El Niño and the Winter Weather Outlook

Size: px
Start display at page:

Download "El Niño and the Winter Weather Outlook"

Transcription

1 El Niño and the Winter Weather Outlook 2015 NASEO Annual Meeting NWS Boston February 10, 2015 Jimmy Taeger Meteorologist National Weather Service San Diego September 15, 2015

2 Outline What is El Niño? El Niño Forecast How might El Niño affect the CONUS? Tropical Cyclones in the Atlantic Temperature and Precipitation Winter Weather Outlook 2

3 What is El Niño? Chris Farley on SNL Godzilla Youtube.com 3

4 What is El Niño? Easterly trade winds near the equator weaken, and allow sea surface temperatures (SSTs) in the eastern equatorial Pacific to warm due to less upwelling El Niño is a phenomenon in the equatorial Pacific Ocean defined by a five consecutive 3-month running mean of SST anomalies in the Niño 3.4 region that is above the threshold of +0.5 C. Niño Regions 4

5 What is El Niño? ( C) C. America Very Warm Australia 5

6 El Niño Forecast Strong El Niño conditions are currently present There is a >90% chance that El Niño will continue through Northern Hemisphere winter , and around an 85% chance it will last into early spring Strong Moderate Weak Yellow Line is the Average Forecast Official forecast peaks near 2.5ºC 3-Month Running Means 6

7 What is El Niño? SST anomalies from 1950-present in the Nino 3.4 region Circled years were strong (>1.5ºC) El Niño years in the winter Strong Years 7

8 How Might El Niño Affect the CONUS? TROPICAL CYCLONES IN THE ATLANTIC El Niño increases shear and enhances sinking air over portions of the Atlantic Updated 2015 Atlantic Hurricane Season Outlook (Issued August 6 th ) Named Storms: 6-10 Hurricanes: 1-4 Major Hurricanes: 0-1 NOAA Season Type Average Number of Tropical Storms Average Number of Hurricanes Average Number of Major* Hurricanes Above-Normal Near-Normal Below-Normal *Major hurricanes have sustained winds of 111 mph or greater (Category 3,4 or 5) 8

9 How Might El Niño Affect the CONUS? TROPICAL CYCLONES IN THE ATLANTIC Tropical cyclone activity usually peaks around September 10 th NOTE: Disastrous hurricanes can still impact the U.S. during El Niño years 9

10 How Might El Niño Affect the CONUS? TEMPERATURE AND PRECIPITATION January through March Warmer in the Pacific Northwest and the northern Rockies Cool from New Mexico to South Carolina Wet over the extreme southern half of the CONUS 10

11 How Might El Niño Affect the CONUS? TEMPERATURE AND PRECIPITATION Winter (DJF) Climate Normals Temperature (ºF) Precipitation (in) 11

12 How Might El Niño Affect the CONUS? TEMPERATURE AND PRECIPITATION DJF Climate Anomalies for Strong (>1.5ºC) El Niño Years - Warmer northern CONUS - Cooler southern CONUS - Wetter coasts and southern CONUS - Below norm. OH Valley, and near norm. elsewhere 12

13 How Might El Niño Affect the CONUS? TEMPERATURE AND PRECIPITATION DJF Climate Anomalies for Strong (>2ºC) El Niño Years - Warmer Northeast and Midwest - Cooler southcentral and southwest CONUS - Wetter coasts, southern CONUS and Midwest - Below norm. OH Valley, and near norm. elsewhere 13

14 How Might El Niño Affect the CONUS? TEMPERATURE AND PRECIPITATION DJF Climate Anomalies for the Strongest El Niño (2.3ºC) on record - Warmer, except extreme S. and SW CONUS - Cooler S. California, Arizona and New Mexico - Wetter coasts and southern CONUS - Below norm. OH Valley, and near norm. elsewhere 14

15 Winter Weather Outlook Climate Prediction Center Winter Probability Outlook Temperature Precipitation A A B B B B A A Greater chances and higher confidence of - Colder and wetter than normal winter in southern portions of the CONUS - Warmer and Drier than normal winter in northern portions of the CONUS 15

16 Summary Strong El Niño forecast to continue through this winter SST anomalies in the Nino 3.4 region could rise to a new record high value Strong El Niño years in the winter tend to correlate to Warmer than normal in the northern CONUS Cooler than normal in the southern CONUS Wetter than normal in the southern CONUS and along the coasts, with below normal in the OH Valley, and near normal precipitation elsewhere CPC winter forecast similar to previous strong El Niño years, except for greater chances of below normal precipitation near the Northern Rockies and Great Lakes region 16

17 Thank You! Questions? Contact: Weather forecasts: weather.gov Useful Links El Niño and long-range forecasts: cpc.ncep.noaa.gov Climate anomaly maps: esrl.noaa.gov/psd/data/usclimdivs/ Tropical cyclone forecasts: hurricanes.gov 17

REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330

REMINDERS: UPCOMING REVIEW SESSIONS: - Thursday, Feb 27, 6:30-8:00pm in HSS 1330 REMINDERS: Midterm 2: Friday, February 28 - lecture material covering chapters 6, 7, and 15 (since first midterm and through Wed lecture) - same Format as first midterm UPCOMING REVIEW SESSIONS: - Thursday,

More information

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville The General Circulation and El Niño Dr. Christopher M. Godfrey University of North Carolina at Asheville Global Circulation Model Air flow broken up into 3 cells Easterlies in the tropics (trade winds)

More information

Equatorial upwelling. Example of regional winds of small scale

Equatorial upwelling. Example of regional winds of small scale Example of regional winds of small scale Sea and land breezes Note on Fig. 8.11. Shows the case for southern hemisphere! Coastal upwelling and downwelling. Upwelling is caused by along shore winds, that

More information

APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007

APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007 APPENDIX B NOAA DROUGHT ANALYSIS 29 OCTOBER 2007 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP October 29, 2007 Outline Overview Recent

More information

ENSO Wrap-Up. Current state of the Pacific and Indian Ocean

ENSO Wrap-Up. Current state of the Pacific and Indian Ocean 18-11-2014 ENSO Wrap-Up Current state of the Pacific and Indian Ocean Tropical Pacific Ocean moves closer to El Niño The Pacific Ocean has shown some renewed signs of El Niño development in recent weeks.

More information

ENSO Update Eastern Region. Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016

ENSO Update Eastern Region. Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016 ENSO Update Eastern Region Michelle L Heureux Climate Prediction Center / NCEP/ NOAA 29 November 2016 Summary La Niña conditions are present.* ENSO Alert System Status: La Niña Advisory Equatorial sea

More information

March 4 th, 2019 Sample Current Affairs

March 4 th, 2019 Sample Current Affairs March 4 th, 2019 Sample Current Affairs 1. A weak El Niño is developing in the equatorial Pacific Ocean, which is expected to continue for a few months at least. What is El Nino? What causes El Nino? What

More information

Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America. Dr. Art Douglas Professor Emeritus Creighton University

Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America. Dr. Art Douglas Professor Emeritus Creighton University Recent Atmospheric and Oceanic Circulation Changes Affecting Winter Weather in North America Dr. Art Douglas Professor Emeritus Creighton University Outline 1. The 2018 El Nino: A Northern Hemisphere induced

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 8 March 2010

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 8 March 2010 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 8 March 2010 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 4 September 2012

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 4 September 2012 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 4 September 2012 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

Lecture 13. Global Wind Patterns and the Oceans EOM

Lecture 13. Global Wind Patterns and the Oceans EOM Lecture 13. Global Wind Patterns and the Oceans EOM Global Wind Patterns and the Oceans Drag from wind exerts a force called wind stress on the ocean surface in the direction of the wind. The currents

More information

What Can We Expect From El Niño This Winter?

What Can We Expect From El Niño This Winter? What Can We Expect From El Niño This Winter? Water Forum September 8, 2015 Pete Fickenscher Senior Hydrologist NOAA / National Weather Service California-Nevada River Forecast Center Sacramento, CA What

More information

Tropical Pacific Ocean remains on track for El Niño in 2014

Tropical Pacific Ocean remains on track for El Niño in 2014 1 of 10 3/06/2014 3:33 PM ENSO Wrap-Up Current state of the Pacific and Indian Ocean Tropical Pacific Ocean remains on track for El Niño in 2014 Issued on Tuesday 3 June 2014 Product Code IDCKGEWWOO The

More information

Monitoring and prediction of El Niño and La Niña

Monitoring and prediction of El Niño and La Niña Monitoring and prediction of El Niño and La Niña Akio NARUI El Niño Monitoring and Prediction Group Climate Prediction Division Japan Meteorological Agency Outline 1. Introduction of El Niño and La Niña

More information

GEOS 201 Lab 13 Climate of Change InTeGrate Module Case studies 2.2 & 3.1

GEOS 201 Lab 13 Climate of Change InTeGrate Module Case studies 2.2 & 3.1 Discerning Patterns: Does the North Atlantic oscillate? Climate variability, or short term climate change, can wreak havoc around the world. Dramatic year to year shifts in weather can have unanticipated

More information

Lecture 29. The El-Niño Southern Oscillation (ENSO) La Niña = the girl; corresponds to the opposite climate situation

Lecture 29. The El-Niño Southern Oscillation (ENSO) La Niña = the girl; corresponds to the opposite climate situation Lecture 29 The El-Niño Southern Oscillation (ENSO) El Niño is Spanish for Christ child, the name given by fishermen to a warm ocean current off the coast of Peru/Ecuador that in some years occurs near

More information

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts (1 of 14) Further Reading: Chapter 07 of the text book Outline - terminology - characteristics of ENSO -impacts (2 of 14) Today: Introduction We want to look at another source of variability in the atmosphere

More information

Intermountain West Climate Summary

Intermountain West Climate Summary Intermountain West Climate Summary A product of The Western Water Assessment Issued October 2010 Vol. 6, Issue 6 ENSO and Intermountain West Water Supply: A Review of Water Year 2010 and Outlook for Water

More information

Applied Earth Science Climate Exam Practice Questions Page 1

Applied Earth Science Climate Exam Practice Questions Page 1 Name: 1. Which combination of climate factors generally results in the coldest temperatures? A) low elevation and low latitude B) low elevation and high latitude C) high elevation and low latitude D) high

More information

Ocean Inter-annual Variability: El Niño and La Niña. How does El Niño influence the oceans and climate patterns?

Ocean Inter-annual Variability: El Niño and La Niña. How does El Niño influence the oceans and climate patterns? Name: Date: Guiding Question: Ocean Inter-annual Variability: El Niño and La Niña How does El Niño influence the oceans and climate patterns? Introduction What is El Niño/La Niña? The El Niño/La Niña cycle

More information

Variability in the tropical oceans - Monitoring and prediction of El Niño and La Niña -

Variability in the tropical oceans - Monitoring and prediction of El Niño and La Niña - Variability in the tropical oceans - Monitoring and prediction of El Niño and La Niña - Jun ichi HIROSAWA Climate Prediction Division Japan Meteorological Agency SST anomaly in Nov. 1997 1 ( ) Outline

More information

El Niño Lecture Notes

El Niño Lecture Notes El Niño Lecture Notes There is a huge link between the atmosphere & ocean. The oceans influence the atmosphere to affect climate, but the atmosphere also influences the ocean, which can also affect climate.

More information

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4 Lecture 13 March 24, 2010, Wednesday Atmospheric Pressure & Wind: Part 4 Synoptic scale winds Mesoscale winds Microscale winds Air-sea interactions The largest synoptic scale wind. Monsoon: Arabic for

More information

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture!

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture! Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction Previous Lecture! Global Winds General Circulation of winds at the surface and aloft Polar Jet Stream Subtropical Jet Stream Monsoons 1 2 Radiation

More information

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere Chapter 7: Circulation of the Atmosphere The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University Scales of Atmospheric Motion Small-

More information

How fast will be the phase-transition of 15/16 El Nino?

How fast will be the phase-transition of 15/16 El Nino? How fast will be the phase-transition of 15/16 El Nino? YOO-GEUN HAM D E P A R T M E N T O F O C E A N O G R A P H Y, C H O N N A M N A T I O N A L U N I V E R S I T Y 2015/16 El Nino outlook One of strongest

More information

El Nino/La Nina. What is El Nino? From NOAA website

El Nino/La Nina. What is El Nino? From NOAA website El Nino/La Nina What is El Nino? From NOAA website El Nino was originally recognized by fishermen off the coast of South America as the appearance of unusually warm water in the Pacific Ocean, occurring

More information

General Introduction to Climate Drivers and BoM Climate Services Products

General Introduction to Climate Drivers and BoM Climate Services Products General Introduction to Climate Drivers and BoM Climate Services Products Climate Information Services Australian Bureau of Meteorology Yuriy Kuleshov El Niño Southern Oscillation (ENSO) El Niño Southern

More information

Weather EOG Review Questions

Weather EOG Review Questions Weather EOG Review Questions 1. Which statement best describes runoff? A Water vapor cools off and changes into water droplets. B Water in the form of rain, snow, sleet, or hail falls from clouds. C Precipitation

More information

El Niño Unit (2.5 pts)

El Niño Unit (2.5 pts) T. James Noyes, El Camino College El Niño Unit (Topic 9B) page 1 Name: Section: El Niño Unit (2.5 pts) El Niño is a warm ocean current that flows along the Equator and towards the west coast of South America

More information

Name: OBJECTIVES: By the end of today s lesson, you will be able to

Name: OBJECTIVES: By the end of today s lesson, you will be able to 7 th Grade Science Unit: Water s Cycles and Patterns Lesson: WCP 21 Name: Date: Monday, October 3, 2016 Homeroom: _ OBJECTIVES: By the end of today s lesson, you will be able to SWBAT Explain how currents

More information

Understanding El Nino-Monsoon teleconnections

Understanding El Nino-Monsoon teleconnections Understanding El Nino-Monsoon teleconnections Dr Neena Joseph Mani Earth & Climate Science INSA Anniversary General meeting, Session: Science in IISER Pune 27 th December 2017 Mean State of the equatorial

More information

Atmospheric Circulation. Recall Vertical Circulation

Atmospheric Circulation. Recall Vertical Circulation Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

3.1 (Read section 3.1), starts p.80

3.1 (Read section 3.1), starts p.80 3.1 (Read section 3.1), starts p.80 Write down these definitions in your notes as you find them when you read: 1. 2. 3. 4. Climate Convection specific heat capacity weather Then turn to p 87 READING CHECK

More information

2015 Evelyn Browning Garriss. El Niño, the Twisted Atlantic and the Effect on Global Agriculture

2015 Evelyn Browning Garriss. El Niño, the Twisted Atlantic and the Effect on Global Agriculture 2015 Evelyn Browning Garriss El Niño, the Twisted Atlantic and the Effect on Global Agriculture Conclusions Climate change is not linear. It ebbs and flows. Recent polar volcano eruptions created a cool

More information

Currents. History. Pressure Cells 3/13/17. El Nino Southern Oscillation ENSO. Teleconnections and Oscillations. Neutral Conditions

Currents. History. Pressure Cells 3/13/17. El Nino Southern Oscillation ENSO. Teleconnections and Oscillations. Neutral Conditions Teleconnections and Oscillations Teleconnection climate anomalies being related to each other over a large scale Oscillations: Macroscale movement of atmospheric systems that can influence weather, climate,

More information

Atmospheric Circulation. Recall Vertical Circulation

Atmospheric Circulation. Recall Vertical Circulation Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and El Niño Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection.

Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection. Fluid Circulation (Student Mastery Objectives) -The most frequent type of heat transfer of energy in the atmosphere is convection. -Differences in density affect the circulation of fluids. Cold air is

More information

Class Notes: Week 10. April 9 th,2019. Topics: Front and Mid-Latitude Wave Cyclones El Niño / La Niña Mid-term 2 review

Class Notes: Week 10. April 9 th,2019. Topics: Front and Mid-Latitude Wave Cyclones El Niño / La Niña Mid-term 2 review Class Notes: Week 10 April 9 th,2019 Topics: Front and Mid-Latitude Wave Cyclones El Niño / La Niña Mid-term 2 review Front- is a boundary between 2 different types of air masses Air masses with different

More information

Climate briefing. Wellington region, February Alex Pezza and Mike Thompson Environmental Science Department

Climate briefing. Wellington region, February Alex Pezza and Mike Thompson Environmental Science Department Climate briefing Wellington region, February 2016 Alex Pezza and Mike Thompson Environmental Science Department For more information, contact the Greater Wellington Regional Council: Wellington PO Box

More information

Chapter 10: Global Wind Systems

Chapter 10: Global Wind Systems Chapter 10: Global Wind Systems Three-cell model of atmospheric circulation Intertropical Convergence Zone (ITCZ) Typical surface wind patterns Upper-level pressure and winds Climatological sea-level pressure

More information

Origin of Inter-model uncertainty in ENSO amplitude change

Origin of Inter-model uncertainty in ENSO amplitude change Origin of Inter-model uncertainty in ENSO amplitude change Shang-Ping Xie Scripps Institution of Oceanography, UCSD Zheng, X.T., S.-P. Xie, L.H. Lv, and Z.Q. Zhou, 2016: Intermodel uncertainty in ENSO

More information

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore L A NIÑA El Niño-Southern Oscillation (ENSO) For the complete encyclopedic

More information

Global Impacts of El Niño on Agriculture

Global Impacts of El Niño on Agriculture Global Impacts of El Niño on Agriculture Presented to the University of Arkansas Division of Agriculture s Food and Agribusiness Series Webinar Series Presented by: Mark Brusberg and Brian Morris USDA

More information

OCEANOGRAPHY 101. Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River.

OCEANOGRAPHY 101. Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River. OCEANOGRAPHY 101 EXAM 2 WINTER 00 NAME STUDENT NUMBER 1 Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River. P a c i f i c O c e a n X WA Columbia

More information

ENSO Jigsaw [Key Science Knowledge Module]

ENSO Jigsaw [Key Science Knowledge Module] ` 3 Teacher Edition 2-3 days ENSO Jigsaw [Key Science Knowledge Module] Activity Overview This module is the most important learning module in terms of the physical science aspects associated with the

More information

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere Chapter 10 General refers to the average air flow, actual winds will vary considerably. Average conditions help identify driving forces. The basic cause of the general circulation is unequal heating of

More information

Lecture 24. El Nino Southern Oscillation (ENSO) Part 1

Lecture 24. El Nino Southern Oscillation (ENSO) Part 1 Lecture 24 El Nino Southern Oscillation (ENSO) Part 1 The most dominant phenomenon in the interannual variation of the tropical oceanatmosphere system is the El Nino Southern Oscillation (ENSO) over the

More information

Chart Discussion: Fri-17-Aug-2018 (Harvey Stern) Combining Forecasts (Apr 13th to Aug 15th)

Chart Discussion: Fri-17-Aug-2018 (Harvey Stern) Combining Forecasts (Apr 13th to Aug 15th) Combining Forecasts (Apr 13th to Aug 15th) 1 Last Week s Rainfall 1 Chart Discussion: Fri-17Aug-2018 (Harvey Stern) Last Week s Surface Charts 3 Chart Discussion: Fri-17Aug-2018 (Harvey Stern) This Month

More information

ATS150: Global Climate Change. Oceans and Climate. Icebergs. Scott Denning CSU 1

ATS150: Global Climate Change. Oceans and Climate. Icebergs. Scott Denning CSU 1 The Oceans Wind-Driven Gyre Circulations Icebergs Scott Denning CSU 1 Surface Balance of Forces friction coriolis wind stress resultant current Wind stress accelerates surface water Friction couples surface

More information

and the Link between Oceans, Atmosphere, and Weather

and the Link between Oceans, Atmosphere, and Weather Geography Worksheet Instructions Using a map, atlas, or any other materials your teacher suggests, label the following on the blank map provided. 1. Label East, West, North, and South. 2. Label the following

More information

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are.

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. 1. A cool breeze is blowing toward the land from the ocean on a warm, cloudless summer day. This condition is

More information

Large-Scale Overview of YOTC Period (ENSO, MJO, CCEWs,.)

Large-Scale Overview of YOTC Period (ENSO, MJO, CCEWs,.) WCRP /WWRP-THORPEX YOTC Implementation Planning Meeting East-West Center, University of Hawaii July 13-15, 2009 Large-Scale Overview of YOTC Period (ENSO, MJO, CCEWs,.) Matthew Wheeler Centre for Australian

More information

Long-Lead Climate Outlook and the Role of ENSO in High Plains Drought

Long-Lead Climate Outlook and the Role of ENSO in High Plains Drought Long-Lead Climate Outlook and the Role of ENSO in High Plains Drought Klaus Wolter NOAA-Earth System Research Lab & University of Colorado at Boulder-CDC klaus.wolter@noaa.gov Kudos to Chad McNutt for

More information

OCN 201 Lab Fall 2009 OCN 201. Lab 9 - El Niño

OCN 201 Lab Fall 2009 OCN 201. Lab 9 - El Niño OCN 201 Lab Fall 2009 OCN 201 Lab 9 - El Niño El Niño is probably one of the most widely publicized oceanic phenomena. If there s one single reason for that it s probably the fact that El Niño s presence

More information

3. Climatic Variability. El Niño and the Southern Oscillation Madden-Julian Oscillation Equatorial waves

3. Climatic Variability. El Niño and the Southern Oscillation Madden-Julian Oscillation Equatorial waves Georges (1998) 3. Climatic Variability El Niño and the Southern Oscillation Madden-Julian Oscillation Equatorial waves ENVIRONMENTAL CONDITIONS FOR TROPICAL CYCLONES TO FORM AND GROW Ocean surface waters

More information

Current: large mass of continuously moving ocean water

Current: large mass of continuously moving ocean water Ocean Currents Current: large mass of continuously moving ocean water Surface Currents--Wind Circulation These waters make up about 10% of all the water in the ocean. These waters are the upper 400 meters

More information

2 Air Masses and Fronts

2 Air Masses and Fronts CHAPTER 16 2 Air Masses and Fronts SECTION Understanding Weather BEFORE YOU READ After you read this section, you should be able to answer these questions: How is an air mass different from a front? How

More information

IX. Upper Ocean Circulation

IX. Upper Ocean Circulation IX. Upper Ocean Circulation World Ocean Covers 71% of Earth s surface Contains 97% of surface water Arctic Ocean NH: 61% ocean, 39% land Pacific Ocean Atlantic Ocean Southern Ocean Indian Ocean SH: 81%

More information

& La Niña Southern Oscillation Index

& La Niña Southern Oscillation Index El Niño & La Niña Southern Oscillation Index Today: first of the natural changes Lectures 1) El Nino/La Nina: year- decadal changes in climate system 2) Next: Short term natural changes (centuries to millenia)

More information

For Class Today How does ocean water circulate? Ocean currents, surface currents, gyres, currents & climate, upwelling, deep ocean circulation

For Class Today How does ocean water circulate? Ocean currents, surface currents, gyres, currents & climate, upwelling, deep ocean circulation For Class Today Modified Cornell Notes on section 16.1 (pg. 448-453) **Follow the guide in your ISN and previous notes for help** Heading: How does ocean water circulate? Left hand side categories: Ocean

More information

Pacific Climate Variability

Pacific Climate Variability Pacific Climate Variability Pacific Islands Climate Education Partnership You may have heard the term climate variability. What does the term climate variability mean? What are the causes and effects of

More information

Wednesday, September 27, 2017 Test Monday, about half-way through grading. No D2L Assessment this week, watch for one next week

Wednesday, September 27, 2017 Test Monday, about half-way through grading. No D2L Assessment this week, watch for one next week Wednesday, September 27, 2017 Test Monday, about half-way through grading No D2L Assessment this week, watch for one next week Homework 3 Climate Variability (due Monday, October 9) Quick comment on Coriolis

More information

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO?

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO? Background The changing temperatures of the tropical Pacific Ocean affect climate variability all over Earth. Ocean warming and cooling dramatically affect human activities by changing weather patterns

More information

Trade winds How do they affect the tropical oceans? 10/9/13. Take away concepts and ideas. El Niño - Southern Oscillation (ENSO)

Trade winds How do they affect the tropical oceans? 10/9/13. Take away concepts and ideas. El Niño - Southern Oscillation (ENSO) El Niño - Southern Oscillation (ENSO) Ocean-atmosphere interactions Take away concepts and ideas What is El Niño, La Niña? Trade wind and Walker circulation. What is the Southern Oscillation? Tropical

More information

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams arise because the Coriolis force prevents Hadley-type

More information

Air Pressure and Wind

Air Pressure and Wind Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways. The

More information

Becky Bolinger NIDIS IMW Drought Early Warning System Webinar November 21, 2017

Becky Bolinger NIDIS IMW Drought Early Warning System Webinar November 21, 2017 NIDIS Intermountain West Dec-Feb Winter Outlook Becky Bolinger NIDIS IMW Drought Early Warning System Webinar November 21, 2017 COLORADO CLIMATE CENTER La Niña Advisory And associated impacts from La Niña

More information

Monday, October 2, Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website)

Monday, October 2, Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website) Monday, October 2, 2017 Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website) Homework 3 Due date Wednesday, Oct 11 (8 pm) Be ready to watch another important

More information

MFE 659 Lecture 2b El Niño/La Niña Ocean-Atmosphere Interaction. El Niño La Niña Ocean-Atmosphere Interaction. Intro to Ocean Circulation

MFE 659 Lecture 2b El Niño/La Niña Ocean-Atmosphere Interaction. El Niño La Niña Ocean-Atmosphere Interaction. Intro to Ocean Circulation MFE 659 Lecture 2b El Niño/La Niña Ocean-Atmosphere Interaction El Niño La Niña Ocean-Atmosphere Interaction Outline Ocean Circulation El Niño La Niña Southern Oscillation ENSO 1 2 Intro to Ocean Circulation

More information

Goals for today: continuing Ch 8: Atmospheric Circulation and Pressure Distributions. 26 Oct., 2011

Goals for today: continuing Ch 8: Atmospheric Circulation and Pressure Distributions. 26 Oct., 2011 Goals for today: 26 Oct., 2011 continuing Ch 8: Atmospheric Circulation and Pressure Distributions Examples of synoptic scale and mesoscale circulation systems that are driven by geographic diversity in

More information

3 Global Winds and Local Winds

3 Global Winds and Local Winds CHAPTER 15 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?

More information

Chapter. Air Pressure and Wind

Chapter. Air Pressure and Wind Chapter Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. 19.1 Understanding Air Pressure Air Pressure Defined Air pressure

More information

Atmospheric and Ocean Circulation Lab

Atmospheric and Ocean Circulation Lab Atmospheric and Ocean Circulation Lab name Key Objectives: The main goal of this lab is to learn about atmospheric and oceanic circulation and how these two processes are strongly inter-dependent and strongly

More information

Review for the second quarter. Mechanisms for cloud formation

Review for the second quarter. Mechanisms for cloud formation Review for the second quarter Mechanisms for cloud formation 1 Rising air expands and cools; Sinking air compresses and warms. (18) (24) Dry adiabatic lapse rate (10 o C/km): the rate of temperature decrease

More information

Winds and Ocean Circulations

Winds and Ocean Circulations Winds and Ocean Circulations AT 351 Lab 5 February 20, 2008 Sea Surface Temperatures 1 Temperature Structure of the Ocean Ocean Currents 2 What causes ocean circulation? The direction of most ocean currents

More information

Record-breaking La Niña events

Record-breaking La Niña events Record-breaking La Niña events An analysis of the La Niña life cycle and the impacts and significance of the 2010 11 and 2011 12 La Niña events in Australia Contents Introduction At a glance: the impact

More information

ATOMOSPERIC PRESSURE, WIND & CIRCULATION

ATOMOSPERIC PRESSURE, WIND & CIRCULATION ATOMOSPERIC PRESSURE, WIND & CIRCULATION A. INTRODUCTION Important because: pressure patterns drive wind patterns which in turn drive oceanic circulation patterns o atmospheric & oceanic circulation: major

More information

Changing Climate and the Outlook

Changing Climate and the Outlook Changing Climate and the Outlook for Oilseed 2016 Evelyn Browning Garriss Conclusions Climate change is not linear. It ebbs and flows. There is a 90% chance the current El Niño will be strong and last

More information

Introduction to Oceanography OCE 1001

Introduction to Oceanography OCE 1001 Introduction to Oceanography OCE 1001 Lecture Notes Chantale Bégin & Jessica Fry Version 2.1 10. Ocean Circulation (Trujillo, Chapter 7) Major ocean currents are stable and predictable; they have been

More information

Arizona Climate Summary

Arizona Climate Summary Arizona Climate Summary March 2012 Summary of conditions for February 2012 February 2012 Temperature and Precipitation Summary February 1 st 17 th : February continued where January left off with a high

More information

9. The Earth's planetary winds are deflected as a result of the Earth's A) revolution around the Sun B) seasonal changes C) rotation on its axis D)

9. The Earth's planetary winds are deflected as a result of the Earth's A) revolution around the Sun B) seasonal changes C) rotation on its axis D) 1. Which ocean current transports warm water away from Earth s equatorial region? A) Brazil Current B) Guinea Current C) Falkland Current D) California Current 2. The Gulf Stream and North Atlantic Current

More information

El Niño as a drought-buster in Texas: How reliable is it, or what can we expect this winter? Are the September rains a sign of things to come?

El Niño as a drought-buster in Texas: How reliable is it, or what can we expect this winter? Are the September rains a sign of things to come? U.S. Drought Monitor Forum, Austin 8oct09 El Niño as a drought-buster in Texas: How reliable is it, or what can we expect this winter? Are the September rains a sign of things to come? Klaus Wolter (klaus.wolter@noaa.gov)

More information

El Nino and Global Warming

El Nino and Global Warming El Nino and Global Warming El Niño and Global Warming El Niño Climate Trade winds Barometric pressure Southern oscillation WHAT YOU WILL LEARN 1. You will identify the cause of El Niño events. 2. You will

More information

Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012.

Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012. Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012. We learned that it takes 3 years to complete one circuit of the North Pacific Gyre flow in the

More information

Lesson: Ocean Circulation

Lesson: Ocean Circulation Lesson: Ocean Circulation By Keith Meldahl Corresponding to Chapter 9: Ocean Circulation As this figure shows, there is a connection between the prevailing easterly and westerly winds (discussed in Chapter

More information

Overview. Learning Goals. Prior Knowledge. UWHS Climate Science. Grade Level Time Required Part I 30 minutes Part II 2+ hours Part III

Overview. Learning Goals. Prior Knowledge. UWHS Climate Science. Grade Level Time Required Part I 30 minutes Part II 2+ hours Part III Draft 2/2014 UWHS Climate Science Unit 3: Natural Variability Chapter 5 in Kump et al Nancy Flowers Overview This module provides a hands-on learning experience where students will analyze sea surface

More information

AT350 EXAM #2 November 18, 2003

AT350 EXAM #2 November 18, 2003 AT350 EXAM #2 November 18, 2003 Name and ID: Enter your name and student ID number on the answer sheet and on this exam. Record your answers to the 50 questions by using a No. 2 pencil to completely fill

More information

Chart Discussion: Fri-25-May-2018 Rainfall Last Week

Chart Discussion: Fri-25-May-2018 Rainfall Last Week Chart Discussion: Fri-25-May-2018 Rainfall Last Week 1 Last Week s Charts 2 MSL Analysis / Sat Image (Thu) 3 MSL Analysis / Sat Image (Fri) 4 Last Week s Model Forecasts OBSERVED Chart Discussion: Fri-25-May-2018

More information

Weather drivers in Victoria

Weather drivers in Victoria August 2008 Weather drivers in Victoria Key facts Major weather drivers in Victoria are: El Niño - Southern Oscillation frontal systems cut-off lows blocking highs Southern Annular Mode cloudbands Figure

More information

New Normal and La Niñas: Dealing with Natural Climate Now and in the Future James Jackson Garriss /Browning Media

New Normal and La Niñas: Dealing with Natural Climate Now and in the Future James Jackson Garriss /Browning Media New Normal and La Niñas: Dealing with Natural Climate Now and in the Future 2018 James Jackson Garriss /Browning Media Conclusions Climate change is not linear. It ebbs and flows. Long term climate conditions

More information

GEOS 513 ENSO: Past, Present and Future

GEOS 513 ENSO: Past, Present and Future GEOS 513 ENSO: Past, Present and Future Jessica Conroy Department of Geosciences Stephen W. Bieda, III Department of Atmospheric Sciences February 22, 2006: Regional Teleconnections (Observations) References:

More information

Welcome to GCSE Geography. Where will it take us today?

Welcome to GCSE Geography. Where will it take us today? Welcome to GCSE Geography Where will it take us today? Topic 1.1: global hazards 1.1a: How can weather be hazardous? iii) El Nino, La Nina and their impact on drought 12/10/2018 Think back.. This a affects

More information

18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Measuring Air Pressure Air pressure barometer

18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Measuring Air Pressure Air pressure barometer 18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways.

More information

Atmospheric Circulation. Density of Air. Density of Air: H 2 O and Pressure effects

Atmospheric Circulation. Density of Air. Density of Air: H 2 O and Pressure effects Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Analysis of 2012 Indian Ocean Dipole Behavior

Analysis of 2012 Indian Ocean Dipole Behavior Analysis of 2012 Indian Ocean Dipole Behavior Mo Lan National University of Singapore Supervisor: Tomoki TOZUKA Department of Earth and Planetary Science, University of Tokyo Abstract The Indian Ocean

More information

GROWING SEASON TEMPERATURES

GROWING SEASON TEMPERATURES Ag-Weather Update: Review of Summer Growing Season & Update on the Wet Forecast for Fall & Winter Paul W. Brown Extension Specialist, Biometeorology College of Agriculture & Life Sciences University of

More information

3 Global Winds and Local Winds

3 Global Winds and Local Winds CHAPTER 6 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?

More information

Weather drivers in South Australia

Weather drivers in South Australia August 2008 Key facts Weather drivers in South Australia Major weather drivers in South Australia are: El Niño - Southern Oscillation frontal systems cut-off lows blocking highs Indian Ocean Dipole cloudbands

More information

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO?

Module 3, Investigation 1: Briefing 1 What are the effects of ENSO? Module 3, Investigation 1: Briefing 1 Background The changing temperatures of the tropical Pacific Ocean affect climate variability all over Earth. Ocean warming and cooling dramatically affect human activities

More information