El Nino-Southern Oscillation

Slides:



Advertisements
Similar presentations
El Niño & La Niña.
Advertisements

Ocean Currents
Ocean Currents
Oceanic Circulation Current = a moving mass of water.
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
What Are the El Nino and La Nina?
More Climatic Interactions
Currents and Climate.
Chapter 5—Part 1 Ocean Circulation/ Upwelling Zones/ El Niño.
What is Climate? The long term average of weather, usually 30 years+
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
Ocean Currents. A penguin walks into a bar and asks the pharmacist for Chapstick. After grabbing the Chapstick, the pharmacist asks the penguin, “How.
 An ocean current is any permanent or continuous, directed movement of ocean water that flows in one of the Earth's oceans. Ocean Currents.
Ocean Circulation.
Oceanic Influences on Climate. Ocean currents redistribute heat Large scale currents are called gyres.
wind – air that moves horizontally convection cell – a pattern of rising and falling air, sinking air, and winds caused by unequal heating and cooling.
Atmospheric movements We learned that energy is transferred from the Sun to the Earth creating convection currents. But, what type of currents???
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
Winds Wind is the horizontal movement of air. Air always moves from H  L pressure. Temperature differences create pressure differences. Weather is based.
Ocean Circulation – Ch Ag Earth Science – Chapter 15.2.
Ocean Currents.
Global Wind Patterns. What is Wind? Wind is the movement of air from an area of higher pressure to an area of lower pressure. Warmer air expands, becoming.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Chapter 5—Part 1 Ocean Circulation/ Upwelling Zones/ El Niño.
1 NORMAL Normally, trade winds blow warm surface water toward the western Pacific. This causes the thermocline to rise near the surface in the eastern.
Ocean Current s.  Warm currents flow away from the equator.  Cold currents flow toward the equator. Ocean Currents.
Air Movement (53) Areas of Earth receive different amounts of radiation from the Sun because Earth is curved.
Oceans Surface Currents. What are surface currents? Surface currents are horizontal, streamline movements of water that occur at or near the surface of.
Normal Conditions The trade winds move warm surface water towards the western Pacific. Cold water wells up along the west coast of South America (the Peru.
Coriolis Effect Because the Earth rotates, and consists of a mixture of land and sea, the Coriolis Effect exists The Coriolis Effect is the movement of.
Atmospheric Circulation. Winds on a Non-Rotating Earth Air at the equator warms and rises. Once aloft, air flows back towards the poles where it cools.
19.1.
Global Weather Patterns
Oceanic Circulation.
Ocean Currents & Global Climates
Global and Local Winds i.
Teleconnection Systems NAO AO PNA
100 pt 100 pt 100 pt 100 pt 100 pt 200 pt 200 pt 200 pt 200 pt 200 pt
El Nino and La Nina Ocean_4_ENSO Lecture.
16.1 – Ocean Circulation.
Gairloch High School / Invergordon Academy
DO NOW Turn in Review #22. Pick up notes and Review #23.
Differential Heating – Specific Heat
Currents.
Chapter 16.1 Ocean Circulation.
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
Answer the question shown up here
Currents and Climate.
Ocean currents are in same direction as the wind – they become circular due to currents hitting land masses
El Nino Southern Oscillation
Oceanic Influences on Climate
Ocean Currents.
Global and Local Winds i Kinsey
Oceans and Climate Visual Vocabulary.
Short term Climate change
Ocean Currents
Oceans The great abyss.
Section 2: Atmospheric Phenomena
Ocean Currents El Niño and La Niña.
Chapter 10 Wind: Global Systems.
Currents and Climate.
El Niño and La Niña.
Aquatic Science Fall Final Review
Ocean Currents.
Currents and Climate.
Air Pressure And Wind Chapter 19.
Unit 13 – The Atmosphere and Air Pollution
2.2.
Air, Weather, and Climate
Winds- Now with even better explanations!
Presentation transcript:

El Nino-Southern Oscillation ENSO El Nino-Southern Oscillation

ENSO El Nino-Southern Oscillation in equatorial Pacific 5-7 year cycle El Nino = warmer surface waters La Nina = cooler surface waters Changes in the walker cell during ENSO. Source: http://www.pmel.noaa.gov/tao/elnino/.noaa/enso.html El Niño: Warmer winters across the northern USGulf states cooler and wetter California can be wetter or drier Pacific salmon and other fisheries disrupted Fewer hurricanes in the Atlantic La Niña: La Niña has equally dramatic, often opposite effects on the US

Signs of El Nino Changes in air pressure at sea surface Trade Winds weaken in the South Pacific Warm air rises over Peru in South America Drought conditions persist in western Pacific This slide shows dry and wet areas around the world during El Nino. http://www.cpc.noaa.gov/products/analysis_monitoring/ensocycle/enso_cycle.shtml

Signs of La Nina Opposite of El Nino Increased Hurricane activity in Atlantic Cold, wet NW N. America Increase upwelling offshore from Peru This slide shows dry and wet areas around the world during La Nina. http://www.cpc.noaa.gov/products/analysis_monitoring/ensocycle/enso_cycle.shtml

Hadley Cells control the Trade winds http://www.boqueteweather.com/climate_article.htm This flow of circulation forms air cells calledHadley Cells which generate the earth’s major air circulation masses and related wind systems (See Figure 8 from Lutgens and Tarbuck, 2007). These air movement systems are also affected by the rotation of the earth which bends and changes their direction (coriolis force). The circulation cells that most affect this part of the world form the Trade Winds. In the northern hemisphere the Trade Winds begin about 30° north latitude and blow in a northeasterly direction toward the lower equatorial pressure. In the southern hemisphere the Trade Winds begin about 30° south latitude and blow in a southeasterly direction toward the lower equatorial pressure. Where the winds meet near the equator, the air is of course heated, the pressure lowered, and if it is over water gets filled with moisture to rise again and continue the ongoing cell dynamics.

Coriolis Force “Apparent” force due to the rotation of the Earth N. Hemisphere - deflection to the right S. Hemisphere - deflection to the left The rotation of the Earth causes an interesting phenomena on free moving objects on the Earth. Objects in the Northern Hemisphere are deflected to the right, while objects in the Southern Hemisphere are deflected to the left. The coriolis effect, thus tries to force winds to shift towards the right or left. The coriolis effect can at times cause winds to blow back up the pressure gradient.

Some Impacts from El Nino Indonesia Drought Southwest US FLOODING Images of some regional impacts from El Nino.

Some Impacts from El Nino Colder temps in Florida cause manatees to congregate near warm water outflows (left). El Nino causes colder winters in Europe due to decreased heat transfer of the Gulf Stream (right).