Research Inst. for Humanity and Nature (also at IIS, University.

Slides:



Advertisements
Similar presentations
Data requirement for empirical climate prediction models By Omar Baddour.
Advertisements

OBJECTIVES Evaporation, precipitation and atmospheric heating ‘communicate’ SSTA to the atmosphere, driving changes in temperature, precipitation and.
Briefing to Premier & Cabinet 18 October Very Wet during 2010.
THE USE OF REMOTE SENSING DATA/INFORMATION AS PROXY OF WEATHER AND CLIMATE IN THE GREATER HORN OF AFRICA Gilbert O Ouma IGAD Climate Applications and Prediction.
APPLICATION OF CLIMATE PREDICTION IN RICE PRODUCTION IN THE MEKONG RIVER DELTA (VIETNAM) Nguyen Thi Hien Thuan Sub-Institute of Hydrometeorology and Environment.
Hydrological Modeling for Upper Chao Phraya Basin Using HEC-HMS UNDP/ADAPT Asia-Pacific First Regional Training Workshop Assessing Costs and Benefits of.
Seasonal Climate Forecast (Forecast Method) (Revised: May 26, 2012) This product is published by the Oregon Department of Agriculture (ODA), in cooperation.
The Potential for Skill across the range of the Seamless-Weather Climate Prediction Problem Brian Hoskins Grantham Institute for Climate Change, Imperial.
Indo-UK Programme on Climate Change Impacts in India : Delhi Workshop, Sep. 5-6, 2002 Impacts of Climate Change on Water Resources INDIAN INSTITUTE OF.
1 G EOSS A nd M AHASRI E xperiment in T ropics (GaME-T) Taikan Oki and Shinjiro.
Climate Variability and Prediction in the Little Colorado River Basin Matt Switanek 1 1 Department of Hydrology and Water Resources University of Arizona.
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.
India’s Water Crisis El Niño, Monsoon, and Indian Ocean Oscillation.
BASICS OF EL NIÑO- SOUTHERN OSCILLATION (ENSO) Ernesto R. Verceles PAGASA.
SIO 210: ENSO conclusion Dec. 2, 2004 Interannual variability (end of this lecture + next) –Tropical Pacific: El Nino/Southern Oscillation –Southern Ocean.
For the lack of ground data the verification of the TRMM performance could not be checked for the entire catchments, however it has been tested over Bangladesh.
Colorado River Basin Long Lead Forecasting Research Tom Piechota (UNLV) Kenneth Lamb (UNLV) Glenn Tootle (University of Tennessee) Tyrel Soukup (University.
Water availability assessment in data scarce catchments: Case Study of Northern Thailand Supattra Visessri 1st Year PhD Student, Environmental and Water.
Dr Mark Cresswell Dynamical Forecasting 2 69EG6517 – Impacts & Models of Climate Change.
Groundwater Modeling Study case : Central Plain of Thailand
ABSTRACTS General Structure Background and Objective Downscaling CGCM climate change output scenario using the Artificial Neural Network model Kang Boosik.
Baseline Climatology of Viti Levu (Fiji) and Current Climatic Trends Melchior Mataki AIACC-SIS09 Pacific Centre for Environment and Sustainable Development.
(Swiss Re, 2012) Emma Gale & Mark Saunders Department of Space & Climate Physics, University College London, UK The 2011 Thailand flood: climate causes.
GHP and Extremes. GHP SCIENCE ISSUES 1995 How do water and energy processes operate over different land areas? Sub-Issues include: What is the relative.
NERC Centre for Global Atmospheric Modelling Department of Meteorology, University of Reading The role of the land surface in the climate and variability.
Assessing Predictability of Seasonal Precipitation for May-June-July in Kazakhstan Tony Barnston, IRI, New York, US.
The La Niña Influence on Central Alabama Rainfall Patterns.
PAGASA-DOST Presscon - 04 October 2010 Amihan Conference Room.
Drought Management in Thailand Wet Season, 2014 Dry Season, 2014/15 Wet Season, 2015 Chao Phraya River Basin Lerdphan Sukyirun Irrigation Engineer Professional.
Water Resources Management in the Philippines during El Niño Episodes
Contacts: Werapol Bejranonda and Manfred Koch
1 G EOSS A nd M AHASRI E xperiment in T ropics (GaME-T) Taikan Oki and Shinjiro.
Introduction 1. Climate – Variations in temperature and precipitation are now predictable with a reasonable accuracy with lead times of up to a year (
Relationship between interannual variations in the Length of Day (LOD) and ENSO C. Endler, P. Névir, G.C. Leckebusch, U. Ulbrich and E. Lehmann Contact:
Indo-UK Programme on Climate Change Impacts in India : Delhi Workshop, Sep. 5-6, 2002 Impacts of Climate Change on Water Resources G.B. Pant INDIAN INSTITUTE.
Dr Mark Cresswell Statistical Forecasting [Part 2] 69EG6517 – Impacts & Models of Climate Change.
Climate Information for Hydrological Outlooks David Wratt, Roddy Henderson, Charles Pearson & James Renwick NIWA, New Zealand Technical Conference on Changing.
Statistical Summary ATM 305 – 12 November Review of Primary Statistics Mean Median Mode x i - scalar quantity N - number of observations Value at.
Chaiwat Ekkawatpanit, Weerayuth Pratoomchai Department of Civil Engineering King Mongkut’s University of Technology Thonburi, Bangkok, Thailand Naota Hanasaki.
Indo-UK Programme on Climate Change Impacts in India : Delhi Workshop, Sep. 5-6, 2002 Objectives Analysis of spatio-temporal variability of precipitation.
Exploring the Possibility of Using Tropical Cyclone Numbers to Project Taiwan Summer Precipitation Patterns Mong-Ming Lu and Ru-Jun May Research and Development.
Using the National Multi-Model Ensemble (NMME) System Johnna Infanti Advisor: Ben Kirtman.
Development of an Ensemble Gridded Hydrometeorological Forcing Dataset over the Contiguous United States Andrew J. Newman 1, Martyn P. Clark 1, Jason Craig.
Downscaling Global Climate Model Forecasts by Using Neural Networks Mark Bailey, Becca Latto, Dr. Nabin Malakar, Dr. Barry Gross, Pedro Placido The City.
Indicators for Climate Change over Mauritius Mr. P Booneeady Pr. SDDV Rughooputh.
Fifth Session of the South Asian Climate Outlook Forum (SASCOF-5) JMA Seasonal Prediction of South Asian Climate for Summer 2014 Hitoshi Sato Climate Prediction.
1/39 Seasonal Prediction of Asian Monsoon: Predictability Issues and Limitations Arun Kumar Climate Prediction Center
Arif Mahmood Chief Meteorologist Pakistan Meteorological Department Monsoon Rainfall Prediction Over Pakistan First session of.
Seasonal Forecast of Antarctic Sea Ice
LONG RANGE FORECAST SW MONSOON
Current State of the Pacific and Indian Oceans
Analysis of Hydro-climatology of Malawi
Dr Patsani G Kumambala (LUANAR)
The Indian Monsoon and Climate Change
Tushar Sinha Assistant Professor
Challenges of Seasonal Forecasting: El Niño, La Niña, and La Nada
LONG RANGE FORECAST SW MONSOON
Course Evaluation Now online You should have gotten an with link.
Course Evaluation Now online You should have gotten an with link.
LONG RANGE FORECAST SW MONSOON
2018 Agricultural Climate Outlook
El Nino-Southern Oscillation
Course Evaluation Now online You should have gotten an with link.
Application of satellite-based rainfall and medium range meteorological forecast in real-time flood forecasting in the Upper Mahanadi River basin Trushnamayee.
Seasonal Predictions for South Asia
ENSO –El Niño Southern Oscillation
Case Studies in Decadal Climate Predictability
Predictive Modeling of Temperature and Precipitation Over Arizona
Kreshna GOPAL C. Prakash KHEDUN Anoop SOHUN
Seasonal Forecasting Using the Climate Predictability Tool
Presentation transcript:

Research Inst. for Humanity and Nature (also at IIS, University of Tokyo) Taikan Oki Water Resources Application Project (WRAP)

Criteria: the most critical problem  Recovery Cost  Duration of problem  Frequency of occurrence  Future perspective (the most critical problem) Drought Data Source: RID, 2001; PAL and Panya,1999. Almost dry up !!! 1. Water Resources and Water Problems in the Study Area 8 Sub River Basin 6 =Ping 7 =Wang 8 =Yom 9 =Nan 10 =Main Chao Phraya 11 =Sakakrang 12 =Pasak 13 =Thachin Made by RID Study Area Water-related Problems  Flooding  Drought  Water Pollution  Excessive Groundwater Extraction Bhumipol Sirikit

Water Situation in Drought Data Source: EGAT (for whole year) Planning Problem Planning Problem Possible Solution: Reliable Long-term Hydroclimatic Prediction

Rainfall (RF) and StreamflowRainfall (RF) and Streamflow Southern Oscillation Index (SOI)Southern Oscillation Index (SOI) Sea Surface Temperature (SST)Sea Surface Temperature (SST) 2.DATA AND METHODOLOGY USED IN HYDROCLIMATIC PREDICTION Sea Surface Temperature (SST) The British Atmospheric Data Centre (BADC), UK -GISST_2.3B Dataset (1 degree x 1 degree) SOI = (Standardized Tahiti - Standardized Darwin) / MSD Bureau of Meteorology (BOM) Australia, AU Thai Meteorological Department (TMD), TH Royal Irrigation Department (RID), TH Global Energy and Water Cycle Experiment (GEWEX), Asian Monsoon Experiment - Tropics (GAME-T) Data Used Data Used (Monthly ) Upper Ping River Basin

Model Used for Long-term Hydroclimatic Prediction PURPOSE TYPE MODEL Physically Based Model Understand the physical mechanisms Climate Model (GCM, AGCM, etc.) Statistically Based Model More Accurate Predicted Result (for real application) Linear Regression Model Generalized Additive Model Artificial Neural Networks, etc. Artificial Neural Network (ANN) Use limited data Computational skill in complex problem No assumption needed as other statistical models Updating parameters process Manusthiparom (2003) By Manusthiparom (2003)

Methodology Used for Hydroclimate Prediction Influence of ENSO On rainfall and streamflow 1.1 El Niño/La Niña composites 1.2 Categorical contingency analysis1 Prediction process 2.1 Prediction by ANN modeling 2 Improvement and extension 3.1 Prediction using additional predictors 3.2 Input Sensitivity Analysis 3.3 Spatial rainfall prediction 3 Potential use of prediction for improved WRM system 4.1 Irrigation Water Demand Forecasting 4 Manusthiparom (2003) By Manusthiparom (2003)

LONG-TERM RAINFALL PREDICTION BY ANN MODELING APPROACH Feed-Forward Direct Multi-step Network Difficulties in Using ANN Modeling Physical considerations, Correlation analysis Determination of Input Nodes 1 SST&RF, SOI& RF, RF& RF Trial and error process Determination of No.of Hidden Layers and Hidden Nodes 2 Hidden layer=1 No. of hidden node=5-10 Adaptive process with changing initial weighting parameters Training Process (Weighting factors) 3 Good pattern=97 % (target error=15%)

Rainfall Anomaly Prediction 12 months ahead Testing Training Case 1 Case 1: Train ( , 18 yrs), Test ( , 20 yrs) Case 2: Train ( , 28 yrs), Test ( , 10 yrs) Case 3: Train ( , 33 yrs), Test ( , 5 yrs) SSTs: 3 areas

Case 3: Train ( , 33 yrs), Test ( , 5 yrs) Target Error=15% Case 2: Train ( , 28 yrs), Test ( , 10 yrs) Large Error Drought Target Error=15% Smaller Error Bad Pattern Rainfall Prediction 12 months ahead SSTs: 3 areas

Spatial Rainfall Prediction Rainfall Anomaly in August Observation Software: Surfer 8 Total: 16 stations Gridding method: Kriging Variogram model: Linear Slope =1.0, Aniso= 1,0 Kriging type: point Drift type: None No search: Use all data (16) Prediction One Month Ahead Manusthiparom (2003) By Manusthiparom (2003)

Date: 2 November 2002 Project: Krasieo Operation and Maintenance Project, Royal Irrigation Department Location: Suphanburi, Thailand Learning the existing system of WRM Period: 4-15 November 2002 Tutor: Mr. Sombat Sontisri (Irrigation Eng.) Chief: Mr. Pongsak Arunwichitsakul Water Allocation Group Office of Hydrology & Water Management Royal Irrigation Department (RID), Thailand Water Manager Irrigation Eng. Learning Existing System of WRM from Water Manager Meeting and Interview Water Users Water Users (Agriculture) Drought is the most serious problemDrought is the most serious problem They want to know how much water will be available for them in next growing seasonThey want to know how much water will be available for them in next growing season Water Manager (RID) They want to know how much water will be available in next seasonThey want to know how much water will be available in next season They want to improve the existing system if it is easy to understand and easy to do in practice) They want to improve the existing system if it is easy to understand and easy to do in practice) 5. POTENTIAL USE OF PREDICTION IN IMPROVING WATER RESOURCES MANAGEMENT SYSTEM

Rainfall Irrigation Water Demand (IWD) Anomaly Value Absolute Value Drought:1993 Forecasted Irrigation Water Demand Using long-term mean: mcm Using observation: mcm Using prediction: mcm Mae Ngat Irrigation Project, Chiang Mai Using predicted rainfall is better Using predicted rainfall is worse 12-month ahead forecasted IWD Manusthiparom (2003) By Manusthiparom (2003)

Water Situation in Drought Forecasted Irrigation Water Demand Using long-term mean: mcm Using observation: mcm Using prediction: mcm IWD Adjustment of Irrigation Area for mcm Based on long-term mean: 30,000 rai (120.61/120.61*30,000) Based on observation:24,081 rai (120.61/150.25*30,000) Based on prediction:24,502 rai (120.61/147.61*30,000) 1 rai =1,600 m 2 1 km 2 = 625 rai Drought: 1993 Potential Use of Forecasted IWD to improve Planning System Water scarcity situation in 1994 should have been improved. 5,953 6,202 4,373 Manusthiparom (2003) By Manusthiparom (2003)

Summary  ANN can predict monthly rainfall a year ahead with fairly good accuracy based on SST, SOI, and preceding rainfall.  Seasonal prediction of rainfall will substantially contribute for better water resources/reservoir operations.  GAME-T Database is there:  New research opportunities under GAME- Tropics/Phase II and WRAP for everybody!

Thank you!