El Niño and Waikato spring climate: dry or wet?
The possibility of a return to El Niño conditions later this year has been strengthened by recent developments in the tropical Pacific (see the Climate Outlook on page 3). The best indication of the effect that El Niño might have on spring rainfall can be found in the historical record of previous El Niño springs. Here we look at Waikato spring rainfall as an example of how to use historical data to determine probable regional El Niño impacts.
Waikato spring rainfall
About 260 to 320 mm of rainfall is typically recorded in lowland Waikato during spring, with higher falls in the hill country. At Morrinsville, in central Waitako, the average spring rainfall is 284 mm.
Morrinsville spring rainfall for all years since 1950 is shown in Figure 1 below. The data points are shown in orange, green, and blue to illustrate the lower, middle, and upper tercile rainfalls respectively (see caption). The vertical green dashed lines mark the boundaries of the tercile ranges.
The driest spring in Morrinsville, 1954, recorded just 129 mm (155 mm below average), and in the wettest year, 1971, there were 477 mm (193 mm above average).
El Niño years
Both the El Niño and La Niña phases of the El Niño-Southern Oscillation are associated with typical spring atmospheric circulation patterns over New Zealand. During El Niños there is a tendency for more southwesterlies than normal over the Waikato.
El Niño seasons are characterised by above- average sea surface temperatures in the equatorial Pacific Ocean, and by changes in atmospheric circulation patterns over the Pacific that can result in the Southern Oscillation Index (SOI) remaining about or less than -1 for periods of three months or longer (near or below the dashed red line in Figure 1).
The El Niño spring seasons since 1950 are labelled in Figure 1. Four seasons, 1963, 1965, 1982, and 1987 had lower tercile rainfalls, five seasons, 1957, 1972, 1977, 1991, and 1997 recorded middle tercile rainfalls, and two seasons, 1951 and 1994, fell in the upper tercile.
El Niño spring outlook?
The data in Figure 1 illustrate why forecasts of 2002 spring rainfall are best given in probabilistic terms. Of the 11 El Niño springs since 1950, only two resulted in upper tercile rainfalls at Morrinsville. These data suggest that the chance of above normal rainfall in central Waikato in an El Niño spring is less than 20%, while the probability of lower decile rainfall is greater than 50%.
Figure 2 shows El Niño spring rainfall anomaly patterns across the Waikato region. The centre map, showing the average anomaly, indicates that rainfall is likely to be near average in the west (95-105% of average), and that there is a tendency to below average rainfalls in the east (less than 85%). This tendency for lower than average rainfall in the east is reflected also in the spring rainfalls of both the driest and wettest El Niño springs, 1965 and 1994 respectively, and provides another clue as to how the spring rainfall pattern might evolve
The surf at Muriwai Beach, Auckland. El niño may bring heightened west to southwest winds, and perhaps better surf, to west coast beaches in spring and summer. (Photograph: Georgina Griffiths)