Fig. 4.• hematic Power S• cua of Variations in• e• ng• of t• Day. observed solid Earth
nutations, and to determine the non-hydrostatic part of the Core-Mantle Boundary (CMB) …

El Niño‐Southern Oscillation (ENSO) periods, which occur irregularly every few years, are a
major perturbation of the Earth's climate system that involves large‐scale changes in winds …

Tropical Pacific Sea Surface Temperature Anomalies, El Niño, and Equatorial Westerly Wind
Events in: Journal of Climate Volume 13 Issue 11 (2000) Jump to Content Logo Logo Logo …

Radiocarbon (14C) content of surface waters inferred from a coral record from the
Galápagos Islands increased abruptly during the upwelling season (July through …

Easterly trade winds from near-equatorial islands in the central Pacific weakened before
each El Niño between 1950 and 1978, except for the 1963 El Niño. The weakening of the …

Time series measurements from surface moored buoys in the eastern equatorial Pacific are
analyzed for the period 1983–86. The data, collected as part of the EPOCS and TROPIC …

The differences in tropical air–sea interactions and global climate connection as well as the
hindcast skills for the warm pool (WP) and cold tongue (CT) El Niños are investigated based …

The initial surface warming of the 1982 El Niño event was of quite different timing and
pattern from that associated with most El Niño events; strong anomalous warming occurred …

We describe the characteristics of surface westerly wind episodes in the tropical Pacific
between mid‐1957 and 1980, as they can be determined from a collection of daily average …

The morphology of westerly wind bursts (WWBs) during the 1980s is investigated using
1000‐mbar winds analyzed by the European Center for Medium‐Range Weather Forecasts …