Alex Jovich- Atmospheric Sciences The Perfect Ocean for Drought On the Cause of the 1930s Dust Bowl Martin Hoerling Science Vol 299 31 Jan. 2003 Siegfried.

Slides:



Advertisements
Similar presentations
VEGETATION FEEDBACK AND DROUGHTS Russell Bird – 3 rd Year Atmospheric Science.
Advertisements

El Nino El Nino is hot air over hot water, which causes warm winds El Nino means boy in Spanish and it causes wet period in Midwestern US.
Climate drivers. Major climate drivers INDIAN OCEAN sea surface temperatures PACIFIC OCEAN sea surface temperatures SOUTHERN ANNULAR MODE – north-south.
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.
Assessment of CFSv2 hindcast (seasonal mean) CPC/NCEP/NOAA Jan 2011.
Starter Consider the climate  Climate is the long-term, widespread weather. There are 3 true statements about climate in the list below. Place an X next.
E l Nino-Southern Oscillation ENSO Richard H. Grumm and Paul Knight V_ February March 2002.
El Nino, La Nina, and their Affects in Oklahoma. El Nino Conditions Warming of central and eastern equatorial Pacific waters Trade wind differences –
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
The Role of Internally Generated Megadroughts and External Solar Forcing in Long Term Pacific Climate Fluctuations Gerald A. Meehl NCAR.
Excerpts of the AAAS Fiscal Year 2009 Appropriations Summary ( September 2008 summary: Congress has made little progress on the federal.
Chapter 25.1 “Factors that Affect Climate”
Ocean Currents. Huge Rivers in the Ocean Ocean currents are huge rivers flowing within the ocean. Each current has its own temperature and its own saltiness.
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.
Surface Currents (ocean) Affect water to a depth of several hundred meters Driven by winds Move in circular patterns in 5 major oceans. Because of Coriolis.
Chapter 7 Ocean Circulation: El Niño
Lesson 11: El Niño Southern Oscillation (ENSO) Physical Oceanography
What Are the El Nino and La Nina?
More Climatic Interactions
What is El Nino and will it end our drought?. What has caused the drought? We have been experiencing drought conditions since September, We've also.
Prentice Hall EARTH SCIENCE
CLIMATE.
Potential Predictability of Drought and Pluvial Conditions over the Central United States on Interannual to Decadal Time Scales Siegfried Schubert, Max.
Climate. Factors that Affect Climate Climate □Average weather conditions over a long period of time □Defined by Many Factors □Temperature □Precipitation.
Climate.
University of Nebraska  Lincoln R School of Natural Resources Atlantic SST influences on North American Drought: A case study on the Medieval Warm period.
Climate & Climate Change Objectives: 1. What factors affect climate? 2. What is El Nino & how does it work? 3. What causes ice ages? 4. How can scientists.
Ch : Climate & Climate Change Objectives: 1
CLIMATE. Weather vs Climate Weather: what is happening in the atmosphere at a particular place and time –Ex: Daily weather forecast for Minneapolis 24ºF,
Dynamic Climate An overview of Climate Oscillations.
The La Niña Influence on Central Alabama Rainfall Patterns.
Me: Jared Persinger Atmospheric Science. Large Scale Drought : Persistent La Nina ( Cool tropical troposphere, pole-ward shifted jet.
Ocean Circulation: El Niño
On the Causes of the 1930s Dust Bowl Siegfried Schubert, Max Suarez, Philip Pegion, Randal Koster and Julio Bacmeister Global Modeling and Assimilation.
Chapter 3 Physical Geography: Climate and Vegetation
The Climate Chapter 25.
Climates.
El Nino Teleconnections Philip Kreycik EPS 131 4/30/04.
July 25, 2001 presents “Past, Present, and Future” Ed Kieser.
Two characteristics of Climate that are most important: 1) The average temperature over the year 2) The annual temperature range (difference between the.
Abnormal Weather October 22, Teleconnections Teleconnections: relationship between weather or climate patterns at two widely separated locations.
C20C Workshop, ICTP Trieste 2004 The impact of stratospheric ozone depletion and CO 2 on tropical cyclone behaviour in the Australian region Syktus J.
The European Heat Wave of 2003: A Modeling Study Using the NSIPP-1 AGCM. Global Modeling and Assimilation Office, NASA/GSFC Philip Pegion (1), Siegfried.
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,
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
Winds Wind is the horizontal movement of air. Air always moves from H  L pressure. Temperature differences create pressure differences. Weather is based.
End of Year – Science Study Guide Earth Systems and Structures.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Understanding and predicting the contrast.
Effects of trends in anthropogenic aerosols on drought risk in the Central United States Dan H. Cusworth Eric M. Leibensperger, Loretta J. Mickley Corn.
Indo-Pacific Sea Surface Temperature Influences on Failed Consecutive Rainy Seasons over Eastern Africa** Andy Hoell 1 and Chris Funk 1,2 Contact:
Hydro-Climate Course March 2004, CU, Boulder Asian Monsoon… K. Krishna Kumar CIRES Visiting Fellow
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
Climate Section 1 Section 1: Factors That Affect Climate Preview Key Ideas Temperature and Precipitation Latitude Heat Absorption and Release Topography.
 El Nino is an abnormal warming of surface ocean waters in the Pacific Ocean  This occurs every 3-5 years  Part of what's called the Southern Oscillation.
The ENSO Cycle Naturally occurring phenomenon – El Nino / Southern Oscillation (ENSO) Cycle Equatorial Pacific fluctuates between warmer-than-average.
Climate Phenomena.
Teleconnection Systems NAO AO PNA
El Niño and La Niña.
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
CLIMATE.
Bellwork 4/13 Describe the weather associated with cyclones and anticyclones. What are the winds called between the Equatorial Low and the Subtropical.
Air Mass: A huge body of air that has similar temperature, humidity, and air pressure at any given height. Classified by 2 characteristics: Temperature.
Interactions between the Responses of
El Niño-Southern Oscillation
Global Climate Change.
El Niño and La Niña.
Combined Effect without Soil Moisture Feedback
Presentation transcript:

Alex Jovich- Atmospheric Sciences The Perfect Ocean for Drought On the Cause of the 1930s Dust Bowl Martin Hoerling Science Vol Jan Siegfried D. Schubert et al. Science Vol Mar. 2004

Intro El Nino / La Nina Dust bowl- 1930s Drought

El Nino Warmer than average SST in Eastern Pacific Higher air pressure in western Pacific Associated with wet winters in SW U.S., drought in Indonesia, Australia Every 3-7 years

La Nina Cooler than average by SST in Eastern Pacific Typically more precip. than average in the Midwest, mild wet summers Typically effects are opposite from El Nino Often preceded by an El Nino

Dust Bowl Drought in the 1930s caused major dust storms In many places nearly ¾ of usable topsoil was blown away 2.5 million people migrated from the plains states

Drought- Some dry material U.S., Mediterranean, Southern Europe, Southwest and Central Asia As little as 50% of the climatological annual average precip. fell during this 4 year period

WHY? WHYYY? Why was the ocean perfect for causing droughts? What Caused the 1930s dust bowl? Did these regional droughts share a common influence? Were slow external forcings responsible for prolonged drought conditions simultaneously over the mid latitudes?

The Perfect Ocean for Drought Data- observed global surface temperature,C, anomalies which were then averaged ( climatology) Global precipitation anomalies mm/yr ( climatology)

June1998-May2002 vs 4 year averaged SST variability ( ) Red is warmer than average Blue is cooler than average Lower chart uses a climatology Exceeds -3 std deviations in Eastern Pacific Exceeds 4 std deviations over the warm pool

Meanwhile at Hall of Justice… Used Atmospheric general circulation models (GCMs) to see if the ocean had anything to do with this Comparing the observed to the ensemble mean, there is a strong implication that the drying was oceanic controlled

Mo’ Models No Problems 4 year average 200 mb height anomalies 3 more experiments, one using both warm and cool, one using just the warm, the other using just the cool

Results The cool Pacific acted synergistically with the warm tropical Indian ocean to definitively claim the ocean was “perfect” for causing drought Suggests an increased risk for severe and synchronized drying of the mid latitudes

Wake up, wake up it’s the first of the month On the Cause of the 1930s Dust bowl Data-precipitation anomalies, sst anomalies Models-used same GCMs as Hoerling, but at a coarser resolution. Used year ( ) runs forced by observed SST

Goin’ for a long run Between the models there is considerable variability Correlation between the mean and observed anomalies is.57 There are periods where all of the curves tend to follow one another (ex 1930s) Main discrepancy is over Mexico, fails to capture full extent of drought, but this is just from ensemble averaging

More stuff SST anomalies (extrapolations) Chopped the earth into 3 regions (Extratropics, Indian ocean, Atlantic/Pacific) Carried out 7 more experiments

Results From the global run, it appears that basic drought conditions are a result from Between tropical and extratropical effects, main features reproduced by tropical run, broadened by extratropical effects

Results Without the feedback from the atmosphere and land surface, there is a 50% reduction in the deficit Great Plains are sensitive to soil moisture feedback

More Results Found that most of the deficits occurred in warm seasons

Conclusion Overall, a cool pacific and a warmer indian working with one another have the potential to cause massive world wide droughts The models don’t always tell the truth (1970s) Land-Atmosphere interaction is important in how severe the drought will be

My 2 cents I agree with the findings in the papers, however I don’t like how they use different time averages and compare them to one another. In the future I would use a better resolution with more runs