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33<br />

As the results in this initial study suggest, more specific<br />

climate in<strong>for</strong>mation provided in advance of a particular<br />

planting or harvest season will be of great help to those who<br />

make specific decisions in the agriculture sector...What is<br />

important is to be able to determine which <strong>for</strong>ecasting system<br />

will be able to yield better results depending on various<br />

variables like season, location, time of year, lead time, and<br />

the status of ENSO.<br />

decreases from 40 to 20 percent from September to March.<br />

• The seasonal <strong>for</strong>ecast skill in Malaybalay and<br />

Tacloban is statistically significant starting the month of<br />

October up to March.<br />

• Meanwhile, like in Tacloban, the percent chance of<br />

exceeding the median rainfall in Tuguegarao is increased<br />

from 60–80 percent during a cooler Pacific Ocean while<br />

the chance of getting this level is reduced during a hotter<br />

Pacific Ocean.<br />

For the Malaybalay site, meanwhile, since the<br />

available climate record is about 79 years, the same site<br />

was used. On the other hand, no evaluation was done as<br />

yet <strong>for</strong> the Cebu site.<br />

As mentioned, the SST phase system using the Pacific<br />

Ocean effects was the one applied in evaluating the<br />

impact on the study sites. In particular, the following main<br />

effects of the Pacific Ocean were tested: (1) cooler Pacific<br />

Ocean pattern where phases 1, 4, and 7 (which are<br />

associated with wetter than normal rainfall condition in<br />

the <strong>Philippine</strong>s) were combined; (2) neutral Pacific Ocean<br />

pattern where phases 2, 5, and 8 (wherein neutral<br />

conditions indicate that there is an equal chance of<br />

getting above normal or below normal rainfall in the<br />

<strong>Philippine</strong>s) were combined; and (3) hotter Pacific Ocean<br />

pattern where phases 3, 6, and 9 (which are associated<br />

with drier than normal rainfall condition in the <strong>Philippine</strong>s)<br />

were combined.<br />

Results of analysis<br />

The following are the key results of the analysis/<br />

evaluation:<br />

• An analysis of the historical data (from 1919–2004)<br />

in Malaybalay found that there is a 70 percent chance or<br />

probability of having the rains exceed the median rainfall<br />

during a cooler Pacific Ocean from September to February<br />

while there is a lower chance—at 20 to 30 percent—of<br />

getting a median rainfall during a hotter Pacific Ocean<br />

from September to March.<br />

• For the study site in Tacloban, analysis of historical<br />

data showed that <strong>for</strong> a constant lead time (0 month)<br />

be<strong>for</strong>e a three-month rainfall period, there is a 60–80<br />

percent chance of exceeding the median rainfall starting<br />

the month of November up to March during a cooler<br />

Pacific Ocean. During Phases 3, 6, 9 of the hotter Pacific<br />

Ocean pattern, the chance of getting above median rainfall<br />

What do the above results mean<br />

Simply told, the impact of ENSO on the <strong>Philippine</strong>s varies<br />

with season and location. Generally, the <strong>for</strong>ecast skill is<br />

higher <strong>for</strong> October to March.<br />

With regard to the status of the ENSO, the results<br />

indicate that during the onset of El Niño and La Niña<br />

(hotter Pacific Ocean and cooler Pacific Ocean<br />

occurrences, respectively), the trends established in the<br />

chances of getting lesser (<strong>for</strong> the El Niño period) or more<br />

(<strong>for</strong> La Niña period) amounts of rain than the median<br />

rainfall are more distinct.<br />

Un<strong>for</strong>tunately, however, there are also neutral<br />

conditions when there is an equal chance of getting<br />

above or below normal rainfall in the country. During this<br />

period, the <strong>for</strong>ecast skill is not statistically significant and<br />

decisionmakers need to use the long-term climate<br />

record.<br />

Conclusion<br />

As the results in this initial study suggest, more specific<br />

climate in<strong>for</strong>mation provided in advance of a particular<br />

planting or harvest season will be of great help to those<br />

who make specific decisions in the agriculture sector.<br />

For this study, focus was on the use of the SST phase<br />

system as an ENSO indicator at zero lead time. There are,<br />

however, other features in Rainman that can look, <strong>for</strong><br />

instance, at the seasonal <strong>for</strong>ecast skill using various lead<br />

times like, say, 30–60 days be<strong>for</strong>e a harvest season.<br />

In this regard, Rainman will be used and tested in<br />

the coming months to provide better answers to the<br />

specific needs of the users.<br />

What is important is to be able to determine which<br />

<strong>for</strong>ecasting system will be able to yield better results<br />

depending on various variables like season, location, time<br />

of year, lead time, and the status of ENSO. (SCF Project<br />

Updates, December 2005)

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