Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998 (3) A moderate El Nino in 1987 Three fields: (a) Surface temperatures and anomalies.

Slides:



Advertisements
Similar presentations
El Niño. How do ocean currents affect weather and climate? Oceans store and transport heat. – High heat capacity – Stores and transports energy from the.
Advertisements

Evolution of the El Niño : The Role of Intraseasonal to Interannual Time Scale Dynamics Michael J. McPhaden NOAA/PMEL Seattle, Washington CLIVAR.
Essentials of Oceanography
Seasonal Climate Forecast (Forecast Method) (Revised: May 26, 2012) This product is published by the Oregon Department of Agriculture (ODA), in cooperation.
E l Nino-Southern Oscillation ENSO Richard H. Grumm and Paul Knight V_ February March 2002.
El Niño, La Niña and the Southern Oscillation
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
El Niño - Southern Oscillation (ENSO) Ocean-atmosphere interactions.
TropicalM. D. Eastin The El-Nino Southern Oscillation (ENSO) La Nina ImpactsEl Nino Impacts.
Chapter 7 Circulation of the Atmosphere The Atmosphere 9e Lutgens & Tarbuck Power Point by Michael C. LoPresto.
The 1997/98 ENSO event. Multivariate ENSO Index Index is based on 6 parameters relevant to phase.
SSH anomalies from satellite. Observed annual mean state Circulation creates equatorial cold tongues eastern Pacific Trades -> Ocean upwelling along Equator.
NATS Lecture 17 Air Masses. Supplemental References for Today’s Lecture Lutgens, F. K. and E. J. Tarbuck, 2001: The Atmosphere, An Introduction.
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
The 1997/98 ENSO event. Multivariate ENSO Index Index is based on 6 parameters relevant to phase.
Tahiti, Darwin, and pressure oscillations. SOI = Tahiti - Darwin (normalized)
Impacts of El Nino Observations Mechanisms for remote impacts.
El Nino and La Nina An important atmospheric variation that has an average period of three to seven years. Goes between El Nino, Neutral, and La Nina (ENSO.
El Nino Southern Oscillation (ENSO)
Chapter 7 Ocean Circulation: El Niño
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
Weather Discussion January 4. Year in Review SEATAC HAD THE WARMEST AVERAGE January TEMPERATURE EVER WITH 47.0 DEGREES BREAKING THE PREVIOUS RECORD.
What is Climate? The long term average of weather, usually 30 years+
“Where America’s Climate, Weather Ocean and Space Weather Services Begin” Michelle L’Heureux NOAA Climate Prediction Center December 3, 2009 El Niño: What.
Ocean Circulation: El Niño
Water Year Outlook. Long Range Weather Forecast Use a combination of long term predictors –Phase of Pacific Decadal Oscillation (PDO) –Phase of Atlantic.
El Nino! By: Katie Durham & Mike Magnuson The Climate Event of the Century.
1 Global Ocean Monitoring: Recent Evolution, Current Status, and Predictions Prepared by Climate Prediction Center, NCEP September 7, 2007
Consolidated Seasonal Rainfall Guidance for Africa, Jan 2013 Initial Conditions Summary Forecast maps Forecast Background – ENSO update – Current State.
GEU 0027: Meteorology Lecture 10 Wind: Global Systems.
Seasonal Outlook Long Range Forecast
La Niña and The U. S. Winter Outlook Mike Halpert, Deputy Director Climate Prediction Center / NCEP December, 2011.
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
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.
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation.
Section (ii) ENSO - Theory
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
El Niño – The Christ Child (in Spanish)
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.
Madden/Julian Oscillation: Recent Evolution, Current Status and Forecasts Update prepared by Climate Prediction Center / NCEP April 3, 2006.
Ocean Circulation: El Niño El Niño-Southern Oscillation (ENSO) El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in.
Anomalous Behavior Unit 3 Climate of Change InTeGrate Module Cynthia M. Fadem Earlham College Russian River Valley, CA, USA.
Winter Outlook for the Pacific Northwest: Winter 06/07 14 November 2006 Kirby Cook. NOAA/National Weather Service Acknowledgement: Climate Prediction Center.
Madden/Julian Oscillation: Recent Evolution, Current Status and Forecasts Update prepared by Climate Prediction Center / NCEP November 6, 2006.
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.
El Niño and La Niña El Niño is characterized by unusually warm ocean temperatures in the Equatorial Pacific, as opposed to La Niña, which characterized.
El Niño–Southern Oscillation (ENSO): What is it?
Complication in Climate Change
El Niño and La Niña.
Daylength Local Mesoscale Winds Chinook Winds (Foehn) Loma, MT: January 15, 1972, the temperature rose from -54 to 49°F (-48 to 9°C), a 103°F (58°C)
Air-Sea Interactions The atmosphere and ocean form a coupled system, exchanging heat, momentum and water at the interface. Emmanuel, K. A. 1986: An air-sea.
El Nino Southern Oscillation
El Niño and La Niña.
El Nino and La Nina An important atmospheric variation that has an average period of three to seven years. Goes between El Nino, Neutral, and La Nina (ENSO.
The El Niño/ Southern Oscillation (ENSO) Cycle Lab
AIR/SEA INTERACTION El Nino
El Nino and La Nina An important atmospheric variation that has an average period of three to seven years. Goes between El Nino, Neutral, and La Nina (ENSO.
El Nino and La Nina.
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
The Climate System TOPICS ENSO Impacts Seasonal Climate Forecasts
The 1997/98 ENSO event.
The 1997/98 ENSO event.
The 1997/98 ENSO event.
2.3.1(iii) Impacts of El Nino
El Niño and La Niña.
Summary Global Circulation
Impacts of El Nino Observations Mechanisms for remote impacts.
NATS Lecture 15 Atmo-Ocean Interactions El Niño-Southern Oscillation
Presentation transcript:

Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998 (3) A moderate El Nino in 1987 Three fields: (a) Surface temperatures and anomalies (b) Sea level pressure and anomalies (c) Precipitable water and anomalies

Colder than average

Lower than average pressure

Drier than average

Not all events have same amplitude…best to think of an analogy between El Nino and La Nina and summer and winter: there are things common to each winter to make it a useful concept, but each one is different owing to different weather, different amplitudes of temperature extremes, etc. El Ninos, particularly strong ones, are generally confined to a single 12 month interval. La Ninas may persist for a few consecutive years, so there the oscillation is not linear in nature.

NOAA/NCEP/CPC

Westerly Wind Bursts (like from an MJO) cause an ocean response

Delayed Oscillator Theory Initially, Kelvin is downwelling (bringing warmer SSTs), and Rossby is upwelling Rossby is much slower than Kelvin At reflection, wave type shift Key: The reflected Rossby from maritime continent becomes an UPWELLING Kelvin “Seeds of its own demise” If this were the only thing happening, would get a very regular oscillation

A real example

There must be more… Clearly there must be other companion mechanisms, with input from atmosphere, to get us to 3-5 (2-7) year irregular cycles – The original feedback theory – Recharge/discharge theory – Heat builds up in the equatorial region, discharged eastward and poleward during El Niño Lots of other theories (text), and active research

Monitoring 3.4 is frequently used because of signal of both convection and SST 1&2 warm first!

SOI = Tahiti - Darwin (normalized)

Niño Region SST Departures ( o C) Recent Evolution The latest weekly SST departures are: Niño ºC Niño ºC Niño ºC Niño ºC

SOI and Nino 3-4 index

Jet stream configur- ations

Global Effects

Mean number of days per season (November - March 1948 through 1993) in which precipitation exceeded 0.50 inches for Neutral years (top). Lower left map is the difference in this quantity between El Niño years and Neutral years. Lower right map is the difference in this quantity between La Niña years and Neutral years. North American Effects