Meredith Taghon Physical Oceanography Fall 2015 Bigger Stronger Faster: Current El Niño

Slides:



Advertisements
Similar presentations
Increased Storm Activity around the Globe.
Advertisements

El Niño- Southern Oscillation
El Niño. What is El Niño? A shift in ocean current direction and water temperature El Niño: the ocean part: Warm phase of ENSO: El Niño - Southern Oscillation.
El Niño & La Niña.
El Niño.
El Niño. How do ocean currents affect weather and climate? Oceans store and transport heat. – High heat capacity – Stores and transports energy from the.
Essentials of Oceanography
Ocean and Atmosphere Coupling El-nino -- Southern Oscillation
El Nino, La Nina, and their Affects in Oklahoma. El Nino Conditions Warming of central and eastern equatorial Pacific waters Trade wind differences –
Class #16 Monday, October 4, 2010 Class #16: Monday, October 4 Chapter 8 Oceanography and El Niño/La Niña/ENSO 1.
Shanese Breitkreitz. Meaning – La Nina  The little girl  El Viejo – Old Man  A cold event  A cold episode.
El Nino – Southern Oscillation - Southern Oscillation (atmosphere) - El Nino (ocean) - change in equatorial Pacific circulation - produces global climate.
Southern Oscillation”
El Nino Southern Oscillation (ENSO)
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
Understanding El Nino and La Nina Aim: To understand the what this weather phenomena is and what conditions it brings (A.K.A – To understand a bloody difficult.
Do Now; Are there weather patterns that influence places thousands of miles away?
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
El Nino and the Southern Oscillation Jon Schrage.
El Niño & La Niña. THREE CIRCULATIONS OF THE OCEANS Normal circulation (Walker circulation) El Nino circulation La Nina circulation.
Abnormal Weather October 22, Teleconnections Teleconnections: relationship between weather or climate patterns at two widely separated locations.
WOW THIS IS FUN!  THE SUN : CLIMATE IS DIRECTLY LINKED TO THE SUN. SOME AREAS RECEIVE MORE OF THE SUN’S HEAT ENERGY THAN OTHERS.  WINDS : MOVEMENT.
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
Climate Change El-Nino Southern Oscillation (ENSO)Phenomena.
2015. equator Normally, trade winds converge at the equator and push warm water westward. In the eastern Pacific, cold water rises to the surface - upwelling.
ENSO: El Niño Southern Oscillation Background, Dynamics, Regional Impacts, and Future Outlook Josh Gellers Luis Poza EESC W4400.
 Abnormally high surface ocean temperatures off the coast of South America  Causes unusual weather patterns across the globe El Nino.
El Niño – The Christ Child (in Spanish)
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.
Much of the work that follows is straight from (or slightly modified) notes kindly made available by Jenny Pollock NCG and or spk (?)…. Nice to have a.
Anomalous Behavior Unit 3 Climate of Change InTeGrate Module Cynthia M. Fadem Earlham College Russian River Valley, CA, USA.
Severe weather is any weather that is destructive. The term is usually used to refer to: thunderstorms tornados tropical storms snowstorms/blizzards ice.
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.
El Nino and La Nina. er/environment/environment-natural- disasters/landslides-and-more/el-nino.htmlhttp://video.nationalgeographic.com/video/play.
The ENSO Cycle Naturally occurring phenomenon – El Nino / Southern Oscillation (ENSO) Cycle Equatorial Pacific fluctuates between warmer-than-average.
ENSO El Niño—Southern Oscillation  El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in equatorial eastern Pacific.
The unpredictability of GW and El Nino events leading to increasing natural hazards.
Recap Use the following graphs to explain what we discussed last lesson regarding frequency.
El Nino WORLD AT RISK Learning Intentions:
El Niño–Southern Oscillation (ENSO): What is it?
Climate Phenomena.
El Niño: A temperature anomaly
El Niño and La Niña.
Ocean/Air interaction
El Niño- Southern Oscillation
El Nino.
Ocean Currents & Global Climates
1. Why do we have climate zones? 2. Can pollution change a climate?
El Niño and La Niña.
El Niño / Southern Oscillation (ENSO)
Differential Heating – Specific Heat
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
El Niño-Southern Oscillation
El Nino Southern Oscillation
Short term Climate change
El Niño - Southern Oscillation
Climate changes Earth is constantly changing, including the climate.
The 1997/98 ENSO event.
El Niño-Southern Oscillation
The 1997/98 ENSO event.
The 1997/98 ENSO event.
El Niño.
El Niño and La Niña.
Oceanic circulation- NADW
Weather Vocabulary.
El Nino.
El Niño/La Niña.
Oceanic Circulation and ENSO
Presentation transcript:

Meredith Taghon Physical Oceanography Fall 2015 Bigger Stronger Faster: Current El Niño

“Christ child” Coupled ocean-atmospheric phenomenon Characterized by warm southward flowing currents in the Equatorial Pacific ocean and weakening of the trade winds Irregular intervals of 2-7 years, but occurs on average every 3-4 years Last around months In occurrence for thousands of years according to tree rings and other geological evidence (AOML) El Niño is associated with changes in the Southern Oscillation, but they are NOT the same! High atmospheric sea level pressures in western tropical Pacific + Indian Ocean; low sea level pressures in southeastern tropical Pacific Definition and Detection

Atmospheric Process Weakening of trade winds in central and west Pacific regions El Niño Cause and Effect Oceanic Process Thermocline: depression in east, elevation in west Reduced upwelling efficiency Higher sea surface temperature (S) /data-access/EQSST_xt.gif

Cause and Effect Cont’d Atmospheric Process Weak easterly trade winds Oceanic Process Warm water moves eastward Easterly-displaced atmospheric heat source Huge changes in global weather patterns

Current El Niño vs. Prior El Niños

6 MEI multivariates: Northwest of Australia: very high P Northeast of Australia: very strong V s Along Equator: U w Central + eastern equatorial Pacific: S and A Dateline region of southern tropical Pacific: C Precipitation: Lower rainfall in large areas of Central America (including Amazon region), Caribbean, and India (monsoon rainfall has been 86% of expected values [WMO]); dryness has contributed to increased wildfires in Indonesia Argentina and Peru: increased rain and flooding Current Global Impact percent-more-precipitation-to-california/

“Definitions of El Nino, La Nina, and ENSO.” Tropical Atmospheric Ocean Project. National Oceanic and Atmospheric Administration, November Web. 27 November “El Niño/ENSO.” Atlantic Oceanographic and Meteorological Laboratory: Physical Oceanography Division. National Oceanic and Atmospheric Administration, 2 October Web. 28 November “Multivariate ENSO Index (MEI).” Earth System Research Laboratory. National Oceanic and Atmospheric Administration, November Web. 27 November Sutherlan, Scott. “As 2015 tops 5-yr record, El Niño may push 2016 even hotter.” The Weather Network. 28 November Web. 29 November may-push-2016-even-hotter-wmo/60387/ “WMO: 2015 likely to be Warmest on Record, Warmest Five Year Period.” World Meteorological Organization. 25 November Web. 27 November warmest-five-year-period References True/False: Days are longer as a result of El Niño events.