ライフサイエンスコーパス: El Nino-southern oscillation

1 ce temperatures in the Bay of Bengal and the El Nino-Southern Oscillation).

2 me scale as demonstrated by responses to the El Nino Southern Oscillation.

3 imately tied to the impact of warming on the El Nino Southern Oscillation.

4 ding grounds varied with fluctuations in the El Nino Southern Oscillation.

5 cal marine ecosystems, African climates, and El Nino Southern Oscillation.

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

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

8 o the fluctuations in salinity driven by the El Nino-Southern Oscillation.

9 n and a shift to more negative phases of the El Nino-Southern Oscillation.

10 ociated with climate modes, particularly the El Nino-Southern Oscillation.

11 istically simulate Atlantic Nino's impact on El Nino-Southern Oscillation.

12 otranspiration is positively correlated with El Nino-Southern Oscillation.

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

14 nnual variability is strongly related to the El Nino/Southern Oscillation.

15 of forcing by external phenomena such as the El Nino/Southern Oscillation.

16 te of large-scale climate modes, such as the El Nino/Southern Oscillation.

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

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

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

20 sification is primarily attributed to a mega-El Nino/Southern Oscillation (a leading mode of interann

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

22 find that the action of climate variability (El Nino southern oscillation and flooding) is quite loca

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

24 state changes in the Arctic Oscillation and El Nino-Southern Oscillation and associated land-atmosph

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

26 mportant for understanding phenomena such as El Nino-Southern Oscillation and for interpreting deep o

27 Climate oscillations like the El Nino-Southern Oscillation and Pacific Decadal Oscilla

28 urning circulation, Arctic sea-ice coverage, El Nino-Southern Oscillation and Sun Spot numbers contri

29 c hurricane activity is greatly modulated by El Nino-Southern Oscillation and the Atlantic Meridional

30 odels in capturing extreme events, including El Nino-Southern Oscillation and upper ocean heat waves.

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

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

33 s associated with climate factors, including El Nino/Southern Oscillation and the Indian Ocean Dipole

34 c dynamics associated with variations in the El Nino/Southern Oscillation and the strength of the Wes

35 is therefore important to understand how the El Nino/Southern Oscillation and the West African monsoo

36 of temperature, snowpack, precipitation, the El-Nino/Southern Oscillation and the North Atlantic Osci

37 duced by climate anomalies from the Pacific (El Nino Southern Oscillation) and Indian Oceans (Indian

38 dent with diminished coherence between ENSO (El Nino Southern Oscillation) and rainfall.

39 hermal disruptions (e.g., marine heat waves, El Nino-Southern Oscillation) and shifts in ocean curren

40 on interannual timescales, controlled by the El Nino-Southern Oscillation, and is less pronounced ove

41 ere feedback explains why the last echoes of El Nino-Southern Oscillation are found in the IO-NWP in

42 l and reflected solar fluxes, the effects of El Nino-Southern Oscillation are minimized, and an indep

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

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

45 highlighted the occurrence and intensity of El Nino-Southern Oscillation as important drivers of the

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

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

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

49 ween the KE and the central tropical Pacific El Nino Southern Oscillation (CP-ENSO) leads to the obse

50 t is, the development of the central-Pacific El Nino-Southern Oscillation (CP-ENSO), the rapid deepen

51 clude that transient processes driven by the El Nino/Southern Oscillation cycle control the formation

52 interannual variability driven primarily by El Nino Southern Oscillation cycles.

53 r depth/UV-B exposure, is strongly linked to El Nino/Southern Oscillation cycles, underscoring the ro

54 gnificant variability is associated with the El Nino/Southern Oscillation cycles.

55 The further amplification of these El Nino-Southern Oscillation-driven contrasts by the Pac

56 om systematic changes that take place in the El Nino Southern Oscillation during the course of the so

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

58 cipitation changes are mainly related to the El Nino-Southern Oscillation, East Asian summer monsoon

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

60 The source of anomaly is linked to super El Nino Southern Oscillation (ENSO) (1997-1998)-induced

61 The associations between El Nino Southern Oscillation (ENSO) and heat stress was

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

63 ale climate modes of variability such as the El Nino Southern Oscillation (ENSO) and the Dipole Mode

64 sistent with climate dynamics related to the El Nino Southern Oscillation (ENSO) and the Pacific Deca

65 The El Nino Southern Oscillation (ENSO) creates strong varia

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

67 The El Nino Southern Oscillation (ENSO) during the Early Eoc

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

69 Since the 1980s, El Nino Southern Oscillation (ENSO) events have been mor

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

71 El Nino Southern Oscillation (ENSO) events modulate ocea

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

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

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

75 El Nino Southern Oscillation (ENSO) has been shown to re

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

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

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

79 fic temperature gradients connected with the El Nino Southern Oscillation (ENSO) influence the Walker

80 El Nino Southern Oscillation (ENSO) is a climate event t

81 The El Nino Southern Oscillation (ENSO) is a climate mode in

82 The El Nino Southern Oscillation (ENSO) is a principal compo

83 The El Nino Southern Oscillation (ENSO) is a semi-periodic f

84 The El Nino Southern Oscillation (ENSO) is Earth's dominant

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

86 El Nino Southern Oscillation (ENSO) is the most dominant

87 The El Nino Southern Oscillation (ENSO) is the most prominen

88 Long-term meteorologic forecasting using El Nino Southern Oscillation (ENSO) may assist in antici

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

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

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

92 sized impacts and strongly contribute to the El Nino Southern Oscillation (ENSO) warm/cold phase asym

93 ydrological system (represented by the GWL), El Nino Southern Oscillation (ENSO), and IOD+ are teleco

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

95 In the year after an El Nino Southern Oscillation (ENSO), captures of P. mani

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

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

98 winter wheat belt, the La Nina phase of the El Nino Southern Oscillation (ENSO), increased abandonme

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

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

101 Large-scale climate variables include El Nino Southern Oscillation (ENSO), Southern Oscillatio

102 A primary example is the El Nino Southern Oscillation (ENSO), the dominant mode o

103 In the Pacific, the dominant climate mode is El Nino Southern Oscillation (ENSO), which has known a r

104 We assessed El Nino Southern Oscillation (ENSO)-derived thermal anom

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

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

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

108 ore frequent and intense fluctuations in the El Nino Southern Oscillation (ENSO).

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

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

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

112 Here, we studied the influence of El Nino Southern Oscillations (ENSO) on Hg concentration

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

114 We reconstructed sea surface temperature, El Nino-Southern Oscillation (ENSO) activity, and the tr

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

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

117 reef growth was increased variability of the El Nino-Southern Oscillation (ENSO) and its coupling wit

118 e demonstrate how the opposing forces of the El Nino-Southern Oscillation (ENSO) and levels of atmosp

119 ts that the inverse relationship between the El Nino-Southern Oscillation (ENSO) and the Indian summe

120 , we demonstrate the combined impacts of the El Nino-Southern Oscillation (ENSO) and the Madden-Julia

121 peratures and two major circulation features-El Nino-Southern Oscillation (ENSO) and the North Atlant

122 Modulated by El Nino-Southern Oscillation (ENSO) and the North Atlant

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

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

125 Global and regional impacts of El Nino-Southern Oscillation (ENSO) are sensitive to the

126 reme precipitation indices are influenced by El Nino-Southern Oscillation (ENSO) at a seasonal scale.

127 It is hypothesized that the 1991-1992 El Nino-southern oscillation (ENSO) caused increased pre

128 The El Nino-Southern Oscillation (ENSO) cycle of alternating

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

130 The El Nino-Southern Oscillation (ENSO) drives large changes

131 ure changes in the seasonal evolution of the El Nino-Southern Oscillation (ENSO) during its onset and

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

133 ature of tropical Pacific Ocean that reflect El Nino-Southern Oscillation (ENSO) dynamics that is obj

134 antic (NTA) during boreal spring can trigger El Nino-Southern Oscillation (ENSO) events in the follow

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

136 The most predictable components of the El Nino-Southern Oscillation (ENSO) evolution in real-ti

137 Additionally, we show how El Nino-Southern Oscillation (ENSO) extreme events disru

138 El Nino-Southern Oscillation (ENSO) features strong warm

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

140 Nino-4 index, a measure of the status of the El Nino-Southern Oscillation (ENSO) had the highest corr

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

142 ential for explosive volcanism to affect the El Nino-Southern Oscillation (ENSO) has been debated sin

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

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

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

146 PP were pronounced in tropical regions where El Nino-Southern Oscillation (ENSO) impacts on upwelling

147 es likely due to increased amplitudes of the El Nino-Southern Oscillation (ENSO) in a warming climate

148 The role of El Nino-Southern Oscillation (ENSO) in greenhouse warmin

149 1-year lagged extratropical response to the El Nino-Southern Oscillation (ENSO) in observational ana

150 modelling evidence of the essential role of El Nino-Southern Oscillation (ENSO) in shaping this chan

151 We further find a clear signature of the El Nino-Southern Oscillation (ENSO) in the record, with

152 e Universal Thermal Climate Index (UTCI) and El Nino-Southern Oscillation (ENSO) indices for the stud

153 Here, we revealed the El Nino-Southern Oscillation (ENSO) influence on gaseous

154 The El Nino-Southern Oscillation (ENSO) influences climate v

155 Although the El Nino-Southern Oscillation (ENSO) is a key driver of g

156 The El Nino-Southern Oscillation (ENSO) is a key driver of g

157 The El Nino-Southern Oscillation (ENSO) is a key ocean-atmos

158 El Nino-Southern Oscillation (ENSO) is a major source of

159 The El Nino-Southern Oscillation (ENSO) is known to respond

160 Improving the prediction skill of El Nino-Southern Oscillation (ENSO) is of critical impor

161 The El Nino-Southern Oscillation (ENSO) is one of the most i

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

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

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

165 El Nino-Southern Oscillation (ENSO) is the dominant mode

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

167 The El Nino-Southern Oscillation (ENSO) is the most potent s

168 El Nino-Southern Oscillation (ENSO) is the strongest int

169 El Nino-Southern Oscillation (ENSO) markedly affects the

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

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

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

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

174 El Nino-Southern Oscillation (ENSO) over the tropical Pa

175 El Nino-Southern Oscillation (ENSO) phases (La Nina, neu

176 El Nino events, the warm phase of the El Nino-Southern Oscillation (ENSO) phenomenon, amplify

177 The El Nino-Southern Oscillation (ENSO) phenomenon, the most

178 The El Nino-Southern Oscillation (ENSO) provides most of the

179 That Western and Eastern tropical Pacific El Nino-Southern Oscillation (ENSO) records differ is an

180 Understanding El Nino-Southern Oscillation (ENSO) response to past cli

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

182 The El Nino-Southern Oscillation (ENSO) shapes extreme weath

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

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

185 Despite decades of effort, predicting the El Nino-Southern Oscillation (ENSO) since the 2000s has

186 ) band of enhanced variability suggestive of El Nino-Southern Oscillation (ENSO) teleconnections into

187 Understanding the response of the El Nino-Southern Oscillation (ENSO) to global warming re

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

189 certainty surrounding the future response of El Nino-Southern Oscillation (ENSO) variability to anthr

190 Seasonal and El Nino-Southern Oscillation (ENSO) warming result in si

191 Atlantic Nino is the Atlantic equivalent of El Nino-Southern Oscillation (ENSO), and it has prominen

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

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

194 d acute temperature anomalies, caused by the El Nino-Southern Oscillation (ENSO), at Cocos Island, Co

195 including the Indian Ocean Dipole (IOD) and El Nino-Southern Oscillation (ENSO), can strongly affect

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

197 The El Nino-Southern Oscillation (ENSO), the primary driver

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

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

200 volcanic eruptions through thermodynamic and El Nino-Southern Oscillation (ENSO)-like dynamic process

201 C strength also alter the variability of the El Nino-Southern Oscillation (ENSO).

202 y is dominated today by the influence of the El Nino-Southern Oscillation (ENSO).

203 ocean/atmosphere system analogous to modern El Nino-Southern Oscillation (ENSO).

204 nnual component at the dominant frequency of El Nino-Southern Oscillation (ENSO).

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

206 cean-atmosphere interactions associated with El Nino-Southern Oscillation (ENSO).

207 livelihoods, is significantly influenced by El Nino-Southern Oscillation (ENSO).

208 ern in UT O(3) is mainly associated with the El Nino-Southern Oscillation (ENSO).

209 scales, the tropical Pacific is home to the El Nino-Southern Oscillation (ENSO).

210 which can trigger La Nina, the cold phase of El Nino-Southern Oscillation (ENSO).

211 between terrestrial water storage (TWS) and El Nino-Southern Oscillation (ENSO).

212 southeastern China that is modulated by the El Nino-Southern Oscillation (ENSO).

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

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

215 an Pattern (PNA), North Pacific Index (NPI), El Nino-Southern Oscillation (ENSO)] to explain decadal-

216 debate about how the IOD interacts with the El Nino/Southern Oscillation (ENSO) and the Asian monsoo

217 ial Pacific iron limitation through multiple El Nino/Southern Oscillation (ENSO) cycles, but that thi

218 The variability of El Nino/Southern Oscillation (ENSO) during the Holocene

219 Although the El Nino/Southern Oscillation (ENSO) often affects season

220 The El Nino/Southern Oscillation (ENSO) originates in the tr

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

222 The El Nino/Southern Oscillation (ENSO) phenomenon is believ

223 ere we present support for a response of the El Nino/Southern Oscillation (ENSO) phenomenon to forcin

224 the full range of natural variability in the El Nino/Southern Oscillation (ENSO) phenomenon.

225 Today, the El Nino/Southern Oscillation (ENSO) system is the primar

226 seasonal temperature and precipitation, the El Nino/Southern Oscillation (ENSO), and the Pacific Dec

227 secular changes in the dominant mode of the El Nino/Southern Oscillation (ENSO), the primary driver

228 interannual mode of the modern climate, the El Nino/Southern Oscillation (ENSO).

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

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

231 troposphere/lower stratosphere via the Ozone El-Nino Southern Oscillations (ENSO) Index (OEI).

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

233 egions worldwide where the leading tropical (El Nino-Southern Oscillation, ENSO) and polar (Arctic Os

234 DAR surveys spanning the hot and dry 2015-16 El Nino Southern Oscillation event to measure canopy hei

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

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

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

238 -in spite of the coincidence with the strong El Nino/Southern Oscillation event-may primarily be an e

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

240 between reductions in annual precipitation, El Nino southern oscillation events, and photosynthetic

241 iance in dry season moisture associated with El Nino Southern Oscillation events.

242 Recently, changes in El Nino-Southern Oscillation events have had a detectabl

243 ferential social response to both transient (El Nino-Southern Oscillation events) and protracted (des

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

245 to 2-month period every 3 to 4 years during El Nino-Southern Oscillation events.

246 such as eustatic sea-level rise and periodic El Nino-Southern Oscillation events.

247 ENSO (El Nino Southern Oscillation) events are becoming more f

248 o multiyear) regional climatic cycles (e.g., El Nino Southern Oscillation)--except when extreme phase

249 h the Indian Ocean Zonal Mode (IOZM) and the El Nino Southern Oscillation exert strong influence on i

250 mate variability, which explains part of the El Nino Southern Oscillation flavours, can be predicted

251 riation in dengue cases can be attributed to El Nino-Southern Oscillation fluctuations, with higher v

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

253 Changes in the phase of the El Nino-Southern Oscillation have been shown to alter th

254 ate modes like the Southern Annular Mode and El Nino-Southern Oscillation, highlight the Southern Oce

255 s to the Lorenz 96 multiscale system and the El Nino Southern Oscillation in a climate model show pro

256 o interannual climate variability related to El Nino southern oscillation in the Mojave Desert.

257 e during an extreme drought event during the El Nino-Southern Oscillation in 2015.

258 resulted from an increasing frequency of the El Nino-Southern Oscillation in the context of weakened

259 ed to the Pacific Decadal Oscillation and to El Nino-Southern Oscillation in the Pacific Ocean.

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

261 e Southern Oscillation Index, an atmospheric El Nino-Southern Oscillation Index.

262 tivity and elevated precipitation related to El Nino southern oscillation indicate this model may be

263 ighly correlated with all India rainfall and El Nino-Southern Oscillation indices.

264 it is correlated with the previous winter's El Nino-Southern Oscillation indices.

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

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

267 pendence encountered in key statistics of an El-Nino-Southern Oscillation model of intermediate compl

268 evidence that shows that dynamical patterns (El Nino/Southern Oscillation, North Atlantic Oscillation

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

270 e related to apparent intensification of the El Nino Southern Oscillation over this interval and its

271 to variations in temperature, rainfall, and El Nino Southern Oscillation patterns.

272 ts of age, sex, group size, seasonality, and El Nino-Southern Oscillation phases, we show low to mode

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

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

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

276 es, possibly through a system similar to how El Nino/Southern Oscillation regulates the poleward flux

277 El Nino/Southern Oscillation related climate anomalies w

278 s related to global climate change (not only El Nino Southern Oscillation-related marine heatwaves, w

279 The positive phase of the 2015-2016 El Nino Southern Oscillation resulted in unprecedented h

280 Consequently, the El Nino-Southern Oscillation shifts eastward, intensifyi

281 ted to large rainfall variability due to the El Nino/Southern Oscillation sub-Saharan Africa and spra

282 oss scales: climate or long-term change, the El Nino-Southern Oscillation, synoptic high-pressure sys

283 dal variability in other regions with strong El Nino-Southern Oscillation teleconnections.

284 r availability anomalies driven by shifts in El Nino/Southern Oscillation teleconnections, including

285 ing modes of climate variability such as the El Nino-Southern Oscillation that also influence fire we

286 thetic problems and on the prediction of the El Nino Southern Oscillation, the dominant interannual m

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

288 rts on improving the long-term prediction of El Nino-Southern Oscillation, the predictability in stat

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

290 e of these currents-in processes such as the El Nino/Southern Oscillation, the Pacific Decadal Oscill

291 ial result of changes in the strength of the El-Nino Southern Oscillation, the region experienced sho

292 he LC, together with a reconstruction of the El Nino-Southern Oscillation to hindcast historical SST

293 In this perspective, we use forecasts of the El Nino-Southern-Oscillation to outline the impact of bi

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

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

296 Hemisphere westerly wind reconstructions and El Nino/Southern Oscillation variability indicate that p

297 ce the strength and rate of evolution of the El Nino Southern Oscillation which, in turn, determines

298 portant driver of climate variability is the El Nino Southern Oscillation, which can trigger disaster

299 related to climatic oscillations such as the El Nino-Southern Oscillation, while heatwaves occur irre

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