El Nino and La Nina Difference, Meaning, Effect

El Nino and La Nina

El Nino and La Nina are two opposing climate phenomena that mess with upwelling patterns and have an impact on the economy, ecosystems, and weather on a worldwide scale. Although inconsistent, El Nino and La Nina events typically happen every two to seven years. El Nino generally happens more frequently than La Nina. Changes in water temperature in the eastern central equatorial Pacific can lead to the complicated weather phenomena El Nino and La Nina.

El Nino and La Nina Meaning

El Nino

El Nino impact refers to sporadic climate changes and the emergence of warm ocean surface waters along the coasts of Peru and Ecuador. The El Nino effect was originally noticed by South American fishermen in the 17th century.

When there is an El Nino, the trade winds that normally sweep from east to west along the Equator diminish, resulting in high air pressure in the western Pacific Ocean and low air pressure in the eastern Pacific Ocean. As a result, the surface water is moving towards the northern South American shore. An El Nino impact results from a six-month period of ocean warming in the central and eastern Pacific. Warming the central and eastern Pacific Ocean during an El Nino diminishes the regular upwelling of cold water, thus lowering the region’s nutrient level.

The East Pacific Ocean’s warmer waters cause the winds in some areas to change direction.

• Usually lasting a few weeks to a few months, the El Nino impact happens around Christmas. Depending on how warm the water is at the moment, it could occasionally last for significantly longer lengths of time.
• When a climate like this warms for seven to nine months, it is referred to as El Nino “conditions,” and when it lasts longer, it is referred to as an El Nino “episode.”
• The El Nino effect typically happens more often than the La Nina effect. The relationship between the ocean-atmosphere climate interaction and the rise in sea surface temperature in the Central and East-Central Equatorial Pacific can be inferred from fluctuations in ocean temperature.
• These complex meteorological conditions develop in the Equatorial Pacific Ocean. El Nino happens regularly, but the “cold phase” of ENSO is infrequent. The Indian monsoon has a disastrous effect on the nation’s agricultural activity as a result of the El Nino influence.
• The El Nino effect is unpredictable; it never follows a set rhythm. El Nino occurs erratically every 2–7 years as well. El Nino is sometimes thought of just a coastal surface water warning, but it is also known to cause significant climate change.

La Nina

It is also known as El Viejo, Anti El Nina, or a “cold occurrence,” and in Spanish it means little girl. El Nino is at odds with La Nina. The trade winds are more powerful when La Nina is present, which causes Asia to get warmer water. Increased upwelling off the west coast of the United States causes cold water rich in nutrients to rise to the surface. Due to the jet stream being driven north by these chilly Pacific Ocean waters, the southern United States experiences droughts, and the Pacific Northwest and Canada experience severe rainfall and flooding.

The south experiences warmer winters than the north, which experience colder ones. Hurricanes can also be caused by La Nina. The Pacific Ocean’s offshore waters are colder than usual. More marine life is supported by them, and areas like the California coast are attracted to more coldwater animals like squid and salmon because they contain more nutrients.

Image of formation of El Nino and La Nina

El Nino and La Nina Effect

Ten of India’s 13 droughts since 1950 have occurred in El Nino years, and one has occurred in a La Nina year. This is due to the fact that an El Nino typically results in India receiving less rain than average. Because Indian agriculture depends so heavily on the monsoons, lower rainfall during the monsoons typically results in below-average crop production.

Effect of El Nino

• Convection over warmer surface water increases the likelihood of precipitation. South American rainfall has increased, causing erosion and coastal flooding.
• Regions hit by tragedies caused by nature, such as flooding and drought, are more vulnerable to the spread of diseases.
• Many areas contend that increased disease transmission is a result of El Nino flooding. Respiratory issues are brought on by cholera, dengue fever, malaria, and other illnesses.
• Dryness is a result of El Nino in Australia and Indonesia. Water shortages result from reservoirs drying up and rivers not carrying enough water, endangering agricultural activity since we need water to irrigate land.
• The El Nino influence has reduced the frequency of hurricanes in the Atlantic.

Effect of La Nina

• It causes severe monsoons in Southeast Asia and India.
• It causes a condition in Peru and Ecuador that resembles a drought.
• It brings about chilly, wet winters in Southeast Africa and wet weather in Eastern Australia.
• It causes winter draughts in the Southern United States.
• It makes the winters in the northwest United States and western Canada extremely chilly.
• In Australia, it leads to significant flooding.
• The Western Pacific, the Indian Ocean, and the area off the coast of Somalia see high temperatures as a result.
• It leads India to experience intense monsoon rains.

El Nino Vs La Nina

El Nino and La Nina Facts for UPSC

• The trade winds that blow from east to west intensify during La Nina.
• The 1997–98 El Nino was the first to be systematically tracked from beginning to end.
• The 1997–1998 events had an impact on many areas; Peru and California had significant rain and flooding, whereas the Philippines, Malaysia, and Indonesia experienced drought conditions.
• La Nina is primarily brought on by an increase in easterly trade winds.
• The El Nino – Southern Oscillation (ENSO) cycle has two opposing phases, El Nino and La Nina.

El Nino and La Nina FAQs

Q What is the difference between El Niño & La Niña?

The term “El Nino” describes the irregularly occurring, above-average sea surface temperatures in the eastern and central equatorial Pacific. The ENSO cycle’s warm phase is represented by it. In the eastern and central equatorial Pacific, there is a periodic decrease of sea surface temperatures known as La Nina.

Q What is the El Nino and La Nina effect?

Ans. El Nino impacts weather systems around the globe, triggering predictable disruptions in temperature, rainfall and winds. La Nina is the opposite – a cooling phase of ENSO that tends to have global climate impacts opposite to those of El Nino.

Q Is it La Niña or El Niño 2022?

Ans. Overall, the coupled ocean-atmosphere system continued to reflect La Niña. The most recent IRI plume forecast of the Nino-3.4 SST index indicates La Nina will persist into the Northern Hemisphere winter 2022-23, and then transition to ENSO-neutral in January-March 2023

Q What are El Nino and La Nina years?

Ans. El Nino and La Nina can both have global impacts on weather, wildfires, ecosystems, and economies. Episodes of El Nino and La Nina typically last nine to 12 months, but can sometimes last for years. El Nino and La Nina events occur every two to seven years, on average, but they don’t occur on a regular schedule

Q Is El Niño wet or dry?

Ans.

• Reduced rainfall.
• Warmer temperatures.
• Shift in temperature extremes.

Q Is La Niña warm or cold?

Ans. La Nina refers to the periodic cooling of ocean surface temperatures in the central and east-central equatorial Pacific. Typically, La Nina events occur every 3 to 5 years or so, but on occasion can occur over successive years. La Nina represents the cool phase of the El Nino/Southern Oscillation (ENSO) cycle.

Other Indian Geography Topics

Other Fundamental Geography Topics

Sharing is caring!