ライフサイエンスコーパス: cyclone

1 ns and salinity changes caused by a tropical cyclone.

2 tation and flooding associated with tropical cyclones.

3 lones, light rain, and land-falling tropical cyclones.

4 al resolution on track forecasts of tropical cyclones.

5 nerated by rainfall associated with tropical cyclones.

6 ing precipitation, temperature, and tropical cyclones.

7 increasingly prone to flooding from tropical cyclones.

8 ociated with anticipated floods and tropical cyclones.

9 ing the effect of global warming on tropical cyclones.

10 consequently, an intensification of tropical cyclones.

11 impacts of natural hazards, such as tropical cyclones.

12 quency and tracks of North Atlantic tropical cyclones.

13 0.09 m s(-1) yr(-1) (s.e.) for the strongest cyclones.

14 nteractions dampen eddy-induced upwelling in cyclones.

15 with the vertical mixing induced by tropical cyclones.

16 ave trains on the front side of the tropical cyclones.

17 ystems such as monsoon rainfall and tropical cyclones.

18 ulnerable to economic damages resulting from cyclones.

19 strength of the jet stream and extratropical cyclones(1-3).

20 he El Nino Southern Oscillation(1), tropical cyclones(2,3) and the monsoons(4-10), and contributes to

21 m wind speeds of the very strongest tropical cyclones (99th percentile) over each ocean basin, with t

22 Climate change is intensifying tropical cyclones, accelerating sea-level rise, and increasing co

23 peeds (that is, the maximum intensities that cyclones achieve during their lifetimes), estimated from

24 e known to influence North Atlantic tropical cyclone activity and because their underlying drivers ar

25 ades, with marked decreases in extratropical cyclone activity and eddy kinetic energy (EKE) in summer

26 Increases in tropical cyclone activity are most prominent in the western North

27 epict a global-average migration of tropical cyclone activity away from the tropics at a rate of abou

28 reconstruction of western Caribbean tropical cyclone activity developed using a new coupled carbon an

29 ished statistical model of Atlantic tropical cyclone activity driven by proxy reconstructions of past

30 tent evidence of a peak in Atlantic tropical cyclone activity during medieval times (around ad 1000)

31 breeding colony and positively by increasing cyclone activity in the Northern Indian Ocean where they

32 Here, we analyze the role of cyclone activity on the seasonal buildup of snow on Arct

33 paring two independent estimates of tropical cyclone activity over the past 1,500 years.

34 Western Caribbean tropical cyclone activity peaked at 1650 A.D., coincident with ma

35 the need to scrutinize mechanisms governing cyclone activity to better understand their effects on t

36 temperature change--the response of tropical cyclone activity to natural climate variations, which te

37 Atlantic tropical cyclone activity, as measured by annual storm counts, re

38 tent with decreases in EKE and extratropical cyclone activity, but convective MAPE increased, implyin

39 a hinder the detection of trends in tropical cyclone activity.

40 be considered in projecting future tropical cyclone activity.

41 late the vertical mixing induced by tropical cyclone activity.

42 eliable to reveal trends in intense tropical cyclone activity.

43 n the same latitudinal zone as most tropical cyclone activity.

44 nly juvenile petrel survival was affected by cyclone activity; negatively by a strong cyclone in the

45 epared to simulate those collected by wetted cyclone aerosol collector of approximately 80% efficienc

46 rties during early- and late-season tropical cyclones affecting Okinawa, Japan.

47 have not been documented for one of the most cyclones affecting regions of the world like Taiwan.

48 In addition, the cyclones also gave southward ice drift.

49 ars of hourly rain gauges data, we estimated cyclones (also called typhoons) rainfall erosivity over

50 Tropical cyclones (also known as hurricanes and typhoons) are now

51 creasing frequency and intensity of tropical cyclones, an accurate forecasting of cyclone evolution a

52 fluence of temperature from that of tropical cyclones, an important correlate.

53 The PENS consists of a respirable cyclone and a micro-orifice impactor with the cutoff aer

54 agree well with those of the IOSH respirable cyclone and MOUDI.

55 ults show that the d(pa50) of the respirable cyclone and the micro-orifice impactor are 3.92 +/- 0.22

56 sters: 26% of the population are affected by cyclones and 70% live in flood-prone regions.

57 n after 1900 because of more active tropical cyclones and a larger extent of forested areas.

58 The CRs associated with both cyclones and anticyclones represents an important contri

59 (e.g., the Atlantic seaboard due to tropical cyclones and atmospheric lows or troughs).

60 t 0.89% y(-1), despite ongoing losses due to cyclones and bleaching.

61 to weaker mid-latitude westerly flow, weaker cyclones and decreased net terrestrial mid-latitude prec

62 e maintenance and reduction of the effect of cyclones and floods include rapid urbanisation and the g

63 linkages between observed trends in tropical cyclones and in the environment.

64 ipitation, atmospheric circulation, tropical cyclones and other extreme events.

65 improving forecasts of extratropical winter cyclones and storm systems and projections of their resp

66 depend on both storm surges during tropical cyclones and the rising relative sea levels on which tho

67 which provides some of the fuel for tropical cyclones and their intensification, but also provides so

68 the potential maximum intensity of tropical cyclones, and human heat stress, and has important effec

69 By anticipating the trajectory of tropical cyclones, and sampling populations before and after they

70 tsunami waves commonly occur during tropical cyclones, and that they can contribute significantly to

71 of chains of inertially pulsating mesoscale cyclones/anticyclones, which to date remain poorly known

72 Tropical cyclones are expected to intensify under a warming clima

73 Atlantic tropical cyclones are getting stronger on average, with a 30-year

74 pper ocean, but the hypothesis that tropical cyclones are important mixing agents at the global scale

75 Tropical cyclones are increasing in intensity and size and, thus,

76 For seabirds, the impacts of cyclones are known to be detrimental at breeding colonie

77 The winds associated with tropical cyclones are known to lead to localized mixing of the up

78 Tropical cyclones are one of the most destructive natural hazards

79 Tropical cyclones are renowned for their destructive nature and a

80 Our results indicate that tropical cyclones are responsible for significant cooling and ver

81 While cyclones are stronger in the Atlantic, Pacific snow accu

82 ts of climate change on landfalling tropical cyclones are unclear.

83 consequences, their impacts during tropical cyclones are underappreciated.

84 climate change on the intensity of tropical cyclones are yet to be fully understood due to the varie

85 Extreme events, such as tropical cyclones, are destructive and influential forces.

86 ged for epidemiological research on tropical cyclones, as well as insights that can inform the design

87 i in the bottom ash, heat exchanger ash, and cyclone ash fractions.

88 uish Jupiter from Saturn, which has only one cyclone at each pole?

89 n the dynamic impacts of historical tropical cyclones at a continental scale.

90 atterns: tropical moisture exports, tropical cyclones, atmospheric lows or troughs, and melting snow.

91 n shielding-an anticyclonic ring around each cyclone, but also on the depth.

92 development and intensification of tropical cyclones, but cyclone genesis and intensity are also aff

93 nough to support the development of tropical cyclones, but the atmospheric monsoon circulation and as

94 ncrease in the frequency of intense tropical cyclones, but this proposal has been challenged on the b

95 lysis, we demonstrate modulated mid-latitude cyclones by Asian pollution over the past three decades.

96 lations, and they suggest that extratropical cyclones can weaken even as their associated convection

97 Tropical cyclones cause extensive tree mortality and damage to fo

98 Additionally, changes in tropical cyclone characteristics have led to increases in the ext

99 er, our study shows that changes in tropical-cyclone climatology affect trends in fluvial suspended s

100 < 0.1) with observed variations in tropical-cyclone climatology, and that a substantial portion (32

101 7.1 megatonnes is due to a shift in tropical-cyclone climatology.

102 sol using a nebulizer and collection using a cyclone collector was used to provide a proof of concept

103 We demonstrate that tropical cyclones contribute to drying the Maritime Continent atm

104 continues to suffer from repeated impacts of cyclones, coral bleaching, and outbreaks of the coral-ea

105 Tropical cyclones, coral predation by crown-of-thorns starfish (C

106 of increase in coral cover in the absence of cyclones, COTS, and bleaching was 2.85% y(-1), demonstra

107 gest that the frequency of Atlantic tropical cyclones could decrease as the climate warms.

108 n the distribution and frequency of tropical cyclones could therefore become an important element of

109 Multidecadal Oscillation (AMO), and tropical cyclone counts (TC).

110 However, our understanding of how tropical cyclones currently affect marine biodiversity, and pelag

111 models to generate large synthetic tropical cyclone data sets for the North Atlantic basin; driving

112 conciles a decadal variation of mid-latitude cyclones derived from the Reanalysis data.

113 associated strong vertical wind shear limits cyclone development and intensification, only permitting

114 eased sea surface temperatures amplify local cyclone development and refuel North Atlantic low-pressu

115 ad to more favorable conditions for tropical cyclone development compared with the orbital forcing al

116 nsity and can also reflect the likelihood of cyclone development.

117 egan with my immersion in cholera control, a cyclone disaster, a smallpox epidemic, and formal traini

118 d socioeconomic data for over 1,000 tropical cyclone disasters from 1979 to 2016.

119 subjected to monsoonal forcing and tropical cyclones, displays a complex field of ocean eddies.

120 del, we show dramatic shifts in the tropical cyclone distribution for the early Pliocene that favour

121 s the final establishment of modern tropical cyclone distribution.

122 Tropical cyclones downscaled from the climate of the period 1950-

123 erived from large sets of synthetic tropical cyclones, downscaled from RCP8.5 simulations from three

124 energetic reservoir from which extratropical cyclones draw.

125 events the vortices from merging, given that cyclones drift poleward in atmospheres of rotating plane

126 USA, has experienced three extreme tropical cyclone-driven flood events since 1999, causing catastro

127 ntensity of pre-monsoon Arabian Sea tropical cyclones during the period 1979-2010, and show that this

128 tanding the fundamental controls on tropical cyclone dynamics.

129 n has suffered from a couple of tornados and cyclones, e.g. Cyclone Gonu on June 1, 2007, making the

130 Our understanding of cyclone ecology is biased towards the North Atlantic Bas

131 nization, but we lack a scale-perspective of cyclone ecology.

132 a global collaboration initiative to advance cyclone ecology.

133 ed towards the North Atlantic Basin, because cyclone effects do differ across oceanic basins.

134 Thus, the greater the accumulated cyclone energy, the stronger (weaker) the El Nino (La Ni

135 Near the event site, cyclone-enhanced strong southeasterly katabatic winds dr

136 of the storm can help in designing tropical cyclone epidemiological research.

137 inform the design and analysis for tropical cyclone epidemiological research.

138 Tropical cyclone epidemiology can be advanced through exposure as

139 ges due to tropical (TCs) and extra-tropical cyclones (ETCs).

140 ssemblages before and after a known tropical cyclone event (Cyclone Hamish) with the aim to better re

141 ropical cyclones, an accurate forecasting of cyclone evolution and ocean response is becoming even mo

142 Provide an open-source data set for tropical cyclone exposure assessment for epidemiological research

143 between county-level assessments of tropical cyclone exposure based on different storm hazards.

144 astal economic activity and find that direct cyclone exposure typically results in permanent loss of

145 ets that spontaneously generates giant polar cyclones, fierce alternating zonal flows, and a high-lat

146 we are witnessing a regime shift in tropical cyclone flooding and associated ecosystem impacts.

147 of the global population exposed to tropical cyclone flooding live on deltas, with 92% (28 million) i

148 Extreme weather events (e.g., cyclones, floods, droughts) are capable of changing ecos

149 Indian Ocean and were potentially exposed to cyclones for a substantial part of their annual cycle.

150 h, the surface assemblage returns to its pre-cyclone form, but results imply that it is unlikely the

151 A number of patterns in tropical cyclone frequency and intensity have been identified.

152 carbon cycle impacts for historical tropical cyclones from 1851 to 2000 over the continental U.S.

153 ude by downscaling large numbers of tropical cyclones from three climate reanalyses and six climate m

154 nd intensification of tropical cyclones, but cyclone genesis and intensity are also affected by the v

155 ed the geographical distribution of tropical cyclone genesis remains unknown.

156 affects tropical precipitation and tropical cyclone genesis, and these changes have been tied to the

157 from a couple of tornados and cyclones, e.g. Cyclone Gonu on June 1, 2007, making the changes even mu

158 re and after a known tropical cyclone event (Cyclone Hamish) with the aim to better resolve the chara

159 sites greatly reduced immediately following Cyclone Hamish, and discernible shifts in assemblage div

160 fy no allochthonous material associated with Cyclone Hamish.

161 The record of tropical cyclones has been extensively impacted by improvements i

162 Consequently, tropical cyclones have a key role in controlling the magnitude of

163 on in the average latitude at which tropical cyclones have achieved their lifetime-maximum intensity

164 Tropical cyclones have been hypothesized to influence climate by

165 Cyclones have both short and long-term effects across th

166 he county level on exposure to four tropical cyclone hazards: peak sustained wind, rainfall, flooding

167 een employed to quantify a region's tropical cyclone history.

168 narios will result in more frequent tropical cyclone impacts on the financial and population centres

169 e maximum intensity achievable by a tropical cyclone in a given local environment.

170 by cyclone activity; negatively by a strong cyclone in the vicinity of the breeding colony and posit

171 ulating large [O(10(4))] numbers of tropical cyclones in climate states described by global gridded d

172 erall flood heights associated with tropical cyclones in New York City in coming centuries to increas

173 We used a 20-year data set on tropical cyclones in the Indian Ocean, tracking data from 122 Rou

174 owever, the observational record of tropical cyclones in the North Atlantic basin is too short (A.D.

175 simulations to isolate the role of tropical cyclones in transmitting suspended sediment to one of th

176 aused by tropical moisture exports (tropical cyclones) in the western and central (eastern) United St

177 models, the frequency of downscaled tropical cyclones increases during the 21st century in most locat

178 Similar cyclone-induced events have occurred at this site in the

179 ere-wave numerical model to analyze tropical cyclone-induced meteotsunami generation and propagation

180 We quantified cyclone-induced ocean warming by directly monitoring the

181 ata provide compelling evidence for tropical cyclone-induced selection driving the evolution of an im

182 y be predictable on synoptic time scales, if cyclone-induced strong wind events can be predicted.

183 The area coverage of tropical cyclones influences their impact on human lives, yet lit

184 herent features of the structure of tropical cyclones: inner and outer spiral rainbands.

185 we systematically demonstrate that tropical cyclone intensification is significantly affected by sal

186 of sea spray, with consequences for tropical cyclone intensification or decline, particularly in area

187 On average, the tropical cyclone intensification rate is nearly 50% higher over r

188 asets show significant increases in tropical cyclone intensification rates in the Atlantic basin that

189 there are observed upward trends in tropical cyclone intensification rates.

190 an environment more favourable for tropical cyclone intensification.

191 the climatological distribution of tropical cyclone intensification.

192 key to more skillful predictions of tropical cyclone intensities through improved ocean state estimat

193 o substantially larger increases in tropical cyclone intensities.

194 '--a measure that provides an upper bound on cyclone intensity and can also reflect the likelihood of

195 ropics, however, possible trends in tropical cyclone intensity are less obvious, owing to the unrelia

196 rculation modification could affect tropical cyclone intensity over the Arabian Sea, but so far no su

197 Recent assessments agree that tropical cyclone intensity should increase as the climate warms.

198 between the two common measures of tropical cyclone intensity, the central pressure deficit and the

199 tion of recent historical trends in tropical cyclone intensity.

200 eals that the rate of warming increases with cyclone intensity.

201 Increasingly, flood and cyclone interventions have leveraged community resilienc

202 we document the regional effects of Tropical Cyclone Irene on thermal structure and ecosystem metabol

203 usly evaluating of the ecological impacts of cyclones is logistically challenging.

204 in convection associated with extratropical cyclones is poorly understood.

205 We find that the long-term effect of cyclones is to warm the ocean at a rate of 0.32 +/- 0.15

206 dition, we show that widespread windthrow by cyclone Klaus in the Landes forest led to a significant

207 ose that the ITE was the product of Tropical Cyclone Lehar interaction on 27 November 2013 with a wes

208 ear convective systems (QLCS), extratropical cyclones, light rain, and land-falling tropical cyclones

209 C) as a tracer of coastal water to show that cyclones located offshore that were generated near the c

210 surface temperatures (SST) from the tropical cyclone main developmental region (MDR), the El Nino-Sou

211 Because most Arabian Sea tropical cyclones make landfall, our results suggest an additiona

212 tion centres as sea levels rise and tropical cyclone maximum intensities migrate poleward.

213 amining trends in the upper quantiles of per-cyclone maximum wind speeds (that is, the maximum intens

214 a) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and

215 or experience with rip currents and tropical cyclones moderated the strength of the actual-perceived

216 ctiveness are associated with lower tropical cyclone mortality, even when controlling for average inc

217 carbon concentrations in their interior than cyclones of the same amplitude generated offshore.

218 Super typhoons (STYs), intense tropical cyclones of the western North Pacific, rank among the mo

219 imultaneously explored the direct impacts of cyclones on different life-history stages across the ann

220 ds, we track from 2000 to 2012 the impact of cyclones on economic activity in coastal regions inhabit

221 potentially increasing the predictability of cyclones on seasonal time scales.

222 Here we calculate the effect of tropical cyclones on surface ocean temperatures by comparing surf

223 ture data to explore the impacts of tropical cyclones on the survival of adult and juvenile (first ye

224 g via the gradual removal of taller trees by cyclones over many generations illustrates that cyclones

225 high precipitation associated with tropical cyclones over the last 120 years.

226 recent increase in the intensity of tropical cyclones over the northern Indian Ocean is thought to be

227 show that Asian pollution invigorates winter cyclones over the northwest Pacific, increasing precipit

228 When tropical cyclones pass over regions with barrier layers, the incr

229 eaker westerlies and increased Mediterranean cyclones penetrating northward at this time.

230 The number of tropical cyclones people had experienced moderated the strength o

231 nges in sea surface temperature and tropical cyclone 'potential intensity'--a measure that provides a

232 an the background equatorial warming, making cyclones potentially important modulators of the climate

233 Global statistics of tropical cyclone rainfall area are not expected to change markedl

234 ric model simulations, we show that tropical cyclone rainfall area is controlled primarily by its env

235 ives, yet little is known about how tropical cyclone rainfall area will change in the future.

236 Tropical cyclone rainfall rates have been projected to increase i

237 udies on regional and global scale, tropical cyclones' Rainfall erosivity is poorly assessed and have

238 adult Round Island petrels utilize the three cyclone regions of the Indian Ocean and were potentially

239 ensity and intensification of major tropical cyclones remains a challenge.

240 Accurately predicting future tropical cyclone risk requires understanding the fundamental cont

241 Improving a tropical cyclone's forecast and mitigating its destructive potent

242 ous environmental factors that influence the cyclone's path and intensity.

243 e generated aerosol were collected using the cyclone SASS 2300, suspended in buffer and then analyzed

244 h a robust size before the austral summer or cyclone season.

245 lones over many generations illustrates that cyclones shape forest structure through the accumulation

246 Thousands of cyclone shelters have been built and government and civi

247 s that the mean track of Cape Verde tropical cyclones shifted gradually north-eastward from the weste

248 Law") to the traveled distances of tropical cyclones since 1842.

249 dicated tight relationships between tropical cyclone size and mid-tropospheric relative humidity.

250 monthly snow accumulation was controlled by cyclone snowfall and 29% by sea-ice freeze-up.

251 Cyclone snowfall comprised ~50% of total snowfall in the

252 cific snow accumulation is more sensitive to cyclone strength.

253 y phenotypes, despite the fact that tropical cyclone strikes are irregular, occurring only every few

254 across the US using a high volume sequential cyclone system that collects PM in dry bulk form segrega

255 influences the yearly variations of tropical cyclone (TC) activities in both the Pacific and Atlantic

256 effectively modulate North Atlantic tropical cyclone (TC) activity in the following years.

257 Western North Pacific tropical cyclone (TC) activity is known to have a significant res

258 re climate change on North Atlantic tropical cyclone (TC) activity is of crucial societal importance,

259 ulation, and therefore could impact tropical cyclone (TC) activity.

260 The response of tropical cyclone (TC) destructive potential to global warming is

261 The severity of a tropical cyclone (TC) is often summarized by its lifetime maximum

262 Tropical cyclone (TC) is one of the earth's most hazardous disast

263 The 2018 tropical cyclone (TC) season over the western North Pacific (WNP)

264 Strong phytoplankton blooming in tropical-cyclone (TC) wakes over the oligotrophic oceans potentia

265 Tropical cyclone (TC) waves can severely damage coral reefs.

266 ng of the thermodynamic controls on tropical cyclone (TC) wind intensity, as well as numerical simula

267 e most destructive natural hazards, tropical cyclone (TC)-induced coastal flooding, will worsen under

268 Tropical cyclones (TC) are one of the most severe storm systems o

269 trasting rapid intensity changes in Tropical Cyclones (TC) Phailin and Lehar (2013) over the Bay of B

270 positive feedback mechanism between tropical cyclones (TCs) and climate warming can be seen by examin

271 ct on the frequency distribution of tropical cyclones (TCs) and its future change is studied using an

272 nfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer

273 tanding of the relationship between tropical cyclones (TCs) and their large-scale environments have r

274 Tropical cyclones (TCs) are among the most devastating weather sy

275 Tropical cyclones (TCs) are powerful agents of destruction, and u

276 Tropical cyclones (TCs) can have devastating socioeconomic impact

277 ities, it reminded us of the threat tropical cyclones (TCs) pose in the eastern North Pacific (ENP) a

278 The movement of tropical cyclones (TCs), particularly around the time of landfall

279 Tropical cyclones (TCs), some of the most influential weather eve

280 an (MAC) region is characterized by tropical cyclones (TCs), strong El Nino-Southern Oscillation even

281 es associated with U.S. landfalling tropical cyclones (TCs).

282 these often explosively developing mesoscale cyclones-termed polar lows-constitute a threat to offsho

283 The event was associated with cyclones that developed at lower latitudes.

284 Tropical cyclones that rapidly intensify are typically associated

285 tre cooling occurred beneath all 11 tropical cyclones that traversed the Mid-Atlantic Bight continent

286 n ocean thermal structure on future tropical cyclones, they did not take into account changes in near

287 ith a predicted shift in the distribution of cyclones toward higher intensities as climate warms, sug

288 upling the framework with synthetic tropical cyclone tracks and extension to the global scale.

289 Over the study period and area, tropical cyclones typically brought different hazards to differen

290 guing prospect that the projected changes in cyclones under current climate change scenarios may have

291 he thermal expansion of water in the wake of cyclones, using satellite-based sea surface height data

292 from deeper water and entrained by tropical cyclone waves and currents, in a shallow-water or terres

293 bservations recorded during a major tropical cyclone, we have estimated this momentum transfer from t

294 ecrease in the overall frequency of tropical cyclones, when the downscaling is based on the ensemble

295 be attributed to the WNP anomalous low-level cyclone, which is due primarily to El Nino Modoki and se

296 ss of this uncertainty, flooding by tropical cyclones will increase as a result of accelerated sea-le

297 Climate change scenarios predict tropical cyclones will increase in both frequency and intensity,

298 e stabilized, as losses due to bleaching and cyclones will otherwise increase.

299 We investigate tropical cyclone wind and storm surge damage reduction for five a

300 ocean has more energy to convert to tropical cyclone wind.

301 Particles are collected in a cyclone with water as the collection medium.