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1 ce temperatures in the Bay of Bengal and the El Nino-Southern Oscillation).
2 ding grounds varied with fluctuations in the El Nino Southern Oscillation.
3 ith global meteorological cycles such as the El Nino Southern Oscillation.
4 me scale as demonstrated by responses to the El Nino Southern Oscillation.
5 imately tied to the impact of warming on the El Nino Southern Oscillation.
6 ary circulation patterns associated with the El Nino-Southern Oscillation.
7 mainly related to convection associated with El Nino/Southern Oscillation.
8 nnual variability is strongly related to the El Nino/Southern Oscillation.
9 of forcing by external phenomena such as the El Nino/Southern Oscillation.
10 sification is primarily attributed to a mega-El Nino/Southern Oscillation (a leading mode of interann
11 find that the action of climate variability (El Nino southern oscillation and flooding) is quite loca
12 state changes in the Arctic Oscillation and El Nino-Southern Oscillation and associated land-atmosph
13 mportant for understanding phenomena such as El Nino-Southern Oscillation and for interpreting deep o
14 ge mask the natural relationship between the El Nino/Southern Oscillation and AGB stocks in disturbed
15 c dynamics associated with variations in the El Nino/Southern Oscillation and the strength of the Wes
16 is therefore important to understand how the El Nino/Southern Oscillation and the West African monsoo
17 duced by climate anomalies from the Pacific (El Nino Southern Oscillation) and Indian Oceans (Indian
18 ere feedback explains why the last echoes of El Nino-Southern Oscillation are found in the IO-NWP in
19 l and reflected solar fluxes, the effects of El Nino-Southern Oscillation are minimized, and an indep
20 te of atmospheric CO2 concentrations and the El Nino-Southern Oscillation are well known, the magnitu
21 highlighted the occurrence and intensity of El Nino-Southern Oscillation as important drivers of the
22 e 2- to 8-year periodicity characteristic of El Nino-Southern Oscillation became evident in the recor
23 t is, the development of the central-Pacific El Nino-Southern Oscillation (CP-ENSO), the rapid deepen
24 clude that transient processes driven by the El Nino/Southern Oscillation cycle control the formation
26 r depth/UV-B exposure, is strongly linked to El Nino/Southern Oscillation cycles, underscoring the ro
28 cipitation changes are mainly related to the El Nino-Southern Oscillation, East Asian summer monsoon
31 sistent with climate dynamics related to the El Nino Southern Oscillation (ENSO) and the Pacific Deca
33 the periodicities of disease prevalence and El Nino Southern Oscillation (ENSO) cycles was examined
34 tropical forest carbon sink strength during El Nino Southern Oscillation (ENSO) events can indicate
36 ribution, wind periodicity, the influence of El Nino Southern Oscillation (ENSO) events, and "shortes
38 at climate change and intensification of the El Nino Southern Oscillation (ENSO) has increased variat
45 Long-term meteorologic forecasting using El Nino Southern Oscillation (ENSO) may assist in antici
46 e strongly influenced by climate change, the El Nino Southern Oscillation (ENSO) phenomenon would be
48 use of errors in predicting the amplitude of El Nino Southern Oscillation (ENSO)-driven sea surface t
49 ERS resulted from a synergy of the 1997/1998 El Nino Southern Oscillation (ENSO)-the strongest on rec
52 We reconstructed sea surface temperature, El Nino-Southern Oscillation (ENSO) activity, and the tr
54 reef growth was increased variability of the El Nino-Southern Oscillation (ENSO) and its coupling wit
55 e demonstrate how the opposing forces of the El Nino-Southern Oscillation (ENSO) and levels of atmosp
56 ts that the inverse relationship between the El Nino-Southern Oscillation (ENSO) and the Indian summe
57 peratures and two major circulation features-El Nino-Southern Oscillation (ENSO) and the North Atlant
64 wledge systems supporting the application of El Nino-Southern Oscillation (ENSO) forecasts, including
65 Nino-4 index, a measure of the status of the El Nino-Southern Oscillation (ENSO) had the highest corr
66 istent modes of climate variability like the El Nino-Southern Oscillation (ENSO) has proven challengi
67 PP were pronounced in tropical regions where El Nino-Southern Oscillation (ENSO) impacts on upwelling
78 That Western and Eastern tropical Pacific El Nino-Southern Oscillation (ENSO) records differ is an
80 ) band of enhanced variability suggestive of El Nino-Southern Oscillation (ENSO) teleconnections into
82 variability along the equatorial Pacific and El Nino-Southern Oscillation (ENSO) variability after 20
89 an Pattern (PNA), North Pacific Index (NPI), El Nino-Southern Oscillation (ENSO)] to explain decadal-
90 debate about how the IOD interacts with the El Nino/Southern Oscillation (ENSO) and the Asian monsoo
93 rming simulations the combined impact of the El Nino/Southern Oscillation (ENSO) phenomenon and long-
95 ere we present support for a response of the El Nino/Southern Oscillation (ENSO) phenomenon to forcin
98 seasonal temperature and precipitation, the El Nino/Southern Oscillation (ENSO), and the Pacific Dec
99 secular changes in the dominant mode of the El Nino/Southern Oscillation (ENSO), the primary driver
105 ic can provide conditions for an interannual El Nino/Southern Oscillation event to trigger a transiti
106 -in spite of the coincidence with the strong El Nino/Southern Oscillation event-may primarily be an e
107 between reductions in annual precipitation, El Nino southern oscillation events, and photosynthetic
110 ferential social response to both transient (El Nino-Southern Oscillation events) and protracted (des
113 o multiyear) regional climatic cycles (e.g., El Nino Southern Oscillation)--except when extreme phase
114 h the Indian Ocean Zonal Mode (IOZM) and the El Nino Southern Oscillation exert strong influence on i
115 mate variability, which explains part of the El Nino Southern Oscillation flavours, can be predicted
118 f spring temperature (local weather) and the El Nino Southern Oscillation index (a global climate cyc
120 tivity and elevated precipitation related to El Nino southern oscillation indicate this model may be
124 pendence encountered in key statistics of an El-Nino-Southern Oscillation model of intermediate compl
125 evidence that shows that dynamical patterns (El Nino/Southern Oscillation, North Atlantic Oscillation
126 e related to apparent intensification of the El Nino Southern Oscillation over this interval and its
127 es, possibly through a system similar to how El Nino/Southern Oscillation regulates the poleward flux
129 ted to large rainfall variability due to the El Nino/Southern Oscillation sub-Saharan Africa and spra
131 rts on improving the long-term prediction of El Nino-Southern Oscillation, the predictability in stat
132 sparate atmospheric phenomena, including the El Nino/Southern Oscillation, the North Atlantic Oscilla
133 e of these currents-in processes such as the El Nino/Southern Oscillation, the Pacific Decadal Oscill
134 he LC, together with a reconstruction of the El Nino-Southern Oscillation to hindcast historical SST
135 ay be driving an increase in central Pacific El Nino-Southern Oscillation variability and/or its hydr
136 Hemisphere westerly wind reconstructions and El Nino/Southern Oscillation variability indicate that p
137 portant driver of climate variability is the El Nino Southern Oscillation, which can trigger disaster
138 strong interannual variability due to ENSO (El-Nino/Southern Oscillation), with more events under La
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