ライフサイエンスコーパス: La Nina

1 e energy, the stronger (weaker) the El Nino (La Nina).

2 l of 6 storms (24.6 for El Nino and 18.6 for La Nina).

3 pacts are more robust following El Nino than La Nina.

4 nd it remains comparable between El Nino and La Nina.

5 t-year La Nina to persist into a second-year La Nina.

6 is what cause the switch between El Nino and La Nina.

7 le to predict the switch between El Nino and La Nina.

8 tion over the Tropical continents during the La Nina.

9 nvestigate the global impacts of El Nino and La Nina.

10 os is followed by a super El Nino and then a La Nina.

11 k and rainfall associated with the 2010-2011 La Nina.

12 an climate which has shifted from El Nino to La Nina.

13 to climate fluctuations dominated by El Nino/La Nina.

14 s (beach widening) are not similarly tied to La Ninas.

15 l Pacific during El Nino but warms it during La Nina(15,16).

16 f these OMZ air parcels are augmented during La Nina and decrease sharply during El Nino.

17 Between 2009 and 2016, La Nina and El Nino conditions were accompanied by sea s

18 The La Nina and El Nino phases of the El Nino-Southern Oscil

19 ents-over a twofold decline between a strong La Nina and strong El Nino for S. lewini.

20 The linkage between La Nina and western US stratospheric intrusions can be e

21 outhern Oscillation), with more events under La-Nina and less under El-Nino conditions.

22 l westerly ducts and subtropical jets during La-Nina and weaker during El-Nino.

23 That is, when the influences of El Nino/La Nina are strong enough to isolate more than 48% of th

24 e western portion of the ENP during El Nino (La Nina), but reduced (enhanced) TC frequency in the eas

25 La Nina climate anomalies have historically been associa

26 EN) events after ~11 ka: eastern Pacific EN, La Nina, coastal EN (COA), and central Pacific or Modoki

27 El Nino and La Nina, collectively referred to as the El Nino-Souther

28 Our results demonstrate that La Nina conditions are associated with cooler temperatur

29 We hypothesize that La Nina conditions bring divergent influenza subtypes to

30 ed to Australian ecosystems, where prevalent La Nina conditions caused up to six consecutive seasons

31 ate with stadials at high latitudes, whereas La Nina conditions correlate with interstadials.

32 most compatible with increased frequency of La Nina conditions during this interval.

33 Subsequent wetter La Nina conditions in boreal winter reverse the phase in

34 in boreal spring or summer, were preceded by La Nina conditions in the equatorial Pacific.

35 In turn, La Nina conditions lagged 0-5 months are associated with

36 cause of tropical inundation associated with La Nina conditions, consistent with trends in the GRACE

37 anic eruptions strengthen El Nino and weaken La Nina conditions, further enhancing Indian droughts.

38 ) central Pacific Ocean, particularly during La-Nina conditions.

39 Relative to single-year La Nina, consecutive La Nina features meridionally broad

40 , and a cyclical change from an El Nino to a La Nina dominate our measure of anthropogenic effects be

41 We use modern El Nino-La Nina dynamics and the Tropical Pacific Decadal Variab

42 y the first (second) type is associated with La Nina (El Nino) like conditions, suggesting that both

43 wever, inconsistencies exist between El Nino/La Nina (ENSO) cycles and precipitation in the historica

44 tremes as seen during historical consecutive La Nina episodes probably occur more frequently in the t

45 spanning a major El Nino event in 2015 and a La Nina event in 2022, observed varying oceanic conditio

46 s were not significantly enhanced during the La Nina event likely because increased stratification be

47 cific and was synchronous to a major El Nino/La Nina event that occurred between 1997 and 1999.

48 atmospheric forcing associated with a strong La Nina event.

49 dback, contributed to the development of the La Nina event.

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

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

52 stic forecasts for the occurrence of El Nino/La Nina events are also performed and assessed via infor

53 tion anomalies during historical El Nino and La Nina events by magnifying or weakening droughts and p

54 The irregular occurrence of El Nino and La Nina events has implications for public health.

55 ) cycle of alternating warm El Nino and cold La Nina events is the dominant year-to-year climate sign

56 tic ENSO cycle with intermittent El Nino and La Nina events of varying intensity and strength as well

57 hough most El Nino events last for one year, La Nina events often persist for 2-3 years.

58 La Nina events often result in a strengthened LC, high c

59 Future changes to multi-year-long La Nina events remain unknown.

60 n (ENSO)--in particular, extreme El Nino and La Nina events that modulate California's climate not on

61 r were sighted with greater frequency during La Nina events, and their abundance dropped considerably

62 Heat-stress events are more frequent during La Nina events, but occur under all climatic conditions,

63 rease in the frequency of strong El Nino and La Nina events, but the change differs vastly across mod

64 cillation, NTA warm anomalies tend to induce La Nina events, droughts in Northeast Brazil, increased

65 t intermittently triggers regular El Nino or La Nina events, super El Nino events, or no events at al

66 In the summers between consecutive La Nina events, the concurrent La Nina opposes the delay

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

68 nts to rapidly rising floods associated with La Nina events, which debouch extraordinary volumes of s

69 historical events, such as strong El Nino or La Nina events, with very little given information.

70 portant contribution to the 2020-2022 strong La Nina events.

71 tic variation in the sequence of El Nino and La Nina events.

72 onal-to-global associations with El Nino and La Nina events.

73 significantly higher values occurring during La Nina events.

74 erstood by analogy to historical El Nino and La Nina events: North Pacific tropical cyclone projectio

75 For years unaffected by strong El-Nino/La-Nina events, the Southeast monsoon wind strength over

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

77 ific cooling was modest, similar to observed La Nina excursions of 1(o) to 2 degrees C.

78 However, the 2021 La Nina exhibited a unique near-neutral impact on the CO

79 during the 1998 El Nino famine and the 1999 La Nina feast period.

80 Relative to single-year La Nina, consecutive La Nina features meridionally broader easterly winds and

81 he two end members of the cycle, El Nino and La Nina, force anomalous oceanographic conditions and co

82 slands (Malvinas) to Tristan da Cunha during La Nina found a more abundant and speciose seabird assem

83 shows a strong asymmetry between El Nino and La Nina impacts, with much larger amplitude and broader

84 Conversely, La Nina increases transmission potential in tropical AEZ

85 onstrate that the switch between El Nino and La Nina is caused by a subsurface ocean wave propagating

86 Nino is followed by a positive NAO, whereas La Nina is followed by a negative NAO.

87 e one phase of a natural mode of oscillation-La Nina is the complementary phase-that results from uns

88 La Nina leads to enhanced Atlantic Hadley cell and a pos

89 that Pinatubo-like eruptions tend to shorten La Ninas, lengthen El Ninos and induce anomalous warming

90 temperature (SST) trends resembling a strong La Nina-like cold condition and the negative phase of th

91 rease followed by a decrease-can sustain the La Nina-like condition for a longer time than expected.

92 This period is marked by a tendency for La Nina-like conditions in the tropical Pacific.

93 ase of the Arctic Oscillation, predominantly La Nina-like conditions, and variation in the position o

94 The GSWS was marked by a La Nina-like decadal cooling in the Pacific Ocean that s

95 A La Nina-like mean SST change intensifies basin-wide El N

96 ed with mid-Holocene cooling suggestive of a La Nina-like pattern with enhanced SST gradients and str

97 In addition to the shallow La Nina-like patterns in the Pacific that were the previ

98 of drying in southwest North America with a La Nina-like response creating a worst case scenario of

99 orial Atlantic, is known to remotely force a La Nina-like response in the Pacific, potentially affect

100 nes feedback and thus the development of the La Nina-like response.

101 model simulations of orbital forcing into a La Nina-like state at that time.

102 cooling of the east equatorial Pacific and a La Nina-like state, analogous to observations of a trans

103 Pacific, consistent with the prevalence of a La Nina-like state, rather than the proposed persistent

104 50 y show the opposite trend, toward a more La Nina-like state.

105 ulate BSISO propagation - with El Nino-like (La Nina-like) conditions favoring quasi-stationary (east

106 We find a generally wet (more La Nina-like) mid-Holocene that shifted towards drier an

107 ity, results from the reinforcing effects of La-Nina-like climate conditions and relative tropical At

108 climate variability, tied specifically to a La-Nina-like decadal cooling.

109 e significance of a strong El Nino preceding La Nina (LN) in the formation of multi-year LN events du

110 El Nino-Southern Oscillation (ENSO) phases (La Nina, neutral, and El Nino years) appear to be a weak

111 s the delayed effect of the preceding winter La Nina on the EASM, causing a reduction in the magnitud

112 ements to estimate the impact of this strong La Nina on the global atmospheric CH4 budget.

113 n consecutive La Nina events, the concurrent La Nina opposes the delayed effect of the preceding wint

114 , contradicting the paradigm of a persistent La Nina pattern.

115 During +SAM/La Nina periods, the at-depth overwintering period is sh

116 sea ice cover and decreased NPP during +SAM/La Nina periods.

117 and with positive anomalies occurring during La Nina periods.

118 o basin and are warmer/cooler during El Nino/La Nina periods.

119 s to date have been associated with the 1998 La Nina phase of ENSO.

120 vealed, across the US winter wheat belt, the La Nina phase of the El Nino Southern Oscillation (ENSO)

121 s asymmetry between warm (El Nino) and cold (La Nina) phases very poorly.

122 W), which intensify (weaken) during El Nino (La Nina), producing low-level anticyclonic (cyclonic) re

123 we argue that, in this case, a strong summer La Nina provided a window of opportunity to issue a much

124 e find an increased frequency of consecutive La Nina ranging from 19 +/- 11% in a low-emission scenar

125 ons and diatom contributions increase, while La Nina reverses that trend.

126 rn and central Pacific co-occurs with strong La Nina's.

127 sink in 2011 during the strongest sustained La Nina since 1917.

128 first half of 2011 experienced the strongest La Nina since the early 1980s, when global surface netwo

129 The El Nino La Nina Southern Oscillation (ENSO) exerts a significant

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

131 essential to correctly forecast the 2007/08 La Nina starting from April 2007.

132 ly unusual in that it took place with a weak La Nina state.

133 past two millennia to entrenched El Nino or La Nina states of the tropical Pacific.

134 ly and peak in a single winter(1-3), whereas La Nina tends to develop after an El Nino and last for t

135 n the equatorial Atlantic, which can trigger La Nina, the cold phase of El Nino-Southern Oscillation

136 Relative to the 2011 La Nina, the pantropical biosphere released 2.5 +/- 0.34

137 litates the cold anomalies of the first-year La Nina to persist into a second-year La Nina.

138 n be observed during rapid shifts from cold (La Nina) to warm (El Nino) conditions in that region.

139 tion that accompanied the largest El Nino to La Nina transition on record.

140 uction (NPP) responses to a major El Nino to La Nina transition.

141 Positive SOI values (La Nina type years) were a predictor of shorter wing cho

142 Consistently, during the 2017-2018 La Nina, unusually low SSTs in the same region contribut

143 en the positive PDO and negative ENSO (i.e., La Nina) was associated with peaks in annual SST.

144 unusually heavy cloud cover associated with La Nina, we installed high-intensity lamps above the for

145 e Indian Ocean Dipole (IOD) and co-occurring La Nina weaken the southeasterlies and cooling from coas

146 tropical wetland emissions during the strong La Nina were at least by 5% larger than the long-term me

147 The El Nino and La Nina were the main drivers for the periodical highest

148 La Ninas were generally associated with lower delta(18)O

149 super typhoons (7.1 for El Nino and 1.5 for La Nina) which nearly matches the mean response overall

150 re larger than the maximum cold anomalies of La Nina, which are centred in the equatorial central Pac

151 onally displaced in association with El Nino-La Nina wind-driven surface current variations.

152 ited States, such as occurs following strong La Nina winters (Nino3.4<-1.0 degrees C).

153 central Pacific (CP) El Nino as well as the La Nina with realistic features.

154 eviating from the typical pattern forced by "La Nina" with the maximum drying in the central and nort

155 0) across direct transitions from El Nino to La Nina, with statistically significant medium effects o

156 elation with adult growth chronologies, with La Nina years (characterised by warmer temperatures and

157 global-mean yields of all four crops during La Nina years tend to be below normal (-4.5 to 0.0%).

158 During La Nina years, maximum June temperatures were higher tha

159 malies of flood risk exist during El Nino or La Nina years, or both, in basins spanning almost half (

160 ty were lower in El Nino years and higher in La Nina years.

161 edging weights in the breeding grounds) than La Nina years.

162 tive growth patterns occurring during strong La Nina years.

163 ics doubles during El Nino years relative to La Nina years.