Attendance Time: Tuesday, 4 May 2010, 17:30–19:00
Chairperson: Eric Guilyardi
Paleo ENSO session
Hall XL
XL262
EGU2010-10120 Explaining a perpetual Pliocene El Niño with enhanced organized convective activity Nathan Arnold and Eli Tziperman
XL263
EGU2010-8581 The changes of equatorial-tropical teleconnection on the Warm Pool during the last century revealed by coral records Anne Juillet-Leclerc and Sylvie Thiria
XL264
EGU2010-10124 Seasonal and interannual variations of tropical Pacific induced by insolation changes in the early and middle Holocene yihua luan, pascale Braconnot, and yongqiang yu
XL265
EGU2010-11430 Influence of orbitally-induced climate change on the occurrence of the Central Pacific El Niño O. Salau, W. Park, M. Latif, and B. Schneider
XL266
EGU2010-13632 ENSO variability from mid- to late Holocene and the Seasonal Cycle of SST off Peru Paul Loubere, Kate Volk, and Jennifer Cumpston
XL267
EGU2010-3471 Relationships between El Niño-Southern Oscillation and nitrogen concentrations in a Western Mediterranean river J. Sigro, T. Vegas-Vilarrúbia, S. Giralt, and M. Brunet
General ENSO session
XL268
EGU2010-4318 Interdecadal change of the types of El Nino in GFDL CM2.1 Soon-Il An, Jung Choi, and Jong-Seong Kug
XL269
EGU2010-2414 El Niño and La Niña amplitude asymmetry caused by atmospheric feedbacks Claudia Frauen and Dietmar Dommenget
EGU2010-3001 Convective control of ENSO simulated in MIROC5 Masahiro Watanabe, Masahide Kimoto, Yukiko Imada, and Minoru Chikira
XL272
EGU2010-7725 Scale Interaction between Tropical Instability Waves and Oceanic Mean Flows Jong-Seong KUG, Yoo-Geun Ham, Fei-Fei Jin, and In-Sik Kang
XL273
EGU2010-1744 El Nino Southern Oscillation as Sporadic Oscillations between Metastable States
Tian Ma and Shouhong Wang
XL274
EGU2010-2983 The Slab Ocean El Nino Dietmar Dommenget
XL275
EGU2010-8504 El Niño in a warming world: Transient and equilibrium responses to enhanced atmospheric greenhouse gases Steven Phipps
XL276
EGU2010-8696 The ENSO related Pacific equatorial currents variability in a global ocean circulation model forced by the ERA-40 data HYOUN-WOO KANG and Ok Hee Seo