4.6 El Niño and La Niña
El Niño and La Niña Overview
El Niño and La Niña are significant climatic phenomena affecting global weather patterns.
Key Features of El Niño and La Niña
El Niño
Characterized by a high-pressure system.
Alters the polar jet stream, resulting in unusual weather conditions.
Associated with increased wet conditions in some areas.
La Niña
Produces low-pressure systems which can lead to dry conditions.
Also affects the polar jet stream and the Pacific jet stream, leading to a varied storm track.
The Influence of Ocean Currents on Global Climate
Ocean currents significantly impact global climates through:
Heat emission into the atmosphere.
Affecting primary productivity in marine environments.
Drivers of Ocean Currents
Factors Influencing Ocean Currents
Ocean currents are influenced by several factors:
Temperature
Gravity
Prevailing winds
The Coriolis effect
Salinity
Locations of continents
Tropical surface waters warm, causing them to expand and rise (approximately 8 cm or 3 inches). This expansion leads to water moving away from the equator.
Role of Prevailing Winds
The movement of ocean surface waters is guided by prevailing winds:
In the Northern Hemisphere, winds push water from the north-east to the southwest.
Gyres and Water Circulation
Gyres are large-scale patterns of water circulation:
Clockwise in the Northern Hemisphere.
Counterclockwise in the Southern Hemisphere.
These gyres help redistribute heat throughout the atmosphere.
Upwelling Processes
Divergence of surface currents along continents (e.g., west coasts) leads to upwelling:
Deeper waters rise to replace displaced surface water.
Upwelled waters bring nutrients from the ocean bottom, supporting a rich ecosystem.
Thermohaline Circulation
Thermohaline circulation refers to a major oceanic current system:
Driven by differences in density based on temperature and salinity variations.
El Niño-Southern Oscillation (ENSO)
An event occurs every 3 to 7 years starting around December 25th.
Responding to Exam Questions
Describe how gyres are formed:
Formed by the combination of wind patterns and the earth's rotation (Coriolis effect).
Potential impact of climate change on thermohaline circulation:
Alterations in temperature and salinity patterns may disrupt current systems, affecting global climates.
Role of salinity in driving deep ocean currents:
Changes in salinity levels affect water density, influencing the flow of deep ocean currents.
Difference between El Niño and La Niña:
El Niño typically brings warmer ocean temperatures leading to wetter conditions, while La Niña results in cooler ocean temperatures and often drier conditions.