ライフサイエンスコーパス: La Nina

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

2 tion over the Tropical continents during the La Nina.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

22 atmospheric forcing associated with a strong La Nina event.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

54 and with positive anomalies occurring during La Nina periods.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

78 tive growth patterns occurring during strong La Nina years.

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

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