1 Trade Winds in Equatorial Pacific. 2 ITCZ Location July January ITCZ.

Slides:



Advertisements
Similar presentations
Current Variations Not all currents are driven by the wind.
Advertisements

Normal Conditions. The Walker Circulation El Niño Conditions.
ENSO El Niño Southern Oscillation Pages NORMAL conditions  Trade Winds  Cool water pools near S.America,  Warm water pools near Australia.
El Niño. How do ocean currents affect weather and climate? Oceans store and transport heat. – High heat capacity – Stores and transports energy from the.
Ocean and Atmosphere Coupling El-nino -- Southern Oscillation
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
El Nino, La Nina, and their Affects in Oklahoma. El Nino Conditions Warming of central and eastern equatorial Pacific waters Trade wind differences –
ENSO (El Nino Southern Oscillation) ENVS
2. Natural Climate Variability
SSH anomalies from satellite. Observed annual mean state Circulation creates equatorial cold tongues eastern Pacific Trades -> Ocean upwelling along Equator.
1 Surface Circulation Pathways Generally, warm currents move poleward and cool currents move equatorward.
El Nino – Southern Oscillation - Southern Oscillation (atmosphere) - El Nino (ocean) - change in equatorial Pacific circulation - produces global climate.
Generalized Surface Circulation
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
Southern Oscillation”
Chapter 5: Other Major Current Systems
El Nino Southern Oscillation (ENSO)
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
What Are the El Nino and La Nina?
Remember “normal” ocean circulation? El Nino? (warm) Trade winds weaken Thermocline drops Upwelling is cut off SST rises in E.Pacific High & Low pressure.
El Niño and La Niña By Mr. D. Atmospheric and oceanic disturbances in Pacific Ocean El Niño-Southern Oscillation (ENSO) –Warm {El Niño} and cold phases.
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.
“Where America’s Climate, Weather Ocean and Space Weather Services Begin” Michelle L’Heureux NOAA Climate Prediction Center December 3, 2009 El Niño: What.
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
What Are the El Nino and La Nina?. Review of last lecture Tropical cyclone genesis: Western Pacific has the highest averaged number per year. 6 necessary.
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.
1 Global Ocean Monitoring: Recent Evolution, Current Status, and Predictions Prepared by Climate Prediction Center, NCEP September 7, 2007
El Nino and La Nina opposite phases of the El Niño-Southern Oscillation (ENSO) cycle. The ENSO cycle describes the changes in temperature between the ocean.
Oceanic Influences on Climate. Ocean currents redistribute heat Large scale currents are called gyres.
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.
The El Niño Southern Oscillation (ENSO) Corey J Gabriel
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
1 Kelvin Waves El Niño October Ocean’s response to changing winds Ocean’s response to changing winds external (or surface)waves external (or surface)waves.
Ocean Circulation: El Niño El Niño-Southern Oscillation (ENSO) El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
Anomalous Behavior Unit 3 Climate of Change InTeGrate Module Cynthia M. Fadem Earlham College Russian River Valley, CA, USA.
Dr. Neil S. Suits. NASA/Goddard Space Flight Center, The SeaWiFS Project and GeoEye, Scientific Visualization Studio SeaWiFS Ocean Biosphere: 1997 to.
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–Southern Oscillation (ENSO): What is it?
El Niño and La Niña.
Global scale circulation
El Niño- Southern Oscillation
Teleconnections Zach Hiris/Phil Pascarelli
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)
Teleconnection Systems NAO AO PNA
El Nino Southern Oscillation
El Niño and La Niña.
An overview of Climate Oscillations
AIR/SEA INTERACTION El Nino
Differential Heating – Specific Heat
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.
Chapter 14: Section ). You will be able to define what an el niño and la niña Event is. 2). You should be able to explain what causes el niño.
ENSO El Nino / La Nina episodes of ocean warming and cooling
El Nino Southern Oscillation
Oceanic Influences on Climate
David Tedesco Physical Oceanography
El Niño - Southern Oscillation
Ocean Currents El Niño and La Niña.
(Pinet) Major ocean current systems 4 Surface patterns extend as deep as 1000 m 5.
El Niño and La Niña.
El Niño and La Niña.
El Niño and the Southern Oscillation (“ENSO”)
Changes in surface climate of the tropical Pacific
El Niño and the Southern Oscillation (“ENSO”) A quick look
Oceanic Circulation and ENSO
Presentation transcript:

1 Trade Winds in Equatorial Pacific

2 ITCZ Location July January ITCZ

3 Equatorial Divergence vs Subtropical Convergence upwellingdownwelling

4 Trade Winds Cause Variations in Sea Surface Height ITCZ SSH

5 Meridional Trends in Trade Wind Strength, Sea Surface Height, and Currents in the Equatorial Pacific Trade Wind Speed Surface Current Direction SSH (cm) Depth (m) HPG westward eastward ITCZ I------Conv------IDivIConI-Div-I---Conv---I

6 Zonal (E-W) Trend in Sea Surface Height Zonal (east-west) trend in Sea Surface Height Wind Stress SSH Temperature (+ = depth of EUC)

7 Equatorial Undercurrent AAAA 6 EUC Velocity (m/s) Temperature (ºC) Velocity Cross Sections

8 SST in Equatorial Pacific ºC

9 Surface Nitrate Distribution

10 Photosynthesis Rates in Surface Ocean

11 Cross Sections in the Equatorial Pacific Temp Salinity Oxygen Phosphate Zonal Vel.

12 Effect of El Nino on Anchovy Catch El Ninos in red

13 Array of Buoys Monitored by NOAA for Wind Speed, SST, Salinity, Current Velocities The best instrumented region of the world’s ocean

14 Sea Surface Temperature Changes

15 Weakening of Trade Winds during El Nino Normal El Nino

16 Atmospheric Circulation and Precipitation Changes during El Nino Normal El Nino

17 SST and Chlorophyll during El Nino El Nino Normal 9

18 Animation of SST Anomalies during El Nino of old_sst/sst_9798_anim.shtmlhttp:// old_sst/sst_9798_anim.shtml

19 History of Southern Oscillation Index (and correlation with El Nino events) ENSO Index

20 Change in Zonal Atmospheric Circulation in Equatorial Pacific

21 Global Weather Anomalies during El Nino

22 Global Weather Anomalies during La Nino

23 El Nino Effects on US Temperatures (Winter) Warmer in northern midwest and cooler in south

24 El Nino Effects on US Precipitation (Winter) Wetter in southeast US

25 El Nino Effects on Jet Stream position and US Weather

26 Currently El Nino Conditions (Nov 2009) SST anomaly is currently 1-4ºC warmer than normal (avg.= 1.5ºC).