The Effect of ENSO on Precipitation in Atlanta

Slides:



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

VEGETATION FEEDBACK AND DROUGHTS Russell Bird – 3 rd Year Atmospheric Science.
Analysis of Eastern Indian Ocean Cold and Warm Events: The air-sea interaction under the Indian monsoon background Qin Zhang RSIS, Climate Prediction Center,
3. Natural Climate Variability. SPM 1b Variations of the Earth’s surface temperature for the past 1,000 years Approx. climate range over the 900 years.
The Effects of El Niño-Southern Oscillation on Lightning Variability over the United States McArthur “Mack” Jones Jr. 1, Jeffrey M. Forbes 1, Ronald L.
Seasonal Climate Forecast (Forecast Method) (Revised: May 26, 2012) This product is published by the Oregon Department of Agriculture (ODA), in cooperation.
Teleconnection of Tropical Pacific and Indian Ocean Oscillation with Monsoon Rainfall Variability over Nepal 8/8/20141 Lochan P. Devkota & Ujjwal Tiwari.
El Nino, La Nina, and their Affects in Oklahoma. El Nino Conditions Warming of central and eastern equatorial Pacific waters Trade wind differences –
PDO/PNA The PDO (Pacific Decadal Oscillation) is an index derived from North Pacific sea surface temperature anomalies and it has a high correlation to.
Contemporaneous and Antecedent Links of Atlantic and Pacific Circulation Features with North American Hydroclimate: Structure and Interannual Variability.
Peru upwelling (Chl concentration) Peru Fishery.
INTERDECADAL OSCILLATIONS OF THE SOUTH AMERICAN MONSOON AND THEIR RELATIONSHIP WITH SEA SURFACE TEMPERATURE João Paulo Jankowski Saboia Alice Marlene Grimm.
Winter Outlook ( ) Winter Weather Forecast Conference OMSI / Oregon Chapter of the AMS 29 October 2011 Winter Weather Forecast Conference OMSI.
India’s Water Crisis El Niño, Monsoon, and Indian Ocean Oscillation.
Atmospheric Variability Why is it so cold winter ? Why was it so hot summer 2010? Why was it so dry in 2007? Why was it so wet in 1998, 2009 (fall)?
Bryson McNulty EAS-4480 Georgia Inst. Of Technology April 22 nd, 2014.
REBECCA KOLLMEYER EAS 4480 APRIL 24 TH, 2012 Impacts on Atlanta weather during winter by Central Pacific and Eastern Pacific El Nino.
Extreme Events and Climate Variability. Issues: Scientists are telling us that global warming means more extreme weather. Every year we seem to experience.
The Correlation between Atlantic Hurricane Frequency and ENSO Jessica Johnson EAS 4480 Spring 2012.
December 2002 Section 2 Past Changes in Climate. Global surface temperatures are rising Relative to average temperature.
The Effect of ENSO on Precipitation in San Diego, California Andrew Horan.
Christian Feliciano The Ohio State University Atmospheric Science.
The La Niña Influence on Central Alabama Rainfall Patterns.
CCA MADE EASY. The Science of Seasonal Climate Forecasting is all about connecting forcing and response. Once a forcing mechanism is identified the response.
Climate Change in the Yaqui Valley David Battisti University of Washington 1.Climatological Annual Cycle –Winter vs. Summer 2.Variability(Winter) –ENSO.
ENSO Variability in SODA: SULAGNA RAY BENJAMIN GIESE TEXAS A&M UNIVERSITY WCRP 2010, Paris, Nov
Abnormal Weather October 22, Teleconnections Teleconnections: relationship between weather or climate patterns at two widely separated locations.
The Madden-Julian Oscillation and North Atlantic Hurricanes Melissa Nord EAS 4480.
The ability to accurately predict climate in the New York metropolitan area has tremendous significance in terms of minimizing potential economic loss.
INTERANUAL VARIABILITY OF PRECIPITATION IN LA PLATA BASIN AND EL NINO (CANONICAL AND MODOKI) - BEHAVIOR OF HADLEY AND GFDL MODELS Renata G. Tedeschi 1.
Volcanic Climate Impacts and ENSO Interaction Georgiy Stenchikov Department of Environmental Sciences, Rutgers University, New Brunswick, NJ Thomas Delworth.
© 2005 Accurate Environmental Forecasting Climate and Hurricane Risk Dr. Dail Rowe Accurate Environmental Forecasting
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
Michelle Hsia Apr. 21, 2009 EAS4803. Objective To analyze data concerning wind direction and precipitation taken from a weather station. To use different.
1 Fourth IAP Meeting February ° Extreme Event: Winter US Tornado Outbreak --- Attribution challenge °2007 US Annual Precipitation Extremes ---
Winter/Spring Outlook Derrick Weitlich National Weather Service Melbourne Central Florida Prescribed Fire Council Annual Meeting September 25,
The CFS ensemble mean (heavy blue line) predicts La Nina will last through at least the Northern Hemisphere spring
El Niňo. El Nińo: A significant increase in sea surface temperature over the eastern and central equatorial Pacific that occurs at irregular intervals,
Extratropical Sensitivity to Tropical SST Prashant Sardeshmukh, Joe Barsugli, and Sang-Ik Shin Climate Diagnostics Center.
Using the National Multi-Model Ensemble (NMME) System Johnna Infanti Advisor: Ben Kirtman.
An Overview of the La Niña Michelle L’Heureux.
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)
ENSO Influence on Atlantic Hurricanes via Tropospheric Warming Brian Tang* and David Neelin Dept. of Atmospheric and Oceanic Sciences, UCLA Institute of.
29th Climate Diagnostic and Prediction Workshop 1 Boundary and Initial Flow Induced Variability in CCC-GCM Amir Shabbar and Kaz Higuchi Climate Research.
El Niño Phenomenon Relation with the Glaciers Retreat in the Andes By Juan Pablo Galarza, Maria Emilia Andrade and Juan Andrés Cajiao.
Exploring the Relationship Between North Atlantic and Global Temperature Anomalies Using Bivariate and Time Series Analysis EAS 4480 Ryan Schilling.
El Niño / Southern Oscillation
Has modulation of Indian Summer Monsoon Rainfall by Sea Surface Temperature of the equatorial Pacific Ocean, weakened in recent years? SRIVASTAVA et al.
Mentor: Dr. Jinchun Yuan
Challenges of Seasonal Forecasting: El Niño, La Niña, and La Nada
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.
Correlations between Atlantic SST and drought conditions
Alfredo Ruiz-Barradas, and Sumant Nigam
An overview of Climate Oscillations
El Nino and La Nina.
The Climate System TOPICS ENSO Impacts Seasonal Climate Forecasts
How is the Ocean affecting our Weather Today?
The Atmosphere: Part 9: Short term climate variability
The 1997/98 ENSO event.
Prospects for Wintertime European Seasonal Prediction
Ocean Currents El Niño and La Niña.
The 1997/98 ENSO event.
The 1997/98 ENSO event.
ENSO –El Niño Southern Oscillation
JSPS 5th University Allied Workshop on Climate and Environmental Studies for Global Sustainability Decadal change in the relationship between East Asian-western.
El Nino.
Section 2.3 Interannual Variability 
Volcanic Climate Impacts and ENSO Interaction
Ocean/atmosphere variability related to the development of tropical Pacific sea-surface temperature anomalies in the CCSM2.0 and CCSM3.0 Bruce T. Anderson,
Presentation transcript:

The Effect of ENSO on Precipitation in Atlanta Steven DiNapoli EAS 4803 YW April 22, 2008

Introduction Current Atlanta Drought Projected to continue due to La Niña conditions Many previous droughts were exacerbated by La Niña (e.g. 1950s, 2000) Objective of Analysis – Analyze relationship between ENSO and precipitation in Atlanta Performed correlations on historical ENSO data and monthly precipitation in Atlanta Hartsfield-Jackson International Airport

ENSO Data ONI – Oceanic Niño Index Measure of 3-month running mean SST anomalies in the Eastern Pacific Positive Values correspond to El Niño conditions

Atlanta Precipitation Hartsfield-Jackson International Airport Monthly totals from NCDC Much more variability than ONI data Numerous outlier points

Correlating the Data (Attempt #1) [r1, p1] = corrcoef(oni, precip);

Problems with Attempt #1 Too much noise in precipitation data Affected by outside influences (e.g. hurricanes) Outlier data points Correlation Coefficient = 0.0690 Explains less than 0.5% of precipitation variance p-Value = 0.0687 Correlation is statistically insignificant p-value should be less than 0.05 Need to filter noise out of precipitation data 3-month running mean precipitation ONI values are derived from a 3-month running mean

Correlating the Data (Attempt #2)

Problems with Attempt #2 Precipitation data still very noisy Correlation Coefficient = 0.1069 Still very weak; explains ~1% of the variance p-value = 0.0048 Correlation is significant More filtering still needed Next attempt correlates average ONI index for each year with total yearly precipitation

Visual Analysis of Filtered Data

Correlating the Data (Attempt #3)

Analysis of Attempt #3 Much less noise in the data Outlier points removed Correlation coefficient = 0.2462 Still weak, but much stronger than before p-value = 0.0625 Significance lost due to lack of data points (58 vs. 696) * Would regional precipitation totals provide a better dataset to correlate with ENSO?

Conclusion All major droughts occurred during La Niña Not all La Niña events lead to drought The opposite is not always true for El Niño Correlations were very weak Data was very noisy Long-wave synoptic patterns Hurricanes & convective thunderstorms La Nina conditions → More hurricanes Numerous other forcings ignored (e.g. NAO) Only one station considered

Questions?