Extreme Events and Climate Variability. Issues: Scientists are telling us that global warming means more extreme weather. Every year we seem to experience.

Slides:



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

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.
Mark Cane Lamont-Doherty Earth Observatory of Columbia University El Niño and the Southern Oscillation (ENSO): An Introduction.
Environmental Science 11/10/14
Climatology Lecture 8 Richard Washington Variability of the General Circulation.
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.
Extratropical climate. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the Walker circulation?
Impacts of El Nino Observations Mechanisms for remote impacts.
CLIMATE AND AIR/SEA INTERACTIONS. Ekman Spiral.
India’s Water Crisis El Niño, Monsoon, and Indian Ocean Oscillation.
Chapter 7 Ocean Circulation: El Niño
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
BASICS OF EL NIÑO- SOUTHERN OSCILLATION (ENSO) Ernesto R. Verceles PAGASA.
El Niño is characterized by unusually warm temperatures that move eastward toward Peru’s coast La Niña is characterized by unusually cool temperatures.
Climate and Climate Change. Climate Climate is the average weather conditions in an area over a long period of time. Climate is determined by a variety.
SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean.
An Overview of California Climate Michael Anderson, State Climatologist.
Climate Variability and Change: An Overview Leigh Welling Crown of the Continent Research Learning Center Glacier National Park.
Extreme Events and Climate Variability X. William Proenza, Director National Weather Service Southern Region Fort Worth, Texas.
Are Exceptionally Cold Vermont Winters Returning? Dr. Jay Shafer July 1, 2015 Lyndon State College 1.
El Niño outlook Eric Boldt Warning Coordination Meteorologist
Dynamic Climate An overview of Climate Oscillations.
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
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.
The Climate Chapter 25.
July 25, 2001 presents “Past, Present, and Future” Ed Kieser.
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.
Teleconnections Current Weather Current Weather Finish ENSO Finish ENSO North Atlantic and Arctic Oscillations North Atlantic and Arctic Oscillations Pacific.
Abnormal Weather October 22, Teleconnections Teleconnections: relationship between weather or climate patterns at two widely separated locations.
© 2005 Accurate Environmental Forecasting Climate and Hurricane Risk Dr. Dail Rowe Accurate Environmental Forecasting
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
Bellringer. Climate Climate is the average weather conditions in an area over a long period of time. – determined by a variety of factors including: latitude,
IGY and the Origins of El Niño/Southern Oscillation (ENSO) Research
Atmosphere and Climate ChangeSection 1 Bellringer.
What is the Difference Between Weather and Climate?
Material for Exam 2 starts HERE. Oceanic Currents Surface Currents –Cold = high latitude –Warm = low latitude –Gyres: circulate in which directions?
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
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.
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.
Winter Outlook for the Pacific Northwest: Winter 06/07 14 November 2006 Kirby Cook. NOAA/National Weather Service Acknowledgement: Climate Prediction Center.
MICHAEL A. ALEXANDER, ILEANA BLADE, MATTHEW NEWMAN, JOHN R. LANZANTE AND NGAR-CHEUNG LAU, JAMES D. SCOTT Mike Groenke (Atmospheric Sciences Major)
Mike McPhaden--El Niño & La Niña John Lyman--Global Warming Dick Feely--Ocean Acidification The Ocean’s Role in Climate Variability and Change NOAA/Pacific.
Teleconnections Current Weather Current Weather Finish ENSO Finish ENSO North Atlantic and Arctic Oscillations North Atlantic and Arctic Oscillations Pacific.
ENSO El Niño—Southern Oscillation  El Niño (Spanish for “the Child” in reference to baby Jesus) = warm surface current in equatorial eastern Pacific.
Climate Prediction: Products, Research, Outreach Briefing for NOAA’s Science Advisory Board March 19, 2002 National Weather Service Climate Prediction.
The unpredictability of GW and El Nino events leading to increasing natural hazards.
1. Why do we have climate zones? 2. Can pollution change a climate?
Climate and Global Dynamics Laboratory, NCAR
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)
Teleconnections.
ENSO Impacts in Central Andes
Warm Water Currents & Climate Cold Water Currents & Climate
Composite patterns of DJF U200 anomalies for (a) strong EAJS, (b) weak EAJS, (c) El Niño and (d) La Niña.
El Niño and La Niña.
An overview of Climate Oscillations
El Nino and La Nina.
El Niño-Southern Oscillation
Global Climate Change.
Ocean Circulation.
2.3.1(iii) Impacts of El Nino
El Niño and La Niña.
Impacts of El Nino Observations Mechanisms for remote impacts.
El Niño/ La Niña (ENSO) The cycle is the consequence of slow feedbacks in the ocean-atmosphere system acting alongside the strong air-sea interaction processes.
WMO El Niño/La Niña Update
Changes in surface climate of the tropical Pacific
Winter/Spring Outlook:
Presentation transcript:

Extreme Events and Climate Variability

Issues: Scientists are telling us that global warming means more extreme weather. Every year we seem to experience weather extremes. What is the origin of extreme events?

A Major Issue for All Countries Is Global Warming and Its Regional Impacts

Seasonal Climate Impacts Depend on the Simultaneous Influences of: Natural Climate Variability El Nino/La Nina Pacific Decadal Oscillation (PDO) Arctic Oscillation (weak impact in Tropics) Climate Change Atmospheric Noise Extreme Events are Mostly Related to Circulation Changes, i.e. to Variability

The El Nino/Southern Oscillation (ENSO) is a major factor in global climate variability.

The Pacific Decadal Oscillation (PDO) Typical wintertime Sea Surface Temperature (colors), Sea Level Pressure (contours) and surface windstress (arrows) anomaly patterns during warm and cool phases of PDO

Societal Impacts from 1997/98 El Nino

Major Weather-Related Natural Disasters (1999 La Nina)

Impacts of December 1999 Floods in Venezuela

Typical winter Weather Anomalies and Atmosphere Circulation Changes During El Nino & La Nina

Contributions to Surface Temperature Trend from

SUMMARY Extremes result from: - major climate anomalies (e.g. especially El Nino and La Nina in Tropics) - unusual atmospheric circulation patterns (mostly related to climate variability) - factors acting together for air temperature (e.g. ENSO, PDO, AO, global warming) The impacts of the warming trend on circulation changes, i.e. also extremes, is still a research issue