ライフサイエンスコーパス: El Nino

1 ver the Pacific Ocean, prevalently known as "El Nino".

2 rees C in response to the developing Pacific El Nino.

3 ge: 4.4-6.7 PgC) estimated for the 1997/1998 El Nino.

4 016 anomaly was caused by warming and 49% by El Nino.

5 ivity of pelagic fish to exploitation during El Nino.

6 variable climate conditions associated with El Nino.

7 fferent teleconnections from the traditional El Nino.

8 the positive Bjerknes feedback critical for El Nino.

9 current data including the extreme 1997-1998 El Nino.

10 orests throughout the dry season of the 2016 El Nino.

11 nded drought period associated with a strong El Nino.

12 emissions and natural phenomena such as the El Nino.

13 d during La Nina and decrease sharply during El Nino.

14 which was augmented by the strong 2015-2016 El Nino.

15 opical jets during La-Nina and weaker during El-Nino.

16 trend, punctuated by saline excursion during El Ninos.

17 varied markedly due to observed ENSO states: El Nino (2015) and neutral (2016-2017).

18 warming of West Antarctica, associated with El Nino activity.

19 Pacific Ocean mixed-layer thickness and both El Nino amplitude and central Pacific variability.

20 ent reconstructions of total variability and El Nino amplitude from individual foraminifera distribut

21 mean response is 5.6 super typhoons (7.1 for El Nino and 1.5 for La Nina) which nearly matches the me

22 mean response overall of 6 storms (24.6 for El Nino and 18.6 for La Nina).

23 xplore the relationships between hurricanes, El Nino and HABs in two Florida estuaries subject to rep

24 gnificant association was identified between El Nino and ID MME occurrence (Z = 0.28, p = .81).

25 El Nino and its effect on local meteorological condition

26 ces a realistic ENSO cycle with intermittent El Nino and La Nina events of varying intensity and stre

27 oject an increase in the frequency of strong El Nino and La Nina events, but the change differs vastl

28 El Nino and La Nina events, the extremes of ENSO climate

29 s anomalies shows a strong asymmetry between El Nino and La Nina impacts, with much larger amplitude

30 Here, we demonstrate that the switch between El Nino and La Nina is caused by a subsurface ocean wave

31 Historical levels of El Nino and La Nina span from -2sigma to +2sigma of the

32 The El Nino and La Nina were the main drivers for the period

33 El Nino and La Nina, collectively referred to as the El

34 The two end members of the cycle, El Nino and La Nina, force anomalous oceanographic condi

35 ey question is what cause the switch between El Nino and La Nina.

36 ed, but unable to predict the switch between El Nino and La Nina.

37 erature to investigate the global impacts of El Nino and La Nina.

38 y is known to have a significant response to El Nino and Southern Oscillation (ENSO).

39 es of 5-y CP El Ninos is followed by a super El Nino and then a La Nina.

40 eruptions tend to shorten La Ninas, lengthen El Ninos and induce anomalous warming when occurring dur

41 Strong El-Nino and positive Indian Ocean Dipole conditions are

42 in response to recurrent disturbances (like El Nino) and climatological and environmental perturbati

43 still simulates its asymmetry between warm (El Nino) and cold (La Nina) phases very poorly.

44 ular moderate traditional El Nino, the super El Nino, and the central Pacific (CP) El Nino as well as

45 Specifically, El Nino as an extreme climate event is known to have not

46 super El Nino, and the central Pacific (CP) El Nino as well as the La Nina with realistic features.

47 The super El Nino associated sub-seasonal signal of the East Asian

48 F successfully predicts the historic 2015/16 El Nino at initialization times as early as June 2015, w

49 re exhibiting stronger correlations with the El Nino basin and are warmer/cooler during El Nino/La Ni

50 damping cools the equatorial Pacific during El Nino but warms it during La Nina(15,16).

51 Models that better simulate the observed El Nino-CA precipitation teleconnection yield larger, an

52 has very likely been fueled by the 2015-2016 El Nino climate phenomenon affecting the region.

53 In Africa, El Nino conditions are associated with increased rainfal

54 amplitude and broader areas affected during El Nino conditions.

55 ith more events under La-Nina and less under El-Nino conditions.

56 Disease outbreaks in multiple El Nino-connected regions worldwide (including Southeast

57 acific site, potentially obscuring a volcano-El Nino connection suggested in previous studies.

58 low oxygen zones are predicted to expand and El Nino cycles change.

59 ) of the tropical Pacific but the impacts of El Nino cycles on this key source region are unknown.

60 B) in June was a key factor that impeded the El Nino development.

61 We used an El Nino drought event as a natural experiment to test wh

62 r seedling survival rates during the extreme El Nino drought of 2015-2016.

63 trees was disproportionately elevated under El Nino drought stress.

64 Across Borneo the 1997-1998 El Nino drought temporarily halted the carbon sink by in

65 nds were amplified during a 2015-2016 severe El Nino drought.

66 ure gradient in Panama that have experienced El Nino droughts.

67 ar Mode (low SAM) is significantly linked to El Nino during austral spring and summer, potentially pr

68 Recent research suggests that the 2014/15 El Nino (EN) event was stalled as a result of an unusual

69 the history of the "flavors" or varieties of El Nino (EN) events after ~11 ka: eastern Pacific EN, La

70 The extreme El Nino (EN) events in 1997/98 and 1982/83, referred to

71 ances, such as those caused by the 1997-1998 El Nino, ETP corals reefs have demonstrated regional per

72 ar pattern was observed during the 2015-2016 El Nino event during which time corals in the northern R

73 bal warming slowdown or hiatus after the big El Nino event in 1997/98 raises the questions of whether

74 isease outbreaks during the strong 2015-2016 El Nino event in relation to climate anomalies derived f

75 ll can be attributed to the concurrent super El Nino event in the tropical Pacific.

76 The powerful El Nino event of 2015-2016 - the third most intense sinc

77 atmospheric CO2 concentrations to the strong El Nino event of 2015-2016.

78 This coincided with the single El Nino event that occurred throughout the study period.

79 f bleaching was limited during the 2009-2010 El Nino event, in contrast to a similar 2004-2005 event,

80 across the globe during the recent 2015-2016 El Nino event, re-igniting research interest in how clim

81 from shifting eastward as seen in a typical El Nino event.

82 ea, likely favoured by the concurrent strong El Nino event.

83 associated with recovery from the 1982-1983 El Nino event.

84 cholera transmission, a relationship between El Nino events and cholera incidence is highly plausible

85 fied at both regional and global scales, and El Nino events are expected to become more severe based

86 El Nino events are often implicated in anomalously warm

87 seasonal forecasts for three recent extreme El Nino events by initialising the forecasts with observ

88 The occurrence of several El Nino events contributed to a lower decadal mean growt

89 ontrast, potential intensification of future El Nino events could negatively impact vital rates and p

90 show that biota respond differently to major El Nino events during positive or negative phases of the

91 It has been hypothesized that El Nino events facilitate eastward dispersal across this

92 TCZ air column and/or generated by triggered El Nino events may be responsible for the late winter we

93 Central Pacific El Nino events may become more frequent in coming decade

94 w) displayed positive excursion during major El Nino events of 1983, 1997/98 and 2015/16, indicating

95 Moreover, the impact of recent strong El Nino events on fire dynamics is not yet known.

96 The far-reaching impacts of central Pacific El Nino events on global climate differ appreciably from

97 y of Machala, following one of the strongest El Nino events on record.

98 The increase in the number of extreme El Nino events projected for the twenty-first century co

99 proximately 2.5-28% higher during years with El Nino events than those without.

100 El Nino events that produce large USWC warming, irrespec

101 ely caused by the interaction of these super El Nino events with the subtropical jet annual cycle.

102 sual SSTs in the Tropical Pacific (including El Nino events) and Atlantic were the main drivers of ex

103 ic trade winds, emergence of Central Pacific El Nino events, and weakening of the North Pacific Aleut

104 floodplain inundation, often associated with El Nino events, that have the lowest NEP and the highest

105 ges in atmospheric CO2 concentrations during El Nino events-a phenomenon inferred but not previously

106 d the cloudy conditions in the region during El Nino events.

107 ic responses cannot be detected for moderate El Nino events.

108 bility, thus favoring more frequent and weak El Nino events.

109 and the Oceanic Nino Index, an indicator of El Nino events.

110 that was distinctly different from previous El Nino events.

111 y lower food availability in years following El Nino events.

112 y from those associated with eastern Pacific El Nino events.

113 ing future droughts, usually associated with El Nino events.

114 ved to affect the evolution and diversity of El Nino events.

115 -sea column may also trigger Central Pacific El Nino events.

116 le landscape, capable of taking advantage of El Nino floodwaters as well as river water.

117 n framework, which uses seasonal climate and El Nino forecasts, allows a prediction to be made at the

118 In the 6-12 months preceding a flood, El Nino generates a positive precipitation anomaly over

119 mean annual fluxes for 2014, the most recent El Nino has contributed to an excess CO2 emission from t

120 s bracketing the cloud base during a severe, El Nino-impacted dry season.

121 have been partially attributed to the strong El Nino in 2015, however there is still a lack of fundam

122 Extreme climate events, such as the El Ninos in 1997/1998 and 2015/16, have led to considera

123 In the wake of the 2015-2016 El Nino-induced mass coral bleaching event, we quantifie

124 El Nino-induced thermal stress is considered the primary

125 The El Nino-influenced coral reefs in the central Gilbert Is

126 we show that the severity of droughts during El Nino is amplified (17%) by changes in aerosols.

127 We show that the strength of extreme El Nino is reduced with the warmer ocean mean state as a

128 e during the 1990s, where a series of 5-y CP El Ninos is followed by a super El Nino and then a La Ni

129 regions of localized activity vary from one El Nino (La Nina) event to another; still, some El Nino

130 Nino (La Nina) event to another; still, some El Nino (La Nina) events are more similar to each other.

131 ncy in the western portion of the ENP during El Nino (La Nina), but reduced (enhanced) TC frequency i

132 inds (CAGW), which intensify (weaken) during El Nino (La Nina), producing low-level anticyclonic (cyc

133 ed cyclone energy, the stronger (weaker) the El Nino (La Nina).

134 However, inconsistencies exist between El Nino/La Nina (ENSO) cycles and precipitation in the h

135 That is, when the influences of El Nino/La Nina are strong enough to isolate more than 4

136 improve the understanding and prediction of El Nino/La Nina events and also may be applied in the in

137 robabilistic forecasts for the occurrence of El Nino/La Nina events are also performed and assessed v

138 e El Nino basin and are warmer/cooler during El Nino/La Nina periods.

139 For years unaffected by strong El-Nino/La-Nina events, the Southeast monsoon wind stren

140 The 2015-2016 El Nino led to historically high temperatures and low pr

141 ontrasting with oceanic proxies that suggest El Nino-like conditions prevail during this period.

142 ool North Atlantic sea surface temperatures, El Nino-like conditions, and a negative phase of the Nor

143 poch analysis reveals a weak tendency for an El Nino-like response in the year after an eruption, but

144 ea interactions in the Pacific, favouring an El Nino-like response.El Nino tends to follow 2 years af

145 ) having relatively realistic NDH shows that El Nino-likeness of the equatorial-Pacific warming patte

146 The El Nino-low SAM relationship also weakens, implying the

147 low-level cyclone, which is due primarily to El Nino Modoki and secondarily to the positive phase of

148 Dipole, although the positive PMM phase and El Nino Modoki still hold.

149 During the 1982-1983 El Nino, most reefs in the Galapagos Islands collapsed,

150 on, sea surface temperature [SST] anomalies, El Nino occurrence).

151 ce those associated with the record breaking El Nino of 1997.

152 Launched just before one of the most intense El Ninos of the past century, OCO-2 measurements of [For

153 orcing and coastal response of the 2015-2016 El Nino, one of the strongest of the last 145 years.

154 ncompassing normal conditions, floods, a dry El Nino period, and a hurricane.

155 in drier climates), except during the drier El Nino period.

156 ts, with negative anomalies occurring during El Nino periods and with positive anomalies occurring du

157 increases in the intensity of hurricanes and El Nino periods predicted by climate change models have

158 wintering period is shorter compared to -SAM/El Nino periods, and return to the surface layers starts

159 In contrast to non-El Nino periods, these stronger in-weighted activities a

160 by increasing frequency and strength of the El Nino phase.

161 71-2013, with greater yields observed during El Nino phase.

162 The La Nina and El Nino phases of the El Nino-Southern Oscillation (ENSO

163 The roles that hurricanes and El Nino play in contributing to HAB events are examined

164 tmosphere system toward a moderate to strong El Nino--potentially an extreme event according to some

165 conclusions, pointing to inherent limits in El Nino predictability.

166 namical response linking volcanic cooling to El Nino remains ambiguous, Robock raises some important

167 on either the sign or physical mechanism of El Nino response to volcanism.

168 y wind anomalies in the Pacific favouring an El Nino response.

169 lcanic eruptions do not produce a detectable El Nino response.

170 e in rainfall associated with hurricanes and El Nino, resulting in enhanced nutrient loads which driv

171 eddy in July 2007 may have combined with the El Nino, resulting in temperatures surpassing 29 degrees

172 Africa in El Nino years, likely mediated by El Nino's impact on local climatic factors.

173 al and recovery elsewhere under intensifying El Nino scenarios.

174 itudes (34 degrees -40 degrees S), where the El Nino signal is weaker, snow cover losses appear to be

175 e PMM energizes the central tropical Pacific El Nino Southern Oscillation (CP-ENSO) and its atmospher

176 The El Nino Southern Oscillation (ENSO) and other climate pa

177 the periodicities of disease prevalence and El Nino Southern Oscillation (ENSO) cycles was examined

178 tropical forest carbon sink strength during El Nino Southern Oscillation (ENSO) events can indicate

179 As an example of such a remote effect, El Nino Southern Oscillation (ENSO) events in the equato

180 El Nino Southern Oscillation (ENSO) events modulate ocea

181 ribution, wind periodicity, the influence of El Nino Southern Oscillation (ENSO) events, and "shortes

182 ternative flooding regimes that occur during El Nino Southern Oscillation (ENSO) events.

183 El Nino Southern Oscillation (ENSO) has a strong influen

184 at climate change and intensification of the El Nino Southern Oscillation (ENSO) has increased variat

185 The El Nino Southern Oscillation (ENSO) has significant impa

186 Large-scale climate modes such as El Nino Southern Oscillation (ENSO) influence population

187 The El Nino Southern Oscillation (ENSO) is highly dependent

188 function analysis revealed influences of the El Nino Southern Oscillation (ENSO) on global groundwate

189 duce shifts in the non-stationary effects of El Nino Southern Oscillation (ENSO) on regional forest c

190 e strongly influenced by climate change, the El Nino Southern Oscillation (ENSO) phenomenon would be

191 or heat-stress events may be associated with El Nino Southern Oscillation (ENSO), but we highlight th

192 ing trend is mainly driven by changes in the El Nino Southern Oscillation (ENSO), especially at latit

193 South Pacific, known as "precursors" of the El Nino Southern Oscillation (ENSO), have been shown to

194 ear or decadal climate patterns, such as the El Nino Southern Oscillation (ENSO), might have on weath

195 count for large-scale oscillations including El Nino Southern Oscillation (ENSO), North Atlantic Osci

196 use of errors in predicting the amplitude of El Nino Southern Oscillation (ENSO)-driven sea surface t

197 s study provides the first long-term data on El Nino Southern Oscillation (ENSO)-driven synchrony of

198 ERS resulted from a synergy of the 1997/1998 El Nino Southern Oscillation (ENSO)-the strongest on rec

199 ted with the Southern Annular Mode (SAM) and El Nino Southern Oscillation (ENSO).

200 anographic anomalies, the "Blob" and extreme El Nino Southern Oscillation (ENSO).

201 opics play a key role in the dynamics of the El Nino Southern Oscillation (ENSO).

202 n Costa Rica, which occurred during the 2015 El Nino Southern Oscillation event.

203 quent natural disasters and question whether El Nino Southern Oscillation events should be approached

204 f spring temperature (local weather) and the El Nino Southern Oscillation index (a global climate cyc

205 The "El Nino Southern Oscillation" (ENSO) occurs irregularly

206 The MJO modulates the El Nino Southern Oscillation(1), tropical cyclones(2,3)

207 birth order and climatic fluctuations (e.g. El Nino Southern Oscillation) on calf survival.

208 tely related to climatic indices such as the El Nino Southern Oscillation, the Pacific Decadal Oscill

209 ith global meteorological cycles such as the El Nino Southern Oscillation.

210 rnia and Humboldt Systems is associated with El Nino Southern Oscillation.

211 and in situ observations, here we show that El Nino - Southern Oscillation (ENSO) is a main driver o

212 BP, the signal of El Nino-Southern Oscillation (ENSO) activity became erra

213 al understanding of the relationship between El Nino-Southern Oscillation (ENSO) and ENP TCs.

214 focus is the link between variations in the El Nino-Southern Oscillation (ENSO) and GMSL.

215 heric pressure fields, we determine that the El Nino-Southern Oscillation (ENSO) and the Southern Ann

216 The El Nino-Southern Oscillation (ENSO) and the variability

217 de use of Noah Land Surface Model (LSM), and El Nino-Southern Oscillation (ENSO) data in an autoregre

218 The evolution of the El Nino-Southern Oscillation (ENSO) during the Holocene

219 eriods of coral loss frequently occur during El Nino-Southern Oscillation (ENSO) events originating i

220 wledge systems supporting the application of El Nino-Southern Oscillation (ENSO) forecasts, including

221 Forecasting the El Nino-Southern Oscillation (ENSO) has been a subject o

222 El Nino-Southern Oscillation (ENSO) has been shown to af

223 istent modes of climate variability like the El Nino-Southern Oscillation (ENSO) has proven challengi

224 The La Nina and El Nino phases of the El Nino-Southern Oscillation (ENSO) have major impacts o

225 The El Nino-Southern Oscillation (ENSO) is the dominant inte

226 El Nino-Southern Oscillation (ENSO) is the dominant inte

227 The El Nino-Southern Oscillation (ENSO) is the dominant inte

228 The El Nino-Southern Oscillation (ENSO) is the main driver o

229 Understanding how the El Nino-Southern Oscillation (ENSO) may change with clim

230 m to community and ecosystem response to the El Nino-Southern Oscillation (ENSO) of 2015.

231 The impact of the El Nino-Southern Oscillation (ENSO) on CH4 emissions fro

232 er hand, the volcanically induced changes in El Nino-Southern Oscillation (ENSO) or sea-surface tempe

233 The El Nino-Southern Oscillation (ENSO) results from the ins

234 The El Nino-Southern Oscillation (ENSO) shapes global climat

235 The El Nino-Southern oscillation (ENSO) simulated in the Com

236 variability along the equatorial Pacific and El Nino-Southern Oscillation (ENSO) variability after 20

237 positively affected by meridional winds and El Nino-Southern Oscillation (ENSO), and negatively affe

238 and La Nina, collectively referred to as the El Nino-Southern Oscillation (ENSO), are not only highly

239 cyclone main developmental region (MDR), the El Nino-Southern Oscillation (ENSO), the North Atlantic

240 El Nino-Southern Oscillation (ENSO), which is one of the

241 The El Nino-Southern Oscillation (ENSO), which originates in

242 vents across the globe, are modulated by the El Nino-Southern Oscillation (ENSO).

243 the land carbon sink, driven largely by the El Nino-Southern Oscillation (ENSO).

244 and plants with climate indices, such as the El Nino-Southern Oscillation (ENSO).

245 y of the global [Formula: see text]O flux to El Nino-Southern Oscillation and anthropogenic stratific

246 y simulating the chlorophyll response to the El Nino-Southern Oscillation and capturing the winter re

247 te of atmospheric CO2 concentrations and the El Nino-Southern Oscillation are well known, the magnitu

248 e 2- to 8-year periodicity characteristic of El Nino-Southern Oscillation became evident in the recor

249 ce height that occurred during the 2015-2016 El Nino-Southern Oscillation event.

250 acterized by tropical cyclones (TCs), strong El Nino-Southern Oscillation events, and climate variabi

251 El Nino-Southern Oscillation has been treated as a disru

252 The El Nino-Southern Oscillation is the dominant mode of int

253 ate variability patterns associated with the El Nino-Southern Oscillation phenomenon result in climat

254 potential advantage of ocean salinity in the El Nino-Southern Oscillation prediction.

255 t that the glaciers' retreat is augmented by El Nino-Southern Oscillation processes, such as convecti

256 ay be driving an increase in central Pacific El Nino-Southern Oscillation variability and/or its hydr

257 The cyclicity is apparently linked to the El Nino-Southern Oscillation, against the background of

258 and three modes of climate variability (the El Nino-Southern Oscillation, Atlantic Multidecadal Osci

259 haracteristics and seasonality, links to the El Nino-Southern Oscillation, triggering processes and i

260 ary circulation patterns associated with the El Nino-Southern Oscillation.

261 rming simulations the combined impact of the El Nino/Southern Oscillation (ENSO) phenomenon and long-

262 ical Pacific variability associated with the El Nino/Southern Oscillation (ENSO).

263 tions ca. 2 ka were caused by changes in the El Nino/Southern Oscillation (ENSO).

264 ge mask the natural relationship between the El Nino/Southern Oscillation and AGB stocks in disturbed

265 ic, large-scale climate patterns such as the El Nino/Southern Oscillation and Pacific Decadal Oscilla

266 Impacts of climate modes such as El Nino/Southern Oscillation are evaluated.

267 d between the variability of the IOD and the El Nino/Southern Oscillation during the last millennium.

268 ic can provide conditions for an interannual El Nino/Southern Oscillation event to trigger a transiti

269 in the interannual range associated with the El Nino/Southern Oscillation is found to be distinguisha

270 sparate atmospheric phenomena, including the El Nino/Southern Oscillation, the North Atlantic Oscilla

271 mainly related to convection associated with El Nino/Southern Oscillation.

272 riability, and suggests the influence of the El Nino/Southern Oscillation.

273 strong interannual variability due to ENSO (El-Nino/Southern Oscillation), with more events under La

274 patterns allow coral to persist under these El Nino-stressed conditions, often recovering from these

275 urface temperature during the 2014/15 failed El Nino, suggesting some potential advantage of ocean sa

276 es in the mean circulation reminiscent of an El Nino teleconnection.

277 Pacific, favouring an El Nino-like response.El Nino tends to follow 2 years after volcanic eruptions

278 Here we show that an El Nino tends to peak during the year following large er

279 During El Nino, the anomalous overturning circulation from the

280 nteractions amongst three key climate modes (El Nino, the Indian Ocean dipole, and the southern annul

281 ulate the quasi-regular moderate traditional El Nino, the super El Nino, and the central Pacific (CP)

282 butions of long-term warming and the 2015-16 El Nino to the extreme April 2016 SATs.

283 This study investigates the 2014/15 failed El Nino using salinity from an ocean general circulation

284 caused by large volcanic eruptions may mask El Nino warming at our central Pacific site, potentially

285 cool the surface, thus masking the relative El Nino warming.

286 en the positive PDO and positive ENSO (i.e., El Nino) was associated with peaks in chlorophyll-a.

287 occur, even with temporary reprieves such as El Nino, we predict substantial future forest change.

288 ne temperatures were higher than Neutral and El Nino, whereas June precipitation was lower than El Ni

289 For example, the maximum warm anomalies of El Nino, which occur in the equatorial eastern Pacific O

290 dicate that the frequency of extreme coastal El Nino will increase under global warming.

291 Our analysis reveals that all super El Nino winters (1982/83, 1997/98, and 2015/16) were acc

292 bservations suggest that they also favour an El Nino within 2 years following the eruption.

293 arbler population growth was lower following El Nino years (which have been linked to poor survival i

294 Cholera incidence during El Nino years was higher in regions of East Africa with

295 on of cholera incidence throughout Africa in El Nino years, likely mediated by El Nino's impact on lo

296 in virtually all April extremes occur during El Nino years.

297 er solar radiation and lower rainfall during El Nino years.

298 almost 50,000 additional cases occur during El Nino years.

299 e Mocan, which in turn mitigated risk during El Nino years.

300 o, whereas June precipitation was lower than El Nino years.