L.: A permanent El Nino-like state during the Pliocene?, Paleoceanography, 22, PA1213, doi:10.1029/2006PA001323, 2007.Haywood, A. M., Valdes, P. J., and Peck, V. L.: A permanent El Nin藴 o-like state during the Pliocene?, Paleoceanography, 22, PA1213, doi:10.1029/20...
western Pacific for H-wEN (Supplementary Fig.8a–c). In contrast, the group L models project El Niño-like tropical warming only regardless of ENSO amplitude change (Figs.6band7g–i). The mean NDH change following the ENSO amplitude change in group H (Fig.6a) leads to an east-west ...
models of dichotomic and polytomic logistic regression are applied to series of historical records spanning one and a half centuries (1840-1990) of the north atlantic seesaw (nas) and el ni?o (en), looking for simultaneous occurrence of both phenomena during the northern winter months and class...
carbon isotope data from a 1-Myr marine record in the southeastern subtropical Pacific with records from the equatorial Pacific and Southern Ocean in order to reconstruct sea surface circulation in this part of the world ocean and its possible link to the El Ni帽o/Southern Oscillation (ENSO). ...
Impacts of the ocean lateral diffusion on the El Niño/Southern Oscillation–like variability of a global coupled general circulation - Raynaud, Speich, et al.Raynaud, S., S. Peich, E. Guilyardi, and G. Madec (2000). Im- pacts of the ocean lateral diffusion on the El Nin˜o ...
The cooling over tropical land is connected with the mean state changes of the coupled system, including a shift in the land/sea partitioning of precipitation toward the oceans, a more westerly wind stress over the tropical Pacific, and a more El Ni卤o-like mean state of the tropical ...
Scientists would like to know what will happen to ENSO variability as the world's climate warms. To find out, some have looked to the mid-Piacenzian Warm Period (mPWP), a period about 3.26–3.03 million years ago that was approximately 3掳C warmer than the present day and that may be...
El-Niño and La-Niña are believed to change the intensity and frequencies of extreme weather events globally. The present study aims to analyse the impact of El-Niño and La-Niña on the lightning activities of cloud systems and their associated
The influence of El Niño–Southern Oscillation (ENSO) on productivity at upwelling systems has been extensively studied. However, in recent decades, ENSO diversity has been documented; there are more frequent events with anomalies in the central Pacif
However, other structurally dependent life forms like epiphytes and non-woody climbers or ground herbs have been studied very little with respect to their susceptibility to drought, associated with El Niño events. Such events are predicted to increase in intensity and frequency [10] and to ...