Read our forecast: Monsoon 2014: ‘Super’ El Niño
is unlikely but rainfall deficiency can cross 16%!
Note EQUINOO is another
terminology for Indian Ocean Oscillation (IOD). Wonder why they need to coin
another terminology for the same phenomenon. Nonetheless the substance of the
article remains interesting...
(Papiya Bhattacharya in
IndianExpress) The warm phase of El Nino Southern Oscillation (ENSO) has
already begun in April with increased rainfall over the Central Pacific. All
weather models predict that it will amplify and persist until the end of the
summer monsoon, according to Sulochana Gadgil, a meteorologist at the Centre
for Atmospheric and Oceanic Sciences (CAOS) in Bangalore.
In an editorial in the
latest issue of Current Science, she describes in detail the effects of a
probable El Nino on rains in India.
The editorial talks about
how the Indian monsoons depend on another phenomenon called the Equatorial
Indian Ocean Oscillation (EQUINOO) and, if the dreaded El Nino shows effect
this year, its bad effects may be neutralised by a favourable phase of EQUINOO.
Gadgil says there are
uncertainties about an El Nino and, by mid-June, it will be known if the
phenomenon will occur.
“In 2014, an unfavourable ENSO phase is expected,
implying the probability of a drought of over 30 per cent. If an El Nino does
develop, the chance of a drought increases to 70 per cent,” she says in the
editorial.
In 2003, it was discovered
that in addition to ENSO, EQUINOO plays an important role in the yearly changes
in rains in India. According to Gadgil, EQUINOO involves a see-saw between a
state with enhanced rainfall over western equatorial Indian Ocean and suppressed
rainfall over eastern equatorial Indian Ocean (favourable phase) and a state
with opposite signs of East-West rainfall anomalies.
El Nino refers to the
process of warming of the sea surface around the coast of Peru due to warm sea
currents with far-reaching consequences. The warm waters cause fish and birds
to die.
A drought in India could
only lead to a fall in GDP, says Gadgil. Studies of the impact of Indian Summer
Monsoon Rainfall (ISMR) on the GDP and food grain production in India during
1954-2004 have shown that bad effects of droughts are worse than the good
effects of rain. Nine such El Nino events have occurred since 1958. Of these,
seven led to less rains, six of them being droughts.
However, the monsoon
rainfall was above average in 1963 as well as during the strongest El Nino
phenomenon of 1997. The editorial says,
“During the El Nino of 1972-73, severe
droughts occurred in Australia, India, Brazil, etc., and heavy flooding
occurred in Kenya and parts of Ecuador and Peru.”
Some of these climatic
extremes may have a common reason — changes in sea surface temperatures in the
Pacific Ocean (El Nino) and changes in the atmospheric sea-level pressure
across the Pacific basin (the Southern Oscillation). These combined changes have
come to be popularly referred to as El Nino, and in scientific literature as El
Nino Southern Oscillation events. Most Indian science models predict and
simulate ENSO and the ENSO-Indian monsoon link, but they do not simulate or
predict the EQUINOO and the EQUINOO-Indian monsoon link correctly. Since the
latter has a larger effect on the monsoons, it may mitigate the effects of El
Nino this year, if it were to occur, the editorial concludes.
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