El Nino Essay, Research Paper
El Nino
Typically, the level of ocean water around the world is higher in the
western Pacific and lower in the eastern, near the Western coast of South and
North America. This is due primarily to the presence of easterly winds in the
Pacific, which drag the surface water westward and raise the thermocline
relatively all the way up to the surface in the east and dampen it in the west.
During El Nino conditions, however, the easterlies move east, reducing the
continuing interaction between wind and sea, allowing the thermocline to become
nearly flat and to plunge several feet below the surface of the water, allowing
the water to grow warm and expand. With the help of the National Oceanic and
Atmospheric Administration’s weather satellites, tracking shifting patterns of
sea-surface temperatures can be made easier. Normally, a “pool” of warm water in
the western Pacific waters exists. Under El Nino conditions, this “pool” drifts
southeast towards the coast of South America. This is because, in a normal year,
there is upwelling on the western South American coastline, and cold waters of
the Pacific rise and push westward. However, during an El Nino year, upwelling
is suppressed and as a result, the thermocline is lower than normal. Finally,
thermocline rises in the west, making upwelling easier and water colder. Air
pressures at sea level in the South Pacific seesaw back and forth between two
distinct patterns. In the high index phase, also called “Southern Oscillation”,
pressure is higher near and to the east of Tahiti than farther to the west near
Darwin. The east-west pressure difference along the equator causes the surface
air to flow westward. When the atmosphere switches into the low index phase,
barometers rise in the west and fall in the east, signaling a reduction, or even
a reversal the pressure difference between Darwin and Tahiti. The flattening of
the seesaw causes the easterly surface winds to weaken and retreat eastward.
The “low index” phase is usually accompanied by El Nino conditions.
The easterly winds along the equator and the southeasternly winds that
blow along the Peru and Ecuador coasts both tend to drag the surface water along
with them. The Earth’s rotation then deflects the resulting surface currents
toward the right (northward) in the Northern Hemisphere and to the left
(southward) in the South Hemisphere. The surface waters are therefore deflected
away from the equator in both directions and away from the coastline. Where the
surface water moves away, colder, nutrient-rich water comes up from below to
replace it which is called upwelling. The winds that blow along the equator also
affect the properties of upwelled water. When there is no wind, the dividing
layer between the warm surface water and the deep cold water would be almost
flat; but the winds drag the surface water westward, raising the thermocline
nearly all the way up to the surface in the east and depressing in the west.
The resulting changes in sea-surface temperature will have an effect on the
winds. When the easterlies are blowing at full strength, the upwelling of cold
water along the equatorial Pacific chills the air above it, making it too dense
to rise high enough for water vapor to condense to form clouds and raindrops. As
a result, this part of the ocean stays indubitably free of clouds during normal
years and the rain in the equatorial belt is mostly confined to the extreme
western Pacific. However, when the easterlies weaken and retreat eastward during
the early stages of an El Nino event, the upwelling slows and the ocean warms.
The moist air above also warms. It would produce deep clouds which make heavy
rain along the equator. The change in ocean temperatures thus causes the major
rain zone over the western Pacific to shift eastward. In this way, the dialogue
between wind and sea in the Pacific can become more and more intense.
Normally, each area of the globe follows a fairly predictable pattern
and receives only that amount of rainfall that it is accustomed to receiving.
However, conditions are quite different during El Nino. During normal years,
when the winds blowing east along the equator are blowing at full strength,
this strip of ocean stays free of clouds and the rain in the equatorial belt
largely confined to the extreme Western Pacific, near Indonesia. But when the
easterlies weaken and retreat eastward during El Nino years, the moist air above
the ocean becomes buoyant enough to form clouds, and the clouds produce heavy
rains along the equator. These rains are only some of the many weather changes
that occur all over the globe during an El Nino event. Many other weather
changes have resulted in great amounts of damage to the area. In 1982-1983, the
El Nino resulted in 100 inches of rain falling during a six month period on
Ecuador and northern Peru. The rain transmogrified the coastal desert into a
grassland mottled with lakes. That same El Nino also caused typhoons to hit
Hawaii and Tahiti. The monsoon rains that fell over the central Pacific, instead
of on the Western side, led to terrible droughts and forest fires in Indonesia
and Australia. Also, winter storms struck southern California and caused a lot
of flooding across the southern United States, while northern regions of the USA
received unusually mild winters and a lack of snow. Obviously, El Nino events
have quite an effect on global weather patterns. Hopefully, as scientists
develop better models, they will soon be better able to understand and make
predictions about this curious event.
Normally, the thermocline is quite high in the eastern Pacific. Stirring
by the wind mixed the nutrient-rich water below with the surface water. In the
presence of sunlight, phytoplankton can produce chlorophyll, a tiny green plant
substance. In turn, this substance feeds zooplankton, which in turn feeds higher
members of the food chain. During El Nino conditions, the water level rises in
the east and lowers in the west, forcing many changes to happen among the plant
and animal life. Sea birds in the east must leave their nests, abandoning their
young and searching for food which is not there, because the critical upwelling
which causes the plankton and other lower members of the food chain to be
produced is not there. Water temperature is above normal, and tropical fish are
displaced poleward or migrate, along with the anchovy and sardines. On land,
the effects produced a great amount of rainfall, making the desert lands into a
grassland with lush vegetation and abundant life. Grasshoppers come, fueling
toad and bird populations, and the increase in rainfall produces lakes which
fish come to inhabit, fish that had migrated upstream during floods produced by
the rain and become somehow trapped. In some flooded coastal cities, shrimp
production set records. So too did the number of mosquito-borne malaria cases.