downscaling global climate model outputs to fine scales sanjaya ratnayake

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Downscaling Global Climate Model Outputs to Fine Scales over Sri Lanka for Assessing Drought Impacts Sanjaya Ratnayake Foundation for Environment Climate and Technology Sri Lanka

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Even though standard precipitation index (SPI) is not a drought predicting tool using downscaled results it was possible to forecast SPI. Forecasted SPI can use for two purposes. Firstly, in order to implement better drought relief payment policy. Secondly, to better water resource planning in order to reduce agriculture risk. Statistical downscaling procedure was developed over Sri Lanka for drought risk. The system was based on Climate Information tool Kit 2.0 (CLIK) by Asia-Pacific Economic Corporation (APEC) Climate Center (APCC). As the predictor region El Niño Southern Oscillation (ENSO) region was considered because recent droughts are more influenced by ENSO compared to traditional South West monsoons (SWM) and North East monsoon (NEM) for the island. Seasonal drought study was carried out considering 3 months intervals for 4 seasons January to March (JFM), April to June (AMJ), July to September (JAS) and October to November (OND). In order to identify optimal SPI scales, models, variables and NINO regions for each season a preliminary study was carried out using a sample stations and based on the results detailed study was carried out for 34 stations covering central and southern parts of the island. Heidke skill score was considered as the categorical verification measure. In order to improve the magnitude of forecasted SPI 2 variance inflation techniques were employed. In CLIK multi model ensemble (MME) predictions were tested considering 3 deterministic models: simple composition method (SCM), multiple regression method (MRG) and synthetic multi model super ensemble method (SSE). However due to low resolution regression based downscaling was considered. Interestingly central high hills showed a very high correlation with ENSO during OND. For highly skilled stations drought characteristics such as trends, onset, duration, frequency and severity can be calculate. Our results highlight that CLIK is skillful over Sri Lanka. Specially in identifying best downscaling characteristics over a station.

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Page 1: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Downscaling Global Climate Model Outputs to Fine Scales over Sri Lanka for Assessing Drought

Impacts

Sanjaya RatnayakeFoundation for Environment Climate and Technology

Sri Lanka

Page 2: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Overview

• Introduction• Problem Definition• Aims and Objectives• My approach• Data and Study Area• Methodology• Results• My Prediction• Conclusion• Acknowledgement

Page 3: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Introduction

• Due to the geographical distribution the island is affected with different kinds of natural disasters.

• The most frequent natural hazards that affect the island are drought, floods, landslides, cyclones and coastal erosion.

• Among all natural disasters, droughts occur most frequently, have the longest duration, and cover the largest area.

Page 4: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Problem Definition

• So far there is no proper drought index over Sri Lanka.

• So far there is no proper drought characteristics predicting mechanism.

• So far drought relief payments made in districts across the country by the government over a 40 years period used as a proxy for drought risk.

Page 5: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Aims and Objectives

• Asses the APCC CLIK tool skill over Sri Lanka• Observer station correlations with NINO

regions• Identify most appropriate downscale

parameters for individual station for different seasons

• Develop drought index over Sri Lanka• Predict Seasonal Droughts

Page 6: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

My Approach

• Calculate SPI over Sri Lanka• Obtain downscale results using SPI• Observe skill of forecasted downscale SPI

results• Amplitude the results using variance inflation

methods• Predict SPI using most appropriate method.

Page 7: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Data and Study Area

• 132 station monthly precipitation data covering entire island.

• 26 stations with missing and corrupted data.• SPI 30 years (24 years here)• CLIK most models support : 1984 to 2008

• Finally, 34 stations covering southern and central parts of the Island.

Page 8: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

(a)

(b)

(c)

Page 9: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Methodology

• Standard Precipitation Index (SPI)• Climate Information tool Kit 2.0• Preliminary Study• Detailed Downscaling• Variance Inflation• Heidke Skill Score

Page 10: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Meteorological drought index • Standard Precipitation Index requires only

precipitation as input (McKee, et al., 1993)• SPI scale 1, 3, 6 and 12– Appropriate for short term drought studies – Appropriate for seasonal drought studies – 3 months droughts have a drastic impact on the

agriculture – Highly successful with drought data

Page 11: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

SPI ClassificationSPI Drought classification

>2.0 Extreme wet1.5 to 1.99 Very wet1.0 to 1.49 Moderately wet

-0.99 to 0.99 Near Normal-1.0 to -1.49 Moderately Dry-1.5 to -1.99 Severe Dry

<-2.0 Extremely Dry

SPI Drought category

0 to -0.99 Mild drought-1.0 to -1.49 Moderately drought-1.5 to -1.99 Severe drought

<-2.0 Extremely drought

Page 12: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Climate Information tool Kit 2.0 (CLIK)

• By APEC Climate Center (APCC) • Statistical Downscaling• Linear Regression• 16 GCM models• 10 predictor variables• 3 months seasonal predictions• Screening Process– First Screening Process (FSC) : Hopeful stations– Second Screening Process (SCP) : Good stations

Page 13: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Preliminary Study

Predictor• Training Period: 1984-2008

• Variables: SLP, SST, U850

• Models: NCEP, NASA, MSC_CANCM4, HMC, CWB, IRIF, GDAPS_F, COLA, MSC_CANCM3, MGO, POAMA, PNU and BCC

• Region : NINO1+2, NINO3, NONO4, NINO3.4

Page 14: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Preliminary Study

Predictand• Season: JFM, AMJ, JAS, OND

• Variables: Precipitation

• Statistical Downscaling: Linear Regression

• Significant Level: 5%

• Minimum pattern score: 0.3

Page 15: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Detailed Downscaling StudySeason JFM AMJ JAS OND

Predictor Model NCEP NCEP NCEP MGO

Predictor Region NINO3 NINO3 NINO3.4 NINO3

Predictor Variable SLP SLP SST U850

No of Stations 34

Predictand Variable SPI

Training Period 1984-2008

Statistical Downscaling Linear Regression

Significant Level 5%

Mini. Pattern score 0.3

Page 16: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Variance Inflation

• Improver magnitude of downscaled forecasted results

Page 17: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Heidke Skill Score

Observed ForecastYes No

Yes A BNo C D

𝐻𝑆𝑆=2 (𝑎𝑑−𝑏𝑐 )

[ (𝑎+𝑐 ) (𝑐+𝑑 )− (𝑎+𝑏) (𝑏+𝑑 ) ]

• For Mild, Moderate, Severe and Extreme droughts HSS was calculated separately.

• JFM and OND seasons were considered separately.

HSS 1: Perfect forecast HSS 0: No skill HSS < 0: Chance forecast is better

Page 18: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Results

• Preliminary Study Results• Downscale results• HSS Results comparison for– Downscale results– VIF1 Results– VIF2 Results

Page 19: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Preliminary Study Results

Page 20: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Preliminary Study Results

• OND showed the best correlations fallowed by JFM

• NINO3 showed higher correlation• JFM : NCEP model with SLP variable• OND : MGO models with U850 variable• Low results for AMJ and JAS

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Detailed Downscaling resultsSeason JFM AMJ JAS OND

Only FSP 3 - 2 8

SCP 15 1 7 18

Highest Correlation 0.52 0.26 0.59 0.7

Corr > 0.6 - - - 3

Corr > 0.3 9 - 5 13

Page 22: Downscaling global climate model outputs to fine scales   sanjaya ratnayake
Page 23: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

JFM AMJ

JAS OND

-WR - -WR - -WR - -WR WR WR WR

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JFM

AMJ

JAS

OND

Page 25: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Variance Inflation

• Mild drought– Almost Downscale and VIF2 similar results– VIF2 slight improvement in OND

• Moderate drought : Good improvement for VIF2

(specially in OND)• Severe Droughts : Good improvement from VIF1

• Extreme Droughts : Longer period data are required

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Mild Drought

Downscale VIF1 VIF2

JFM

Downscale VIF1 VIF2

OND

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Moderate Drought

Downscale VIF1 VIF2 JFM

Downscale VIF1 VIF2 OND

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My Prediction for 2012 OND

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Conclusion

• Overall CLIK is skillful over Sri Lanka• Variance Inflation methods are important

when drought magnitude increases• OND was high skill season• Central High hills showed higher correlation• NINO3 showed good correlation over all

seasons except AMJ

Page 30: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

How to use my study results

• Even though SPI is not a drought predicting tool using downscaled SPI it was possible to forecast drought in Sri Lanka.

• Predicted drought characteristics for better water resource planning in order to reduce agriculture risk

• Use my drought index to proper drought payment relief payment

Page 31: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Acknowledgement• Funders

– Asia-Pacific Economic Corporation (APEC) Climate Center (APCC)

• Supervisors– Dr. Soo-Jin Sohn, Team Leader(Climate Prediction Team), APCC– Dr. Lareef Zubair, Principal Scientist, Foundation for Environment Climate and Technology, Sri Lanka

• Data Providers– Precipitation data : Ministry of Irrigation and Water Resources Management, Sri Lanka– GCM model data providers

• Individuals– Mr. Wimal Ratnayake (Irri Mini) : Station details– Ms. Hye-Jin Park (APCC) : CLIK– Dr. Prasanna Venkatraman (APCC) : ENSO– Ms. Ruvindee Rupasinghe (Uni Peradeniya) : English and Report corrections – Ms. Sooyang Joo (APCC) : Operation support– Mr. Dede Tarmana (The Indonesian Agency for Meteorology Climatology and Geophysics, Indonesia) : Arc GIS

• Free Software– SPI_tool : The National Drought Mitigation Center– Arc Portable : ESRI– Goole earth : Google Inc– Goole Fusion : : Google Inc– CLIK : APCC – Eviews : HIS Inc.

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Flashback

• Introduction• Problem Definition• Aims and Objectives• My approach• Data and Study Area• Methodology• Results• Forecast• Conclusion• Acknowledgement

Page 33: Downscaling global climate model outputs to fine scales   sanjaya ratnayake

Thank you