» Geography of the El Niño and La Niña

Geography of the El Niño and La Niña

EL NIÑO AND La Niña are parts of global weather systems that recur every 2 to 7 years. An El Niño, which usually lasts 12 to 18 months, is characterized by warm winters and wet springs in , a lessening of monsoonal rains in Asia, and droughts affecting Africa and the south Pacific Ocean. A La Niña system follows for up to 3 years, producing opposite effects. Southern Oscillation indicates the variations in sea level pressure noted in the Pacific between the southern and northern hemispheres. Both El Niño’s and La Niña’s are considered part of the El Niño Southern Oscillation (ENSO), a term used to describe the full range of wind and ocean patterns reflected in the Southern Oscillation itself. An El Niño occurs when the northeast tradewinds of the south Pacific slacken, and in the same area, ocean water warms and moves east. This action can reverse the trade winds by causing an increase in warm air, which rises and changes air pressure patterns. Abnormally dry weather then settles over islands in the tropical Pacific like Indonesia, Borneo, and the Philippines, while humid, warm air affects the west coast of . Over several months, an El Niño impacts world weather patterns. In winter, the U.S. Pacific northwest and western Canada get less rain, while southern California and the Gulf Coast experience more rain and storms. Also in the United States, warmer temperatures affect the Great Plains and upper midwest. Brazil, southern Africa, and Australia experience dryness and drought. Rainfall lessens and drought often hits India and southern Asia. Monsoonal moisture, a critical element on which all farmers depend, may not arrive, and the result is famine, often followed by diseases and death. Fewer hurricanes develop in the Atlantic Ocean, and less rain falls in Mexico and the southwestern United States. In the Pacific Ocean, more typhoons occur. Clearly, aberrations in the weather can cause great hardship and loss of life. The loss of monsoon rains in India for several years in the 1890s caused a famine that claimed over 4 million lives. An El Niño brings other troubles as well: Abnormal ocean temperatures keep fish from shore, ruining coastal economies. Normally dry high altitudes get snow, and months later when the snow melts, mudslides and flooding can follow. Huge brush fires, sparked in unusually dry conditions, can devastate large areas; in 1997 and 1998, fires in Indonesia caused at least $9 billion in damage and lost timber, as well as dramatically polluting the air throughout Southeast Asia to such an extreme extent that the sun could not be seen for days in some cities. Even when the fires were extinguished, underground peat continued to burn, contributing to the pollution. An El Niño is typically, but not always, followed by a year or more of La Niña conditions. During La Niña, also called an El Viejo, the temperatures in the equatorial Pacific region are colder than normal. This results in wet winter weather in the South Pacific and southern Asia, and drier conditions along the South American coast. In the United States, winter temperatures are warmer in the southeast and cooler in the northwest. The history of the ENSO goes back thousands of years, but it was not identified until recently. In 1891, the president of the Lima Geographical Society first officially reported that fishermen in Peru sometimes noted a warm countercurrent in the Pacific Ocean right after Christmas that indicated more rain, exotic fish, and lots of vegetation would come the following year. The locals called it El Niño, a term referring to the Christ child. Although droughts, floods, and seasons of unusual weather had been noted and even studied for years, it was not until the 1920s that scientist Gilbert Walker identified the Southern Oscillation. In the 1960s, Norwegian meteorologist Jacob Bjerknes connected Walker’s discovery with the extensive ocean warming of an El Niño system. He described the anomalous circulation patterns that followed, and named them the Walker Circulation. Scientists, historians, archaeologists, and researchers all over the world are now putting events and data together, realizing that weather systems such as the ENSO last for years and have impacted civilizations on a global scale for millennia. Events once considered random and unrelated are now being explained in terms of climatic events. El Niño droughts were likely responsible for the downfall of the Mayan civilization in Central America, the Moche Empire of Peru, and the Anasazi complex of the American southwest. Glacial ice cores, coral reefs, and tree rings provide evidence of ancient weather patterns and anomalies. The El Niño of 1997–98 was 1 of the worst in recent memory. The fires of Indonesia have been mentioned; large economic losses impacted many areas, such as Australia and Southeast Asia, where drought occurred. Ironically, this El Niño came with much advance warning, and areas like heavily populated California were able to invest millions of dollars in preparation, thus avoiding more losses. Groups such as the National Oceanic and Atmospheric Administration (NOAA) predict and track El Niños using satellites, research ships, buoy arrays, computer modeling, and other tools to analyze ocean temperatures, wind speeds, fish populations, precipitation, and other early indicators of developing weather systems.
  • image

    Geography of the Pacific Ocean

    THE PACIFIC OCEAN HAS an area of approximately 68,767,000 square mile (178,106,000 square kilometer) with its adjacent seas;
  • image

    Geography of the Orographic precipitation

    OROGRAPHIC PRECIPITATION is caused or enhanced by 1 or more of the effects of mountains on the Earth’s atmosphere.
  • image

    Geography of the Monsoon

    THE HEAVY RAINS of the monsoon appear in June and subside in September every year in the Northern Hemisphere.
  • image

    Geography of the Humboldt Current

    THE HUMBOLDT CURRENT, also known as the Peru Current, is an ocean current that flows along the western coast of South America,
  • image

    Geostrophic winds

    GEOSTROPHIC WINDS blow above the friction layer of the Earth, balanced between pressure gradient forces and the Coriolis force.
  • Comments: