ライフサイエンスコーパス: cyclone

1 ing precipitation, temperature, and tropical cyclones.

2 increasingly prone to flooding from tropical cyclones.

3 ociated with anticipated floods and tropical cyclones.

4 ing the effect of global warming on tropical cyclones.

5 consequently, an intensification of tropical cyclones.

6 quency and tracks of North Atlantic tropical cyclones.

7 0.09 m s(-1) yr(-1) (s.e.) for the strongest cyclones.

8 nteractions dampen eddy-induced upwelling in cyclones.

9 with the vertical mixing induced by tropical cyclones.

10 rine boundary layer associated with tropical cyclones.

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

12 al resolution on track forecasts of tropical cyclones.

13 nerated by rainfall associated with tropical cyclones.

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

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

16 he need for better understanding of tropical cyclone activity apart from the records provided by mete

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

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

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

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

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

22 ate that instead of "unprecedented" tropical cyclone activity having occurred in recent years, hurric

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

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

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

26 The response of tropical cyclone activity to global warming is widely debated.

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

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

29 be considered in projecting future tropical cyclone activity.

30 late the vertical mixing induced by tropical cyclone activity.

31 eliable to reveal trends in intense tropical cyclone activity.

32 to improved long-range forecasts of tropical cyclone activity.

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

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

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

36 ubstantially longer time series for tropical cyclones affecting the continental United States does no

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

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

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

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

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

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

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

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

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

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

47 We examined the number of tropical cyclones and cyclone days as well as tropical cyclone in

48 creases have taken place while the number of cyclones and cyclone days has decreased in all basins ex

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

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

51 that, although plankton blooms occur in both cyclones and mode-water eddies, the biological responses

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

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

54 f power, integrated over the lifetime of the cyclone, and show that this index has increased markedly

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

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

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

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

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

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

61 Tropical cyclones are renowned for their destructive nature and a

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

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

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

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

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

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

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

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

70 Tropical cyclones cause extensive tree mortality and damage to fo

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

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

73 < 0.1) with observed variations in tropical-cyclone climatology, and that a substantial portion (32

74 7.1 megatonnes is due to a shift in tropical-cyclone climatology.

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

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

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

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

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

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

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

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

83 examined the number of tropical cyclones and cyclone days as well as tropical cyclone intensity over

84 taken place while the number of cyclones and cyclone days has decreased in all basins except the Nort

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

86 ming may lead to an upward trend in tropical cyclone destructive potential, and--taking into account

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

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

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

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

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

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

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

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

95 tanding the fundamental controls on tropical cyclone dynamics.

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

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

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

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

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

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

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

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

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

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

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

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

108 fy no allochthonous material associated with Cyclone Hamish.

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

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

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

112 Tropical cyclones have been hypothesized to influence climate by

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

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

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

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

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

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

119 temperatures and destructiveness by tropical cyclones in the Atlantic and western North Pacific basin

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

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

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

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

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

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

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

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

128 Coupled with a PM2.5 cyclone inlet and a membrane-based parallel plate denude

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

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

131 an environment more favourable for tropical cyclone intensification.

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

133 o substantially larger increases in tropical cyclone intensities.

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

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

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

137 yclones and cyclone days as well as tropical cyclone intensity over the past 35 years, in an environm

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

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

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

141 tion of recent historical trends in tropical cyclone intensity.

142 Increasingly, flood and cyclone interventions have leveraged community resilienc

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

144 of Lighthill's "sandwich model" of tropical cyclones is the existence of "ocean spray," a layer inte

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

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

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

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

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

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

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

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

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

154 ring oxygen isotope proxy record of tropical cyclone occurrence extending back many centuries based o

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

170 Tropical cyclone rainfall rates have been projected to increase i

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

172 In a second channel, a cyclone removes large particles and the aerosol stream i

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

196 Tropical cyclones (TCs) can have devastating socioeconomic impact

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

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

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

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

201 d by landfalling hurricanes--strong tropical cyclones that reach the coast.

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

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

204 lightly increasing the intensity of tropical cyclones through warming of sea surface temperatures.

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

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

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

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

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

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

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

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

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

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

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