Southern Oscillation and ENSO (El Niño-Southern Oscillation)
Definition of ENSO: A climate phenomenon involving fluctuations in ocean temperatures and atmospheric pressure in the Pacific Ocean.
Key Components:
El Niño: Periodic warming of ocean surface temperatures in the central and eastern Pacific, causing changes in weather patterns.
La Niña: Opposite phase characterized by cooler ocean surface temperatures.
Characteristics of El Niño
Ocean-Wind Interaction:
Reversal of normal pressure and wind patterns across the Pacific Basin (Western Pacific low pressure, Eastern Pacific high pressure).
Changes lead to warmer Pacific Ocean temperatures which affect weather patterns globally.
Duration:
Lasts approximately 3 to 6 months; can extend to over a year.
Detection:
Observed through sea surface temperatures and atmospheric pressure metrics using satellite technology and pressure stations in key locations (e.g., Tahiti, Darwin, Peru).
Normal vs. El Niño Conditions
Normal Conditions:
High pressure off the coast of Peru leads to colder ocean waters due to upwelling, nutrient-rich fisheries, and typical dry weather.
Low pressure in the Western Pacific (Indonesia) produces warm sea conditions and significant precipitation.
El Niño Conditions:
Low pressure systems shift towards the Eastern Pacific, reducing upwelling and replacing cold water with warmer water.
Impacts: Drought in Western Pacific areas, increased precipitation and flooding in Eastern Pacific (e.g., Peru).
Predictive Aspects of ENSO
Teleconnections:
ENSO influences weather patterns not only in the Pacific Basin but also in regions such as the Atlantic and Indian Oceans, albeit to a lesser extent.
Global Climate Impact:
Changes in temperature and precipitation patterns can affect agricultural practices and increase natural disasters (e.g., flooding, drought).
Southern Oscillation Index (SOI)
Measurement:
SOI computes the pressure difference between Tahiti and Darwin, providing insight into ENSO conditions.
Indicators:
A drop in pressure at Tahiti indicates the onset of El Niño, while an increase suggests La Niña or neutral conditions.
La Niña Overview
Characteristics:
Enhanced normal conditions with stronger trade winds and lower sea surface temperatures.
Often results in wetter conditions in the Pacific, contrasting the drier conditions resulting from El Niño.
Global Climate Effects of ENSO
El Niño's Influence:
Increased rainfall in the southern U.S.; drier conditions in Southeast Asia, influence on storm patterns in other regions.
Weather Implications:
El Niño usually associated with warmer winters in Northern U.S., increased precipitation in Southern U.S.
La Niña leads to cooler and wetter conditions in the North and drier conditions in the South.
Formation of Hurricanes
Essential Elements:
Warm ocean waters (at least 26.5^{ ext{o}}C), Coriolis force, and atmospheric conditions promoting thunderstorms required for hurricane formation.
Categorization:
Tropical Wave: The initial low-pressure area; can evolve into a tropical depression, then a tropical storm, and finally a hurricane.
Conditions for Naming: Wind speeds of at least 74 mph classify systems as hurricanes.
Hurricane Structure and Mechanics
Cross Section:
Low-pressure center dictates rotation; pressure gradients drive wind speeds.
Eye of the storm: calm conditions, surrounded by the eye wall with the strongest winds.
Operational Dynamics:
Hurricanes draw energy from warm ocean water; dissipate upon landfall.
Climate Change and Hurricanes
Potential Influence:
Rising sea surface temperatures may lead to stronger hurricanes, increasing both precipitation and storm intensity.
Emphasis on population growth in vulnerable areas increases potential damage from storms.
Summary Points to Remember
Key Topics for Quiz:
Definitions of ENSO and its components (El Niño/La Niña).
Normal vs El Niño conditions and their global impacts.
Understanding hurricane formation and characteristics.
The role of climate change in influencing hurricane patterns.