 CLIMATE MODEL PRECIPITATION TREND ANALYSIS IN THE 20 TH CENTURY Karen Rivas Key Acknowledgements: Xubin Zeng & Koichi Sakaguchi UA/NASA Space Grant Symposium.

Slides:



Advertisements
Similar presentations
Michael B. McElroy ACS August 23rd, 2010.
Advertisements

1 Trend and Year-to-year Variability of Land-Surface Air Temperature and Land-only Precipitation Simulated by the JMA AGCM By Shoji KUSUNOKI, Keiichi MATSUMARU,
A Look At The Research Perspective Assessed in IPCC Third Assessment Report (TAR) Climate Change 2001: The Scientific Basis (Working Group 1; Sir John.
Climate Change & Global Warming: State of the Science overview December 2009 Nathan Magee.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 8) Climate Models Primary Source: IPCC WG-I Chapter 8 - Climate Models.
1 MET 112 Global Climate Change Dr. Craig Clements San José State University MET 112 Global Climate Change - Lecture 1.
Scaling Laws, Scale Invariance, and Climate Prediction
Climate Change Impacts on the Water Cycle Emmanouil Anagnostou Department of Civil & Environmental Engineering Environmental Engineering Program UCONN.
Dynamical Downscaling of CCSM Using WRF Yang Gao 1, Joshua S. Fu 1, Yun-Fat Lam 1, John Drake 1, Kate Evans 2 1 University of Tennessee, USA 2 Oak Ridge.
Climate Change and Malaysia
Outline Further Reading: Detailed Notes Posted on Class Web Sites Natural Environments: The Atmosphere GE 101 – Spring 2007 Boston University Myneni L29:
WFM 6311: Climate Risk Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6311: Climate Change Risk Management Akm Saiful Islam Lecture-1: Module-1.
Determining the Local Implications of Global Warming Clifford Mass University of Washington.
Liu, J. et al., PNAS, 2012 World Weather Open Science Conference, Montreal, Canada, August 17, 2014 Jiping Liu University at Albany, State University of.
Evaluation of IPCC Soil Moisture Simulations for the latter half of the 20 th Century Haibin Li 1, Alan Robock 1, Martin Wild 2 1 Department of Environmental.
Essential Principles Challenge
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
Impacts of Climate Change on Corn and Soybean Yields in China Jintao Xu With Xiaoguang Chen and Shuai Chen June 2014.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Observed Surface & Atmosphere (from IPCC WG-I, Chapter 3) Observed Changes in Surface and Atmosphere Climate.
Climate Change Impacts & Resource Management Stephen T. Gray Water Resources Data System WY State Climate Office University of Wyoming.
Barcelona, 2015 Ocean prediction activites at BSC-IC3 Virginie Guemas and the Climate Forecasting Unit 9 February 2015.
What is a Climate Model?.
Global warming and Sea Level Rise: Best estimates by 2100 John King
Impact of Wind and Ice Biases on the Southern Ocean Carbon and Heat Uptake Jessica Rudd Joellen Russell, Ph.D. & Paul Goodman, Ph.D. Department of Geosciences,
Anthropogenic Climate Change. Global Temperature is Increasing.
Relationship between global mean sea-level, global mean temperature and heat-flux in a climate simulation of the past millennium Hans von Storch, Eduardo.
NOTE to the Teacher  In an inquiry classroom, teachers facilitate the construction of new knowledge by activating and then pursuing the inquisitive nature.
CLIMATE CHANGES DURING THE PAST MILLENNIUM Michael E. Mann Department of Environmental Sciences University of Virginia Gavin A. Schmidt and Drew T. Shindell.
Climate change projections for Vietnam from CMIP5 simulations Ramasamy Suppiah 29 November 2012.
Future Climate Projections. Lewis Richardson ( ) In the 1920s, he proposed solving the weather prediction equations using numerical methods. Worked.
Global Energy Balance and the Greenhouse Effect What determines Earth’s surface temperature? What is the history of CO 2 on Earth? ultravioletinfrared.
Variation of Surface Soil Moisture and its Implications Under Changing Climate Conditions 1.
Climate Modeling Idania Rodriguez EEES PhD Student Idania Rodriguez EEES PhD Student “Science Explorations Through the Lens of Global Climate Change” Workshop.
Environment Canada Environnement Canada Effects of elevated CO 2 on modelled ENSO variability Bill Merryfield Canadian Centre for Climate Modelling and.
Opportunities for Research in the Dynamics of Water Processes in the Environment at NSF Pam Stephens Directorate of Geosciences, NSF Directorate of Geosciences,
Global and SE U.S. Assessment of Precipitation: Comparison of Model Simulations with Reanalysis-based Observations Eduardo Ponce Mojica Polytechnic University.
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
Investigation of Atmospheric Recycling Rate from Observation and Model James Trammell 1, Xun Jiang 1, Liming Li 2, Maochang Liang 3, Jing Zhou 4, and Yuk.
TOPIC III THE GREENHOUSE EFFECT. SOLAR IRRADIANCE SPECTRA 1  m = 1000 nm = m Note: 1 W = 1 J s -1.
Instrumental Surface Temperature Record Current Weather Data Sources Land vs. Ocean Patterns Instrument Siting Concerns Return Exam II For Next Class:
An Overview of the Observations of Sea Level Change R. Steven Nerem University of Colorado Department of Aerospace Engineering Sciences Colorado Center.
The lower boundary condition of the atmosphere, such as SST, soil moisture and snow cover often have a longer memory than weather itself. Land surface.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
1. Analysis and Reanalysis Products Adrian M Tompkins, ICTP picture from Nasa.
Past and Projected Changes in Continental-Scale Agro-Climate Indices Adam Terando NC Cooperative Research Unit North Carolina State University 2009 NPN.
Climate Modeling Research & Applications in Wales John Houghton C 3 W conference, Aberystwyth 26 April 2011.
Exploring the Possibility to Forecast Annual Mean Temperature with IPCC and AMIP Runs Peitao Peng Arun Kumar CPC/NCEP/NWS/NOAA Acknowledgements: Bhaskar.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 12 Future Predictions Eugene Cordero San Jose State University Outline  Scenarios.
Of what use is a statistician in climate modeling? Peter Guttorp University of Washington Norwegian Computing Center
Seasonal Anomalies in the Sea Ice Concentration in the Ross Sea and Their Correlation to the Southern Annular Mode Kiley Yeakel 1, Joellen Russell 2, Paul.
VERIFICATION OF A DOWNSCALING SEQUENCE APPLIED TO MEDIUM RANGE METEOROLOGICAL PREDICTIONS FOR GLOBAL FLOOD PREDICTION Nathalie Voisin, Andy W. Wood and.
EVALUATION OF A GLOBAL PREDICTION SYSTEM: THE MISSISSIPPI RIVER BASIN AS A TEST CASE Nathalie Voisin, Andy W. Wood and Dennis P. Lettenmaier Civil and.
“CLIMATE IS WHAT WE EXPECT, AND WEATHER IS WHAT WE GET” ~ MARK TWAIN.
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 Extreme Climatic and atmospheric.
WFM 6311: Climate Risk Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6311: Climate Change Risk Management Professor A.K.M. Saiful Islam Lecture-1:
Mingyue Chen, Wanqiu Wang, and Arun Kumar
1. Analysis and Reanalysis Products
Instrumental Surface Temperature Record
What is a Climate Model?.
Using Remote Sensing to Monitor Plant Phenology Response to Rain Events in the Santa Catalina Mountains Katheryn Landau Arizona Remote Sensing Center Mentors:
Instrumental Surface Temperature Record
Analysis of NASA GPM Early 30-minute Run in Comparison to Walnut Gulch Experimental Watershed Rain Data Adolfo Herrera April Arizona Space Grant.
Modeling the Atmos.-Ocean System
What is a Climate Model?.
Global Monsoon Onset and Retreat based on Precipitable Water and Wind
Amplified Eurasian springtime warming from snow darkening
Globale Mitteltemperatur
Predictive Modeling of Temperature and Precipitation Over Arizona
The Nuts and Bolts of Climate Change
Globale Mitteltemperatur
Presentation transcript:

 CLIMATE MODEL PRECIPITATION TREND ANALYSIS IN THE 20 TH CENTURY Karen Rivas Key Acknowledgements: Xubin Zeng & Koichi Sakaguchi UA/NASA Space Grant Symposium April 21,

Questions  Based on climate models how will global mean precipitation change?  How reliable are climate models in comparison with observational data in the past ~100 years? 2

Approach and Methods  Analyze various climate model precipitation trends  Analyze observational precipitation trends from two distinct set of data  Draw conclusions from comparison of model precipitation trends and observational trends 3

Climate Models  “Climate models use quantitative methods to simulate the interactions of the atmosphere, oceans, land surface, and ice.”  The use of climate models ranges from studying earth weather dynamics, to making predictions about future climate.  Model accounts for incoming and outgoing energy due to electromagnetic radiation 4

Data Analyzed  Models:  NCAR-CCSM-4 21 st Century Projections (future)  NASA-GISS-E2-R21 st Century Projections (future)  NCAR-CCSM-4 20 th Century Hindcasts (past)  NASA-GISS-E2-R 20 th Century Hindcasts (past) As used in the coming IPCC Report  Observational Data:  Global Land Precipitation,  Climatic Research Unit (CRU) 5

Analysis Techniques Global mean precipitation is used to calculate:  change over ~100 year periods  respective change in 10-year windows 6 Blue: Global mean annual precipitation from GISS E2-R Green: Linear fits for different 10-year periods

Results 7 Average annual precipitation rateChange Observational GISS E2R CCSM Global Average Annual Precipitation (mm/year) and its Change over Historical Period

Results 8 ErrorGISS E2RCCSM4 Correlation (R) R2R Root Mean Square Error (RMSE) (mm/year/decade) Comparison between Models and CRU data for 10 year windows from Historical Period

Future Projections 9 Models20 th century21 st century GISS E2R CCSM Change of annual precipitation rate (mm/year) over the whole 20 th and 21 st centuries Annual precipitation (black) and 10-year linear fits (colors)

Conclusion  Over the entire 20 th century observational global mean precipitation has slightly increased  Over the entire 21 st century both models project an increase in global mean precipitation  For the 10 year timescale, trend is highly variable and the model performance is poor for the 20 th century. 10

Future Studies  Look at smaller spatial scales  Look at longer temporal scale  Look at more models 11

 Thank You Karen Rivas Department of Chemical and Environmental Engineering University of Arizona April 21, 2012 Tucson, Arizona 12