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First Assessment Report - IPCC

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7 Observed Climate Variation and Change<br />

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Figure 7.21: (a) Schematic diagram of areas and times of the year with a consistent ENSO precipitation signal (adapted from<br />

Ropelewski and Halpert, 1987). (b) Monthly tropical sea surface and land air temperature anomalies 1961-1989; land data from P.D.<br />

Jones and sea surface temperature data from the UK Meteorological Office. Tropics extend from 20°N to 20°S. Arrows mark<br />

maximum ENSO warmth in the tropics.<br />

strong SO fluctuations from 1880 to 1920 led to the<br />

discovery and naming of the SO (Walker and Bliss, 1932)<br />

and strong SO events are clearly evident in recent decades.<br />

A much quieter period occurred from the late 1920s to<br />

about 1950, with the exception of a very strong multi-year<br />

ENSO in 1939-42 (Trcnbcrth and Shea, 1987; Cooper et<br />

al., 1989). Quinn et al. (1987) (covering the past 450 years)<br />

and Ropelewski and Jones (1987) have documented<br />

historical ENSO events as seen on the northwest coast of<br />

South America. Therefore, the potential exists for a longer<br />

palaeo-record based on river deposits, ice cores, coral<br />

growth rings and tree rings.<br />

During ENSO events, the heat stored in the warm<br />

tropical western Pacific is transferred directly or indirectly<br />

to many other parts of the tropical oceans. There is a<br />

greater than normal loss of heat by the tropical oceans,<br />

resulting in a short period warming of many, though not all,<br />

parts of the global atmosphere (Pan and Oort, 1983).<br />

Consequently, warm individual years in the record of<br />

global temperatures (Figure 7.10) are often associated with<br />

El Nifios. Maxima in global temperatures tend to occur<br />

about three to six months after the peak warmth of the El<br />

Nino (Pan and Oort, 1983). Figure 7.21b shows monthly<br />

anomalies of combined land surface air temperatures and<br />

SST for the global tropics from 1961-1989. The strong,<br />

coherent, warming influence of the 1972-73, 1982-83 and<br />

1986-88 ENSO events on the record of tropical temperature<br />

is very clear, as is the cold influence of the strong La Nina<br />

episodes of 1974-75 and 1988-89.

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