack of seasonality observed at southern hemisphere marine sites. Aircraft observations in the lowermost stratosphere show a strong TGM-ozone relationship indicative of fast Hg0 oxidation, but we show that this relationship provides only a weak test of Hg chemistry because it is also influenced by mixing. The model reproduces observed Hg wet deposition fluxes over North America, Europe, and China, including the maximum over the US Gulf Coast driven by HgBr oxidation by NO2 and HO2. Low Hg wet deposition observed over rural China is attributed to fast HgII reduction in the presence of high organic aerosol concentrations. We find that 80 % of global HgII deposition takes place over the oceans, reflecting the marine origin of Br and low concentrations of marine organics for HgII reduction, and most of HO2 and NO2 for second-stage HgBr oxidation.


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