Climate Change in the Yaqui Valley David Battisti University of Washington 1.Climatological Annual Cycle –Winter vs. Summer 2.Variability(Winter) –ENSO.

Slides:



Advertisements
Similar presentations
El Niño- Southern Oscillation
Advertisements

The Perfect Ocean for Drought, Martin Hoerling & Arun Kumar On the Cause of the 1930s Dust Bowl, Siegfried D. Schubert, Max J. Suarez, Philip J. Pegion,
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.
© Crown copyright Met Office Decadal Climate Prediction Doug Smith, Nick Dunstone, Rosie Eade, Leon Hermanson, Adam Scaife.
Climatology Lecture 8 Richard Washington Variability of the General Circulation.
Jim Noel Service Coordination Hydrologist March 2, 2012
Downstream weather impacts associated with atmospheric blocking: Linkage between low-frequency variability and weather extremes Marco L. Carrera, R. W.
2009 global climate: A tale of five timeseries Global mean temperature El Ni ñ o / Southern Oscillation (ENSO) Pacific Decadal Oscillation Annular modes.
The Role of Internally Generated Megadroughts and External Solar Forcing in Long Term Pacific Climate Fluctuations Gerald A. Meehl NCAR.
PDO research: a few new insights into lingering questions and a simple method for 1 year forecasting Nate Mantua Climate Impacts Group October 21, 2003.
Climate variations in the Northwest, seasonal climate forecasting, and outlook for winter Nate Mantua Climate Impacts Group University of Washington.
Climate Review for WY 2004 and Outlook for WY 2005 Philip Mote Climate Impacts Group University of Washington Annual Fall Forecast Meeting October 26,
New climate change scenarios for the Pacific Northwest Eric Salathé Climate Impacts Group University of Washington.
Climate recap and outlook Nate Mantua, PhD University of Washington Climate Impacts Group Nate Mantua, PhD University of Washington Climate Impacts Group.
Climate and Food Security Thank you to the Yaqui Valley and Indonesian Food Security Teams at Stanford 1.Seasonal Climate Forecasts 2.Natural cycles of.
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
El Nino Southern Oscillation (ENSO)
Pacific vs. Indian Ocean warming: How does it matter for global and regional climate change? Joseph J. Barsugli Sang-Ik Shin Prashant D. Sardeshmukh NOAA-CIRES.
Extreme Events and Climate Variability. Issues: Scientists are telling us that global warming means more extreme weather. Every year we seem to experience.
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.
The speaker took this picture on 11 December, 2012 over the ocean near Japan. 2014/07/29 AOGS 11th Annual Meeting in Sapporo.
The Caribbean Low Level Jet variability during August and September and its relation with the regional hydroclimate Ernesto Muñoz.
Climate Literacy Session: Climate, Climatology of California Elissa Lynn August 5, 2015.
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.
Climate: Outlook and Operational Planning Jayantha Obeysekera (’Obey’), Ph.D.,P.E.,D.WRE Department Director Hydrologic & Environmental Systems Modeling.
NERC Centre for Global Atmospheric Modelling Department of Meteorology, University of Reading The role of the land surface in the climate and variability.
Influence of the blended ship log book and station SLP data set on Mediterranean temperature & precipitation back to 1750 June Jürg Luterbacher.
The La Niña Influence on Central Alabama Rainfall Patterns.
Climate Change and Global Warming Michael E. Mann Department of Environmental Sciences University of Virginia Symposium on Energy for the 21 st Century.
Water Year Outlook. Long Range Weather Forecast Use a combination of long term predictors –Phase of Pacific Decadal Oscillation (PDO) –Phase of Atlantic.
The South American Monsoon System: Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 1 October 2012 For more information,
El Nino Teleconnections Philip Kreycik EPS 131 4/30/04.
“Effects of Pacific Sea Surface Temperature (SST) Anomalies on the Climate of Southern South Carolina and Northern Coastal Georgia ” Whitney Albright Joseph.
Climate of North America 101 What are the major controls on North American climate? What is the dominant flow pattern across North America in winter? How.
The role of the basic state in the ENSO-monsoon relationship and implications for predictability Andrew Turner, Pete Inness, Julia Slingo.
July 25, 2001 presents “Past, Present, and Future” Ed Kieser.
Abnormal Weather October 22, Teleconnections Teleconnections: relationship between weather or climate patterns at two widely separated locations.
Introduction 1. Climate – Variations in temperature and precipitation are now predictable with a reasonable accuracy with lead times of up to a year (
© 2005 Accurate Environmental Forecasting Climate and Hurricane Risk Dr. Dail Rowe Accurate Environmental Forecasting
Climate Model Simulations of Extreme Cold-Air Outbreaks (CAOs) Steve Vavrus Center for Climatic Research University of Wisconsin-Madison John Walsh International.
Coral records of El Niño and Tropical Pacific climate change Kim M. Cobb Harold Nations Symposium October 14, 2005.
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
1 Fourth IAP Meeting February ° Extreme Event: Winter US Tornado Outbreak --- Attribution challenge °2007 US Annual Precipitation Extremes ---
Global Climate Change: Past and Future Le Moyne College Syracuse, New York February 3, 2006 Department of Meteorology and Earth and Environmental Systems.
What is the Summer North Atlantic Oscillation (SNAO)?
Modeling North Pacific Decadal Variations and Their Teleconnection Patterns Speaker/ Pei-Ning Kirsten Feng Advisor/ Yu-Heng Tseng.
Global Climate Change: Past and Future 2006 Scott Margolin Lecture in Environmental Affairs Middlebury College Middlebury VT March 7, 2006 Michael E. Mann.
Reconciling droughts and landfalling tropical cyclones in the southeastern US Vasu Misra and Satish Bastola Appeared in 2015 in Clim. Dyn.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
Winter Outlook for the Pacific Northwest: Winter 06/07 14 November 2006 Kirby Cook. NOAA/National Weather Service Acknowledgement: Climate Prediction Center.
Climate Change and Global Warming Michael E. Mann Department of Environmental Sciences University of Virginia Waxter Environmental Forum Sweet Briar College.
The South American Monsoon System: Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 7 November 2011 For more information,
Climatology of the Río de la Plata Basin: short and long term variability Mario Bidegain Facultad de Ciencias Universidad de la Republica Uruguay Workshop.
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Impacts of Climate Change and Variability on Agriculture: Using NASA Models for Regional Applications Radley Horton 1, Cynthia Rosenzweig 2, and David.
The role of Atlantic ocean on the decadal- multidecadal variability of Asian summer monsoon Observational and paleoclimate evidences Observational and.
The South American Monsoon System: Recent Evolution and Current Status Update prepared by Climate Prediction Center / NCEP 4 June 2012 For more information,
El Niño-Southern Oscillation and regional rainfall of Vietnam Ramasamy Suppiah 10 December 2012.
Andrew Turner, Pete Inness, Julia Slingo
El Niño and La Niña.
Prospects for Wintertime European Seasonal Prediction
Global Climate Change.
Senior Meteorologist, WSI
Case Studies in Decadal Climate Predictability
Nonlinearity of atmospheric response
XiaoJing Jia Influence of Forced Large-Scale Atmospheric Patterns on winter climate in China XiaoJing Jia
Winter/Spring Outlook:
Presentation transcript:

Climate Change in the Yaqui Valley David Battisti University of Washington 1.Climatological Annual Cycle –Winter vs. Summer 2.Variability(Winter) –ENSO and Extreme Events 3.Trends and Climate Change 1.(wheat yield and climate) 4.Puzzles

1. The Annual Cycle Summer –Tropical storms, hurricane debris, (monsoon) Winter –El Nino/Southern Oscillation (ENSO) –Pacific North American Pattern –More

2. Interannual Variability Winter –El Nino/Southern Oscillation (ENSO) –Pacific North American Pattern –More Summer –Not today Extreme Events –Extended Drought Precipitation Anomalies (Lobell 2003)

ENSO ENSO warms offshore and cools to the east in the Sierra. ENSO brings winter rainfall to the Yaqui Valley catchment basin (r = 0.55) Temperature Anomalies Precipitation Anomalies (January-April)

The (+) PNA brings winter rainfall to the Yaqui Valley catchment basin (r=.6). The (+) PNA warms offshore and cools to the east in the Sierra. –Yaqui Valley is on a nodal line for PNA -- no signal. Precipitaiton Anomalies (January-April) The Pacific North American (PNA) Pattern Temperature Anomalies (January-April)

The mechanisms for the year-to-year variability in this ‘new’ pattern of natural variability are not known. The WP pattern does bring seasonal temperature and precipitation anomalies to the Yaqui Valley (warm/dry, cold/wet). Precipitation Anomalies (January-April) Temperature Anomalies (January-April) The West Pacific (WP) Pattern

The WP pattern does bring seasonal temperature and precipitation anomalies to the Yaqui Valley (warm/dry, cold/wet; r=0.5/0.7). The WP pattern is only weakly correlated to SST in the eastern Pacific. The West Pacific (WP) Pattern (cont) Temperature Anomalies (January-April)

Extreme Drought The instrument record of Yaqui Valley basin precipitation has been extended using tree ring data. Correlation of observed and reconstructed Nov-April rainfall is (Diaz et al. 2002) Precipitation Anomalies (Nov-April)

Extreme Drought The reconstructed precipitation record extends from 1650 to 1985 AD. The average return time for a drought similar to the present drought is about 20 years. Correlation of observed and reconstructed Jan-April rainfall is Precipitation Anomalies (November-April)

3. Trends and Climate Change Annual wheat yield in Yaqui Valley ( ) is highly correlated to the Jan-April average minimum daily temperature. Is this due to climate or management? Note: much of the relationship between minimum temperature and yield is interannual (r =0.7) (Lobell et al. 2003) Temp Yield

Yield and Climate Increased yield is related to –Less precipitation (r = 0.8!) –Reduced minimum temperatures –Cold SST immediately offshore –Warm SST in the western Pacific The PNA and the WP are weakly related to yield (r=-.31 and.42, respectively) Temperature Anomalies Precipitation Anomalies (January-April)

4. Conclusions Much of the variability in wintertime precipitation in the Yaqui Vally catchment is due to patterns of natural climate variability: ENSO, the PNA and the WP phenomenon. The local ocean SST conditions are probably not influencing Tmin: –ENSO, remotely forced atmospheric teleconnections (WP) and variability intrinsic to the atmosphere (PNA) are likely to be responsible. Some of the relationship between yield and climate could be explained by the collection of natural patterns of interannual variability: –The PNA and the WP are weakly related to yield (r =-.31 and.42, respectively) –Another Pattern is worth checking: the North Pacific pattern.

4. Conclusions The trend (20 year) in yield and minimum temperature are correlated with the 40 year (warming) trend in the western Pacific (WP). The latter has been argued in several studies to be due to increasing greenhouse gas concentrations (e.g., Hoerling et al. 2003) Warm Pool(WP) Index

4. Conclusions and Puzzles Problems: If the variability and trend in wheat yield are due to the natural variability in the PNA and WP (and the trend in WP), …. How do drier conditions (r=.7) lead to lower minimum daily temperatures? Does clearing lead to a greater diurnal temperature range, and hence a lower minimum daily temperature, even though the daily mean temperature might be rising? Summer vs. winter precipitation and reservoir levels

ENSO Forecast Forecast Made Sept 2003 Skill: Forecasts for August Skill: Forecasts from April Operational forecasts of ENSO from the Univ. of Washington

Summer Precipitation 2003

North American Monsoon Experiment

Detail of WP and Mexico Temperature

4. Conclusions and Puzzles Problems: If the variability and trend in wheat yield are due to the natural variability in the PNA and WP (and the trend in WP), …. How do drier conditions (r=.7) lead to lower minimum daily temperatures? Does clearing lead to a greater diurnal temperature range, and hence a lower minimum daily temperature, even though the daily mean temperature might be rising?