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1 riables (including lower pressure during the hurricane).
2 ditions, floods, a dry El Nino period, and a hurricane.
3 multiple streams for several weeks after the Hurricane.
4 ion results for the first 2 months after the hurricane.
5 Symptoms were reassessed 8 months after the hurricane.
6 ct externalizing symptoms 8 months after the hurricane.
7 likely contributed to the subsequent extreme hurricane.
8 ior management was stronger than that of the hurricane.
9 spite exposure to two consecutive category 5 hurricanes.
10 sis and thermodynamic potential intensity of hurricanes.
11 ubject to more frequent extreme flooding and hurricanes.
12 ficantly more deaths than do masculine-named hurricanes.
13 upply favourable for the formation of strong hurricanes.
14 also exhibited stronger responses following hurricanes.
15 nd detect the changes subsequent to the 2017 hurricanes.
16 n linked to eutrophication, overfishing, and hurricanes.
17 ific, warmer tropics and, in turn, even more hurricanes.
18 isting wetlands rendering them vulnerable to hurricanes.
19 ect of assigning female versus male names to hurricanes.
20 major outages in the US have been caused by hurricanes.
21 S), a metric that strongly controls Atlantic hurricanes.
22 who developed new-onset disorders after the hurricane, 18.5% received some form of treatment for emo
23 uencing a range of climate processes such as hurricane activity and African Sahel and Amazonian droug
25 deed, toepad area positively correlates with hurricane activity for both 12 island populations of Ano
28 ening phase and thus favorable for increased hurricane activity in the Main Development Region (MDR),
30 ast Coast during decadal periods of enhanced hurricane activity is substantially reduced by GHG forci
31 Problematically, determining whether high hurricane activity levels remained constant through time
32 ons conducive to greater basin-wide Atlantic hurricane activity occur together with conditions for mo
33 , and documents a period of elevated intense hurricane activity on the western North Atlantic margin
35 ble for approximately 40% of the increase in hurricane activity relative to the 1950-2000 average bet
36 gests that spatial heterogeneity in Atlantic hurricane activity since 1850 CE could have persisted th
37 ns about the natural range in variability of hurricane activity that the instrumental record is too s
38 te that the sensitivity of tropical Atlantic hurricane activity to August-September sea surface tempe
39 position on geologic timescales can modulate hurricane activity, but continuous and long-term storm r
40 enhouse gases contributed to the increase in hurricane activity, but the ability of climate models to
41 s climate index is associated with shifts in hurricane activity, rainfall patterns and intensity, and
49 gly influences many natural hazards (such as hurricanes and droughts) and their resulting socioeconom
52 was the increase in rainfall associated with hurricanes and El Nino, resulting in enhanced nutrient l
57 reproduce the observed relationship between hurricanes and sea surface temperature will serve as a u
58 Here we describe a positive feedback between hurricanes and the upper-ocean circulation in the tropic
61 most-recent period of basin-wide quiescence, hurricanes (and particularly major hurricanes) near the
63 riability (such as earthquakes, tsunamis and hurricanes) and climate change (such as flooding and mor
64 t), hydrological (flooding), meteorological (hurricanes), and geophysical (volcanic activity, tsunami
65 the precursors to the most intense Atlantic hurricanes, and contribute to the global transport of Sa
67 ntially reduced by GHG forcing, which allows hurricanes approaching the U.S. coast to intensify more
71 rturbations to the Florida Current caused by hurricanes are relevant to the spread of invasive lionfi
74 rn region, highlighting the positive role of hurricanes as a natural fertilization mechanism influenc
75 coral reefs, highlighting the potential for hurricane-associated cooling to mitigate climate change
78 ate events such as droughts, cold snaps, and hurricanes can be powerful agents of natural selection,
79 re natural environmental disturbances (e.g., hurricanes) can restore themselves via processes of natu
80 om US hurricanes to show that feminine-named hurricanes cause significantly more deaths than do mascu
81 d anthropogenic phenomena including climate, hurricanes, coastal development, agricultural runoff, oi
83 des of data, we find that violent storms and hurricanes contribute less than 1% to long-term salt mar
85 t it shares some properties with terrestrial hurricanes: cyclonic circulation, warm central region (t
86 onomic activity using nightlights, potential hurricane damages using a detailed wind field model, and
88 omparing pre-hurricane data (2013) with post hurricane data we find that management style had only a
89 no was instrumental in collecting post-Maria Hurricane data, as part of the Next Generation Ecosystem
94 tabase data to estimate associations between hurricane disaster declarations, which could disrupt ele
100 ong the Atlantic and Gulf coasts as fire and hurricane disturbances became progressively more common.
101 In 2019, category 5 (Saffir-Simpson scale) Hurricane Dorian demonstrated the destructive potential
104 that residents were highly vulnerable to the hurricane--due in part to previous development assistanc
107 rtunity to explore the relationships between hurricanes, El Nino and HABs in two Florida estuaries su
108 y established accumulation rates, this multi-hurricane event equates to ~1-3 centuries of deposition.
110 racteristics, baseline neighborhood poverty, hurricane exposure, and residence in the New Orleans met
111 ction (SBO), mushroom sign, clustered loops, hurricane eye, small bowel behind the superior mesenteri
112 severe disturbances caused by major tropical hurricanes facilitate gene-flow and increase overall gen
113 eveloped an operational remote sensing-based hurricane flood extent mapping method, examined potentia
114 term impacts of extreme river discharge from Hurricane Florence were particularly evident as PicoP bi
115 examined the impacts of moderate to extreme (Hurricane Florence, September 2018) precipitation events
120 portion of the variance in tropical Atlantic hurricane frequency and activity between 1965 and 2005.
122 r evaluating how potential future changes in hurricane frequency and intensity will impact forest tre
123 nction of climate change-triggered shifts in hurricane frequency and intensity; yet projections of bo
124 show that the decline of the Atlantic major hurricane frequency during 2005-2015 is associated with
125 suggesting the decline of the Atlantic major hurricane frequency during 2005-2015 is not likely due t
127 volving the inferred AMOC and Atlantic major hurricane frequency, along with indices of Atlantic Mult
129 tern United States also experienced frequent hurricanes from 1500 to 1670 CE, but frequency was depre
134 bility of areally averaged hurricane rain of Hurricane Harvey's magnitude by downscaling large number
140 erty damage caused by 88 tropical storms and hurricanes hitting the United States between 1996 and 20
141 cted in the same forest in Puerto Rico after Hurricanes Hugo (1989, category 3), Georges (1998, categ
142 ases the probability and intensity of severe hurricanes, human management of disturbance-adapted land
143 a signal (e.g., whether to evacuate before a hurricane), (ii) choosing among fixed options (e.g., whi
144 ptoms in a longitudinal study (N = 561) of a Hurricane Ike affected population in Galveston and Chamb
146 hamas have experienced more frequent intense-hurricane impacts than almost anywhere else in the Atlan
147 ds show that a more compact yet more intense hurricane in 1821 CE probably resulted in a similar stor
148 sment, Hurricane Sandy, the second costliest hurricane in United States history, hit the region.
149 water quality implications of two "500-year" hurricanes in 2016 and 2018, and identified options to i
150 iscus; N = 30) before, during, and after two hurricanes in 2017 using fine-scale acoustic telemetry a
154 nse to two of the most destructive Caribbean hurricanes in known history - Irma and Maria, which were
158 in of the MRD that assesses both fluvial and hurricane-induced contributions to sediment accumulation
159 gh density wood were resistant to uprooting, hurricane-induced mortality, and were protected from bre
160 indicate that over multidecadal timescales, hurricane-induced sediment delivery may be an important
161 ithout considering the positive influence of hurricane-induced sediment deposition and associated nut
164 les from Hawaiian volcanic and West Atlantic hurricane interactions, this work illustrates how the di
166 ed ocean observations and simulations during hurricane Irene (2011) reveal that the wind-forced two-l
171 from Costa Rica and event-based sampling of Hurricanes Irma and Maria (2017), to underpin the dynami
174 or that governs the genesis and intensity of hurricanes is ambient environmental vertical wind shear
175 of Turbidity-Maximum types before and after Hurricane Ivan (2004), which implies that extreme events
176 e results show that the track prediction for Hurricane Joaquin is much more accurate with higher vert
177 f rogue waves during the 1-hour sea state of Hurricane Joaquin when the Merchant Vessel El Faro sank
178 ed out at different vertical resolutions for Hurricane Joaquin, which occurred from September 27 to O
179 dren with asthma were perilously impacted by Hurricane Katrina as a result of disrupted health care,
181 e also identify important events such as the Hurricane Katrina in August 2005 and the Oil Price Crisi
182 Through a natural experiment focused on post-Hurricane Katrina Louisiana, I examine a counterfactual
185 on 569 poor, predominantly African American Hurricane Katrina survivors to examine the extent to whi
187 dy of young, low-income mothers who survived Hurricane Katrina, we find that bereavement, fearing for
192 of the attacks on the World Trade Center and Hurricane Katrina; and development of novel biological a
193 e storm surge and wave field associated with Hurricanes Katrina and Rita eroded 527 km(2) of wetlands
196 ning whether the frequency of recent intense hurricane landfalls in the northern Gulf of Mexico (GOM)
197 on the Saffir-Simpson Hurricane Wind Scale) hurricane landfalls, prompting questions about the natur
199 suggest that extreme weather events such as hurricanes likely help to homogenize the gene pool for a
200 high) was reduced in the year following the hurricanes, mainly due to a decline in abundance of recr
202 a comprehensive assessment of the impact of Hurricane Maria (HM) on drinking water quality in Puerto
208 rs associated with damage severity caused by Hurricanes Maria and Irma across Puerto Rican forests.
211 y provides long-term context for events like Hurricane Michael and suggests that the observational pe
212 n temperatures occurred prior to landfall of Hurricane Michael during October of 2018 and, as critica
213 of Florida LPE that was directly affected by Hurricane Michael in 2018, an unprecedented Category 5 s
214 wahka community in Honduras before and after Hurricane Mitch (1994-2002) indicate that residents were
217 ry experiments indicate that this is because hurricane names lead to gender-based expectations about
219 iescence, hurricanes (and particularly major hurricanes) near the United States coast, although subst
220 hen seaweed was added to mimic deposition by hurricanes, no interactive predator effect occurred.
222 ivity are common following disasters such as hurricanes, oil spills, and tsunamis, which may lead to
224 al hazard events (e.g., earthquakes, floods, hurricanes) on assets, people and society is of primary
228 ar-annually resolved stratigraphic record of hurricane passage near Thatchpoint Blue Hole (TPBH) on A
231 o 1670 CE, which exceeds the 9 >= category 2 hurricanes per century within 50 km of TPBH since 1850 C
232 downscaling strategy by using an operational hurricane-prediction model that produces a realistic dis
233 for the first time, bridge the physics-based hurricane projections and intricate outage risk models.
234 the epistemic uncertainties in physics-based hurricane projections under climate change, largely due
236 , the annual probability of areally averaged hurricane rain of Hurricane Harvey's magnitude by downsc
237 orcing, but additional high-resolution paleo-hurricane reconstructions are required to assess the mec
238 ence to sea-level rise and is used to extend hurricane records beyond historical accounts by reconstr
239 e hurricane, mothers reported on exposure to hurricane-related stress and children's internalizing an
240 Among children exposed to higher levels of hurricane-related stress, enhanced neural reactivity to
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
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
259 Patricia's intensity and the active 2015 ENP hurricane season have been partially attributed to the s
260 effects of the most energetic North Atlantic hurricane season in 50 years on the genetic diversity an
266 lionfish became established in the Bahamas, hurricanes significantly hastened their spread through t
267 studying rare events, including damage from hurricanes, stock market crashes, insurance claims, floo
268 ere we present a 3000 year record of intense hurricane strikes in the northern Bahamas (Abaco Island)
269 the ITCZ has likely helped modulate intense hurricane strikes on the western North Atlantic margin o
272 canus) left the study area shortly after the hurricanes, suggesting vulnerability stemming from alter
274 while VWS inhibits genesis and prevents any hurricanes that do form from reaching their potential in
275 ese regions together account for most of the hurricanes that make landfall in the United States.
277 mble at the first challenge by earthquake or hurricane, there may be defectively assembled maternal b
278 mulated ocean currents during the passage of hurricanes through the Florida Straits and (2) the devel
281 ertical accretion, but the contribution from hurricanes to long-term sediment accumulation is substan
282 more than six decades of death rates from US hurricanes to show that feminine-named hurricanes cause
283 This feedback is based on the ability of hurricanes to warm water parcels that travel towards the
284 ive impacts of higher vertical resolution on hurricane track forecasts suggest that National Oceanic
287 surface temperature (SST) is correlated with hurricane variability through its relationship with the
288 area (GHMA) starting on August 25, 2017; the Hurricane was also associated with damage to environment
290 strial or marine) and changes induced by the hurricanes, we collected bathymetry surveys and sediment
293 d population growth rates in the year of the hurricane were higher in previously managed plots than i
295 ed within 2 yr after disturbance by fire and hurricane, when soil nutrient availability was high.
296 regional sedimentary evidence of landfalling hurricanes, while the second estimate uses a previously
297 eeding Category 4 or 5 on the Saffir-Simpson Hurricane Wind Scale) hurricane landfalls, prompting que
298 fluence of future global warming on Atlantic hurricanes with a downscaling strategy by using an opera
299 or structure for the years prior to the 2017 hurricanes, with genetic structure occurring at the loca
300 tended consequence of the gendered naming of hurricanes, with important implications for policymakers