Abstract

This study examines the relationship of climate extremes indices with the large-scale factors like Sea Level Pressure (SLP) and Sea Surface Temperature (SST). The prediction of extreme indices is carried out and is based on statistical downscaling using the extreme indices data, National Centers for Environmental Prediction (NCEP) monthly SLP and SST reanalysis data. For this purpose, five extreme indices (PRCPTOT, R95p, RX5day, TN90p and TX90p) are developed by using homogenized and high quality daily data of temperature and precipitation for the period 1961-2010 of 10 meteorological stations of monsoon-dominated region of Pakistan. These indices are then average to develop an average time series of each extreme index. To check the assumption of regression model, extreme indices data are tested for heteroscedasticity, auto-correlation and normality. All extreme indices are independent, normal and homogeneous. These indices data are then used as predictand and SLP & SST datasets are used as predictors in regression model. Data for period 1961-2000 and 2001-2010 is used for training and validation purpose respectively. Stepwise regression procedure is adopted to compute regression coefficients based on algorithm of Jennrich. Predictors having strong correlation with extreme indices are identified and a regression model is developed using these predictors and also apply cross-validation technique. Performance of regression model and cross validation models is tested by using statistical measures (Root Mean Square Error (RMSE), Mean Absolute Error (MAE) and bias). The performance is seen reasonably high both in training and validation period. The actual and estimated values show a close agreement. It is seen that ensemble mean prediction obtain from crossvalidation models well estimated the extreme indices than the regression model. This study is useful because extremes have a large impact on human society & economy and causing huge losses of the country. The timely prediction of extremes is a major factor and will help the policy makers to take necessary measures for reducing the huge losses.

Highlights

  • Some natural climate variations can significantly alter the behavior of extreme events (Intergovernmental Panel on Climate Change (IPCC)), Third Assessment Report [1]

  • We developed the climate extreme indices using the daily station data and these climate extreme indices data and National Centers for Environmental Prediction (NCEP) monthly mean sea level pressure (MSLP) and monthly sea surface temperature (SST) reanalysis data sets prepared for different months/combination of months are used to develop correlation graph to identify the initial predictors for regression models and to predict extreme indices

  • As it is seen from the results, Root Mean Square Error (RMSE) and ABSE both are less than standard deviation of the observed data of each climate extreme index, which shows that there is a close agreement between estimated and observed extreme indices

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Summary

Introduction

Some natural climate variations can significantly alter the behavior of extreme events (Intergovernmental Panel on Climate Change (IPCC)), Third Assessment Report [1]. Any change in the frequency or severity of extreme climate events could have profound impacts on nature and society. A record 620 mm of rain fell in Islamabad, Pakistan during 10 h in July 2001 bringing urban storm flooding and causing catastrophic losses to life and property [7] Such events have led to many studies of observed changes in temperature and precipitation extremes. According to IPCC TAR [1] some natural climate variations such as ENSO (El-Nino Southern Oscillation), PDO (Pacific Decadal Oscillation), IOD (Indian Ocean Dipole) and NAO (Northern Atlantic Oscillation)/NAM (Northern Hemisphere Annular Mode), can significantly alter the behavior of extreme events, including floods, droughts, hurricanes and cold waves. Predictors having strong correlation with extreme indices are identified and a regression model is developed using these predictors

Monthly maximum precipitation consecutive
Station Data
Variables used
Development of Climate Extremes Indices
Preparation of Gridded data
Gridded Data
Identification and Selection of Predictors for Regression Models
Predictors Longitudes
Validation of Regression Models
Summary and Conclusion
Full Text
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