Hawai`i’s
wettish winter could continue, as the current La Nina climate cycle is expected
to last through the winter.
That’s
the latest assessment (January 11, 2018) from NOAA’s Climate Prediction Center
and the International Research Institute for Climate and Society.
Long-term
prediction of climate cycles is problematic, but most climate models seem to
suggest that we could shift into El Nino by mid-summer. If that holds true, it could result an more tropical storms and hurricanes later this year than normal.
La
Nina and El Nino are two major climate cycles affecting weather conditions in
the Pacific. La Nina has cooler water in the equatorial central Pacific and El Nino
has warmer waters.
Generally,
for Hawaiian islands, El Nino conditions are associated with dry winters and
stronger and more frequent hurricanes June to November. La Nina—which we’re now
in—tend to have fewer storms from June to November and wetter winters.
Have you
noticed a lot of strong tradewinds recently? La Nina conditions are also
associated with stronger low-level tradewinds.
The
new report suggests that La Nina conditions continued through the end of 2017
and are expected to persist through the rest of the winter, while weakening. After that, conditions
should drift toward a neutral condition for the spring. And the models seem to indicate a continued shift toward El Nino as the summer progresses.
El
Nino/La Nina conditions don’t only impact the climate of the Pacific, but are
also associated with rainfall and temperature patterns on the Mainland.
Based
on the latest climate models, “The outlooks generally favor above-average
temperatures and below-median precipitation across the southern tier of the
United States, and below-average temperatures and above-median precipitation
across the northern tier of the United States.”
Since central Pacific ocean water temperatures are a key indicator of El Nino and La Nina cycles, the climate agencies have computerized models that track where they think water temperature is going. There are many such models, but as shown below, most of them are showing water warming into the summer months.
The bottom line shows months in three-month periods. The dynamic average shifts from negative to positive temperatures in May-June-July (MJJ)
Forecasts of sea surface temperature (SST) anomalies for the Niño 3.4 region (5°N-5°S, 120°W-170°W). Figure updated 18 December 2017. Credit: NOAA. |
© Jan TenBruggencate 2018
Figure 6. Forecasts
of sea surface temperature (SST) anomalies for the Niño 3.4 region (5°N-5°S,
120°W-170°W). Figure updated 18 December 2017.
Figure 6. Forecasts
of sea surface temperature (SST) anomalies for the Niño 3.4 region (5°N-5°S,
120°W-170°W). Figure updated 18 December 2017.