ライフサイエンスコーパス: hurricane

1 ion results for the first 2 months after the hurricane.

2 Symptoms were reassessed 8 months after the hurricane.

3 ct externalizing symptoms 8 months after the hurricane.

4 n linked to eutrophication, overfishing, and hurricanes.

5 ific, warmer tropics and, in turn, even more hurricanes.

6 isting wetlands rendering them vulnerable to hurricanes.

7 ary to support intervals of frequent intense hurricanes.

8 in 2 months of the flooding induced by these hurricanes.

9 re as contributing to the intensification of hurricanes.

10 landfalling/near-coastal tropical storms and hurricanes.

11 ubject to more frequent extreme flooding and hurricanes.

12 sis and thermodynamic potential intensity of hurricanes.

13 ficantly more deaths than do masculine-named hurricanes.

14 upply favourable for the formation of strong hurricanes.

15 also exhibited stronger responses following hurricanes.

16 Six months after the hurricane, 158 adolescents from three differentially exp

17 who developed new-onset disorders after the hurricane, 18.5% received some form of treatment for emo

18 ental health services in the year before the hurricane, 22.9% experienced reduction in or termination

19 olis sagrei) was generally strong before the hurricane; 7 months after, the lizard effect on abundanc

20 By 19 months after the hurricane, A. sagrei populations occurred on 88% of the

21 y sample of adults 6-9 months after the 2004 hurricanes about hurricane exposure, social support, and

22 uencing a range of climate processes such as hurricane activity and African Sahel and Amazonian droug

23 t historical climate events such as peaks in hurricane activity and Sahel drought.

24 produces a realistic distribution of intense hurricane activity for present-day conditions.

25 ures, but work on the detection of trends in hurricane activity has focused mostly on their frequency

26 Atlantic hurricane activity has increased significantly since 199

27 erienced the highest level of North Atlantic hurricane activity in the reliable record.

28 Here we present a record of intense hurricane activity in the western North Atlantic Ocean o

29 ecadal time scale, the present high level of hurricane activity is likely to persist for an additiona

30 ons conducive to greater basin-wide Atlantic hurricane activity occur together with conditions for mo

31 dy the links between climatic conditions and hurricane activity on longer timescales, because they pr

32 , and documents a period of elevated intense hurricane activity on the western North Atlantic margin

33 A predicted increase in the frequency of hurricane activity over the next few decades may cause l

34 ble for approximately 40% of the increase in hurricane activity relative to the 1950-2000 average bet

35 te that the sensitivity of tropical Atlantic hurricane activity to August-September sea surface tempe

36 position on geologic timescales can modulate hurricane activity, but continuous and long-term storm r

37 enhouse gases contributed to the increase in hurricane activity, but the ability of climate models to

38 To accurately predict changes in intense hurricane activity, it is therefore important to underst

39 s climate index is associated with shifts in hurricane activity, rainfall patterns and intensity, and

40 that is known to strongly modulate Atlantic hurricane activity.

41 le projections of future changes in Atlantic hurricane activity.

42 cert to either enhance or inhibit basin-wide hurricane activity.

43 oast during periods of heightened basin-wide hurricane activity.

44 After a category 5 hurricane, adolescents in heavily affected areas with ex

45 ferent bacterial communities, revealing that hurricanes aerosolize a large amount of new cells.

46 ters per second), and a fivefold increase in hurricanes affecting the Caribbean.

47 Before the hurricane, an island's area was a better predictor of th

48 thic taxa under climate-driven disturbances (hurricanes and coral bleaching).

49 gly influences many natural hazards (such as hurricanes and droughts) and their resulting socioeconom

50 In coastal ecosystems, hurricanes and flooding can cause dramatic changes in wa

51 DTNP, 24.64N 82.86W), Florida, and show that hurricanes and other storm events are an additional and

52 reproduce the observed relationship between hurricanes and sea surface temperature will serve as a u

53 at have been observed after some landfalling hurricanes and that they cause much of the observed gust

54 Here we describe a positive feedback between hurricanes and the upper-ocean circulation in the tropic

55 ntion has focused on understanding trends in hurricanes and their destructive potential.

56 Tropical cyclones (also known as hurricanes and typhoons) are now believed to be an impor

57 all, European summer precipitation, Atlantic hurricanes and variations in global temperatures.

58 most-recent period of basin-wide quiescence, hurricanes (and particularly major hurricanes) near the

59 Growth and the mechanical (hurricanes) and biological erosion (parrotfish) of carbo

60 riability (such as earthquakes, tsunamis and hurricanes) and climate change (such as flooding and mor

61 the precursors to the most intense Atlantic hurricanes, and contribute to the global transport of Sa

62 Hurricanes are a potential risk to these turbines.

63 If hurricanes are indeed becoming more destructive over tim

64 ontrol the formation, intensity and track of hurricanes are poorly understood.

65 rturbations to the Florida Current caused by hurricanes are relevant to the spread of invasive lionfi

66 at, in addition to severity, the timing of a hurricane as it coincides with reproductive scheduling o

67 coral reefs, highlighting the potential for hurricane-associated cooling to mitigate climate change

68 increase in the potential destructiveness of hurricanes based on identification of a trend in an accu

69 an index of the potential destructiveness of hurricanes based on the total dissipation of power, inte

70 The passage of a hurricane can alleviate thermal stress on coral reefs, h

71 e only known scenario where the effects of a hurricane can benefit a stressed marine community.

72 Island inundation during hurricanes can have devastating effects on lizard popula

73 re natural environmental disturbances (e.g., hurricanes) can restore themselves via processes of natu

74 om US hurricanes to show that feminine-named hurricanes cause significantly more deaths than do mascu

75 d anthropogenic phenomena including climate, hurricanes, coastal development, agricultural runoff, oi

76 titioners, and the general public concerning hurricane communication and preparedness.

77 A later, stronger hurricane completely exterminated lizard populations at

78 ults suggest that over-water dispersal after hurricanes constrains adaptive diversification in Anolis

79 des of data, we find that violent storms and hurricanes contribute less than 1% to long-term salt mar

80 We discriminate and illustrate four kinds of hurricanes, cross-classified by two contrasts: earlier v

81 t it shares some properties with terrestrial hurricanes: cyclonic circulation, warm central region (t

82 ibbean reef community affected by bleaching, hurricane damage, and an increasing abundance of macroal

83 water volume of the second hurricane season (Hurricanes Dennis, Floyd, and Irene in 1999) delivered g

84 Three sequential hurricanes, Dennis, Floyd, and Irene, affected coastal N

85 However, their annualized hurricane deposition rate is overestimated, whereas rive

86 When averaged over the main hurricane-development region in the Atlantic, SST and VW

87 The hurricanes differed in two ways: one struck during the r

88 Our analysis shows that the pattern after a hurricane differs from the pattern after a simple tree-f

89 g open-top chambers for 11 yr, punctuated by hurricane disturbance in year 8.

90 with elevated CO(2) occurred after fire and hurricane disturbance.

91 ong the Atlantic and Gulf coasts as fire and hurricane disturbances became progressively more common.

92 gradient during the three dominant seasons (hurricane, dry, and early wet).

93 that residents were highly vulnerable to the hurricane--due in part to previous development assistanc

94 ignificant link to the energy of landfalling hurricanes during the subsequent hurricane season.

95 We also find that hurricanes during this period increased the rate of spre

96 before, during, and after two major tropical hurricanes, Earl and Karl.

97 d combined amount of inorganic sediments per hurricane equals (i) 12% of the Mississippi River's susp

98 d, consequently, greater coastal risk during hurricane events.

99 ession but only under the conditions of high hurricane exposure and low social support after adjustme

100 nd major depression under conditions of high hurricane exposure and low social support, confirming an

101 rricane PTSD and major depression given high hurricane exposure and low social support.

102 lly exposed cities were evaluated by using a hurricane exposure questionnaire, the Child Posttraumati

103 racteristics, baseline neighborhood poverty, hurricane exposure, and residence in the New Orleans met

104 ions to objective and subjective features of hurricane exposure, death of a family member, forced rel

105 s 6-9 months after the 2004 hurricanes about hurricane exposure, social support, and posthurricane PT

106 High-risk individuals (high hurricane exposure, the low-expression 5-HTTLPR variant,

107 ction (SBO), mushroom sign, clustered loops, hurricane eye, small bowel behind the superior mesenteri

108 of "eyewall replacement." Clouds outside the hurricane eyewall coalesce to form a new eyewall at a gr

109 s (two of the three lowest) that the earlier hurricane failed to exterminate even though it was stron

110 In contrast, interacting effects of hurricane floodwaters in 1999 and intensive fishing pres

111 nds in the Bahamas that were directly hit by Hurricane Floyd in September 1999.

112 fore and then 4 years after the catastrophic Hurricane Floyd passed directly over the site, inundatin

113 eful skill the wind energy of US landfalling hurricanes for the following main hurricane season (Augu

114 nd of increasing numbers of category 4 and 5 hurricanes for the period 1970-2004 is directly linked t

115 or forecasting the occurrence of landfalling hurricanes for the season ahead has been reported, but t

116 levels off as the wind speeds increase above hurricane force.

117 anticyclonic eddies, and was not affected by hurricane-forced mixing.

118 for multiseasonal, medium-range weather and hurricane forecasts.

119 Most Atlantic hurricanes form in the Main Development Region between 9

120 which would make the basin more suitable for hurricane formation and growth.

121 ificantly less water volume was delivered by Hurricane Fran (1996), but massive fish kills occurred i

122 portion of the variance in tropical Atlantic hurricane frequency and activity between 1965 and 2005.

123 ociated with a approximately 40% increase in hurricane frequency and activity.

124 r evaluating how potential future changes in hurricane frequency and intensity will impact forest tre

125 show that the decline of the Atlantic major hurricane frequency during 2005-2015 is associated with

126 suggesting the decline of the Atlantic major hurricane frequency during 2005-2015 is not likely due t

127 Observed Atlantic major hurricane frequency has exhibited pronounced multidecada

128 volving the inferred AMOC and Atlantic major hurricane frequency, along with indices of Atlantic Mult

129 AMOC in the recent decline of Atlantic major hurricane frequency.

130 tterns that either favour or hinder evolving hurricanes from reaching US shores.

131 High-resolution hindcast of hurricane-generated sea states and wave simulations are

132 sterly, Gulf of Mexico and western Caribbean hurricane genesis is four times more likely than when th

133 he whole basin, a 2.5-fold increase in major hurricanes (>/=50 meters per second), and a fivefold inc

134 nd Bahamian site, whereas an earlier, weaker hurricane had no detectable effect at a third Bahamian s

135 bility of areally averaged hurricane rain of Hurricane Harvey's magnitude by downscaling large number

136 In the MRD, hurricanes have been paradoxically identified as both su

137 a signal (e.g., whether to evacuate before a hurricane), (ii) choosing among fixed options (e.g., whi

138 ptoms in a longitudinal study (N = 561) of a Hurricane Ike affected population in Galveston and Chamb

139 ds show that a more compact yet more intense hurricane in 1821 CE probably resulted in a similar stor

140 We show that a major hurricane in the Bahamas led to the extinction of lizard

141 sment, Hurricane Sandy, the second costliest hurricane in United States history, hit the region.

142 The destruction wrought by North Atlantic hurricanes in 2004 and 2005 dramatically emphasizes the

143 umber of turbines that would be destroyed by hurricanes in an offshore wind farm.

144 More frequent and/or stronger hurricanes in the central Pacific imply greater heating

145 es at eight salt marsh locations affected by hurricanes in the United States.

146 sequent 3 months; no evidence of a long-term hurricane-induced algal bloom was observed.

147 in of the MRD that assesses both fluvial and hurricane-induced contributions to sediment accumulation

148 We provide evidence that hurricane-induced cooling was responsible for the docume

149 indicate that over multidecadal timescales, hurricane-induced sediment delivery may be an important

150 The impact of climate warming on hurricane intensities was investigated with a regional,

151 bility that the reef will withstand moderate hurricane intensity for two decades without becoming ent

152 Theory and modelling predict that hurricane intensity should increase with increasing glob

153 To better understand the change in global hurricane intensity since 1970, we examined the joint di

154 ne activity having occurred in recent years, hurricane intensity was equal or even greater during the

155 1970, we examined the joint distribution of hurricane intensity with variables identified in the lit

156 gh they influence shorter-term variations in hurricane intensity, do not contribute substantially to

157 hanism is vital to forecasting variations in hurricane intensity.

158 dels can lead to improvements in forecasting hurricane intensity.

159 changes in sea surface temperature (SST) and hurricane intensity.

160 undary layer dynamics, and the prediction of hurricane intensity.

161 Hurricane-intensity forecast improvements currently lag

162 e western North Atlantic margin to an active hurricane interval.

163 These hurricanes inundated the region with up to 1 m of rainfa

164 ed ocean observations and simulations during hurricane Irene (2011) reveal that the wind-forced two-l

165 North Carolina, before and after passage of Hurricane Irene in August 2011.

166 or that governs the genesis and intensity of hurricanes is ambient environmental vertical wind shear

167 The accumulation from hurricanes is sufficient to account for all the inorgani

168 of Turbidity-Maximum types before and after Hurricane Ivan (2004), which implies that extreme events

169 Hurricane Ivan, a category 4 storm, passed directly over

170 sing a 10-year data series accumulated since Hurricane Joan struck the Caribbean coast of Nicaragua i

171 e results show that the track prediction for Hurricane Joaquin is much more accurate with higher vert

172 f rogue waves during the 1-hour sea state of Hurricane Joaquin when the Merchant Vessel El Faro sank

173 ed out at different vertical resolutions for Hurricane Joaquin, which occurred from September 27 to O

174 dren with asthma were perilously impacted by Hurricane Katrina as a result of disrupted health care,

175 In August 2005, Hurricane Katrina created an environmental disaster that

176 Through a natural experiment focused on post-Hurricane Katrina Louisiana, I examine a counterfactual

177 Storm waves during Hurricane Katrina produced shear stresses between 425-36

178 Rain and flooding from Hurricane Katrina resulted in widespread growth of mold

179 t rapid subsidence in the three years before Hurricane Katrina struck in August 2005.

180 on 569 poor, predominantly African American Hurricane Katrina survivors to examine the extent to whi

181 Many Hurricane Katrina survivors with mental disorders experi

182 hurricane residents of the areas affected by Hurricane Katrina was administered via telephone survey

183 Hurricane Katrina's impact on U.S. Gulf Coast forests wa

184 As a result of Hurricane Katrina, > 100,000 homes were destroyed or dam

185 Since the record impact of Hurricane Katrina, attention has focused on understandin

186 many veterans were able to obtain care after Hurricane Katrina, there was a substantial disruption in

187 Due to Hurricane Katrina, which destroyed the Veterans Administ

188 the median level of samples collected before Hurricane Katrina.

189 sthma symptoms in New Orleans children after Hurricane Katrina.

190 ember 11, 2001, attack on New York City, and hurricane Katrina.

191 ice use by veterans from regions affected by Hurricane Katrina.

192 w-onset mental disorders in the aftermath of Hurricane Katrina.

193 of mental disorders among people exposed to Hurricane Katrina.

194 e on the reconstruction of New Orleans after Hurricane Katrina.

195 the system from a natural disaster like the hurricane Katrina.

196 of the attacks on the World Trade Center and Hurricane Katrina; and development of novel biological a

197 diments accumulated in coastal wetlands when Hurricanes Katrina and Rita crossed the Louisiana coast

198 e storm surge and wave field associated with Hurricanes Katrina and Rita eroded 527 km(2) of wetlands

199 Turner et al. measured sedimentation from Hurricanes Katrina and Rita in coastal Louisiana and inf

200 Hurricanes Katrina and Rita showed the vulnerability of

201 Floodwaters in New Orleans from Hurricanes Katrina and Rita were observed to contain hig

202 cord indicates that the frequency of intense hurricane landfalls has varied on centennial to millenni

203 rse-grained deposits associated with intense hurricane landfalls.

204 tennial- to millennial-scale records of past hurricane landfalls.

205 ed rapid recovery of prey populations to pre-hurricane levels on all control islands but on only a th

206 suggest that extreme weather events such as hurricanes likely help to homogenize the gene pool for a

207 d in an earlier study of spiders impacted by Hurricane Lili in a different Bahamian region.

208 The direct impact of Hurricane Lili in October 1996 did not alter the develop

209 ever, my analysis of a long-term data set of hurricane losses in the United States shows no upward tr

210 wahka community in Honduras before and after Hurricane Mitch (1994-2002) indicate that residents were

211 reactions among Nicaraguan adolescents after Hurricane Mitch and the relationship of these reactions

212 Using a downscaling hurricane model, we show dramatic shifts in the tropical

213 Eight weeks after the hurricane, mothers reported on exposure to hurricane-rel

214 ry experiments indicate that this is because hurricane names lead to gender-based expectations about

215 th conditions for more probable weakening of hurricanes near the United States coast.

216 iescence, hurricanes (and particularly major hurricanes) near the United States coast, although subst

217 hen seaweed was added to mimic deposition by hurricanes, no interactive predator effect occurred.

218 pendent: there was no apparent impact of the hurricanes on commercial landings of bivalve molluscs or

219 e study lizards regenerated from the earlier hurricane only via the egg stage, whereas eggs were unav

220 Two recent hurricanes passed directly over the northern Bahamas 2 y

221 Hurricane Patricia in 2015 was the strongest Pacific hur

222 g populations were a smaller fraction of pre-hurricane populations than on control islands.

223 I find that the record of net hurricane power dissipation is highly correlated with tr

224 vestigated with a regional, high-resolution, hurricane prediction model.

225 downscaling strategy by using an operational hurricane-prediction model that produces a realistic dis

226 The late-season hurricane produced a significant relation between popula

227 ed at least through two seasons; the earlier hurricane produced no such relationship.

228 s can be observed in cultures by varying the hurricane radius and mean rotational velocity.

229 , the annual probability of areally averaged hurricane rain of Hurricane Harvey's magnitude by downsc

230 ase was seen in the number and proportion of hurricanes reaching categories 4 and 5.

231 pressive reactions and features of objective hurricane-related experiences followed a "dose-of-exposu

232 oastal population--a substantial increase in hurricane-related losses in the twenty-first century.

233 e hurricane, mothers reported on exposure to hurricane-related stress and children's internalizing an

234 Among children exposed to higher levels of hurricane-related stress, enhanced neural reactivity to

235 The survey assessed hurricane-related stressors and screened for 30-day DSM-

236 ns between DSM-IV anxiety-mood disorders and hurricane-related stressors separately among prehurrican

237 y-mood disorders, the strong associations of hurricane-related stressors with these outcomes, and the

238 er by differential exposure or reactivity to hurricane-related stressors.

239 majority of respondents reported exposure to hurricane-related stressors.

240 areas with extreme objective and subjective hurricane-related traumatic features of exposure experie

241 the predictor variables to the frequency of hurricanes remain unclear.

242 variety of modelling applications, including hurricane risk assessment and prediction of storm motion

243 Do people judge hurricane risks in the context of gender-based expectati

244 itions, including history of flooding during Hurricane Sandy 7 months prior to the study.

245 eastern USA on (i) regional flood damages by Hurricane Sandy and (ii) local annual flood losses in Ba

246 with titles, descriptions or tags related to Hurricane Sandy bears a striking correlation to the atmo

247 To investigate user attention to the Hurricane Sandy disaster in 2012, we analyze data from F

248 inlets in these areas, even though prior to Hurricane Sandy in 2012, no inlet was present in the eas

249 e occurrence of additional flood events like Hurricane Sandy in recent centuries, and highlight the i

250 he magnitude of flooding in New York City by Hurricane Sandy is commonly believed to be extremely rar

251 enarios that start 4 weeks after landfall of Hurricane Sandy on October 29, 2012, and ending 2 years

252 Here we compare resultant deposition by Hurricane Sandy to earlier storm-induced flood layers in

253 fect of sea level rise, the return period of Hurricane Sandy's flood height decreased by a factor of

254 wing the event-related potential assessment, Hurricane Sandy, the second costliest hurricane in Unite

255 We applied these strategies to Hurricane Sandy, which struck the northeastern United St

256 $625 Million in direct flood damages during Hurricane Sandy.

257 es in the areas of New York City affected by Hurricane Sandy.

258 ng in the areas of New York City affected by Hurricane Sandy.

259 andfalling hurricanes for the following main hurricane season (August to October).

260 The high water volume of the second hurricane season (Hurricanes Dennis, Floyd, and Irene in

261 ntic that may have contributed to the strong hurricane season caused widespread coral bleaching in th

262 Observations made during the historic 2005 hurricane season document a case of "eyewall replacement

263 Patricia's intensity and the active 2015 ENP hurricane season have been partially attributed to the s

264 During the 2005 hurricane season, the storm surge and wave field associa

265 landfalling hurricanes during the subsequent hurricane season.

266 Ecosystem-level impacts of two hurricane seasons were compared several years after the

267 lionfish became established in the Bahamas, hurricanes significantly hastened their spread through t

268 Twelve months after the hurricane, species richness averaged over all islands re

269 studying rare events, including damage from hurricanes, stock market crashes, insurance claims, floo

270 ere we present a 3000 year record of intense hurricane strikes in the northern Bahamas (Abaco Island)

271 the ITCZ has likely helped modulate intense hurricane strikes on the western North Atlantic margin o

272 n the United States is caused by landfalling hurricanes--strong tropical cyclones that reach the coas

273 le of 590 participants from the 2004 Florida Hurricane Study.

274 Responses after fire and hurricanes suggest that disturbance promotes the growth

275 while VWS inhibits genesis and prevents any hurricanes that do form from reaching their potential in

276 ese regions together account for most of the hurricanes that make landfall in the United States.

277 about 2.2 degrees C, the simulations yielded hurricanes that were more intense by 3 to 7 meters per s

278 Before the hurricane, the predator had reduced prey populations to

279 After the hurricane, the slope increased from near zero (7 months

280 Before the hurricane, the species-area relation was generally stron

281 mble at the first challenge by earthquake or hurricane, there may be defectively assembled maternal b

282 in shallow estuaries frequently disturbed by hurricanes, there can be relatively rapid recovery in wa

283 mong the victims of floods, earthquakes, and hurricanes, there is an increased prevalence of post-tra

284 mulated ocean currents during the passage of hurricanes through the Florida Straits and (2) the devel

285 e Patricia in 2015 was the strongest Pacific hurricane to make landfall in Mexico.

286 ertical accretion, but the contribution from hurricanes to long-term sediment accumulation is substan

287 more than six decades of death rates from US hurricanes to show that feminine-named hurricanes cause

288 This feedback is based on the ability of hurricanes to warm water parcels that travel towards the

289 ive impacts of higher vertical resolution on hurricane track forecasts suggest that National Oceanic

290 In the present climate, very few hurricane tracks intersect the parcel trajectories; cons

291 ents currently lag the progress achieved for hurricane tracks.

292 surface temperature (SST) is correlated with hurricane variability through its relationship with the

293 Two months after the hurricane, we found only recently hatched individuals--a

294 The atmosphere-ocean coupled Hurricane Weather Research and Forecast model (HWRF) dev

295 The samples from the two hurricanes were characterized by significantly different

296 ed within 2 yr after disturbance by fire and hurricane, when soil nutrient availability was high.

297 regional sedimentary evidence of landfalling hurricanes, while the second estimate uses a previously

298 The late-season hurricane wiped out populations of lizards on two island

299 fluence of future global warming on Atlantic hurricanes with a downscaling strategy by using an opera

300 tended consequence of the gendered naming of hurricanes, with important implications for policymakers