130 likes | 178 Views
BALWOIS 2010 Conference on water observation and information systems for decision support 25-29 May 2010, Ohrid, Republic of Macedonia. Trend Analysis of Hydrometeorological Parameters in Climate Regions of Turkey. Hakan Aksu. General Directorate of State Hydraulic Works , Ankara, Turkey.
E N D
BALWOIS 2010 Conference on water observation and information systems for decision support 25-29 May 2010, Ohrid, Republic of Macedonia Trend Analysis of Hydrometeorological Parameters in Climate Regions of Turkey Hakan Aksu General Directorate of State Hydraulic Works, Ankara, Turkey
Objectives Investigation of trends 1. Long term precipitation data 2. Long term temperature data 3. Long term estimated evapotranspiration values Understanding trends in spatial extent. Understanding trends in temporal extent • Clues for climate change.
Data and Methodology 1. • Long term annual total precipitation • Long term annual average temperature • Between 1950-2005 years • 14 stations all over Turkey • Swed- Eisenhart test was applied for temperature and precipitation data • Only one station (Alanya) showed inhomogenity. For this reason Alanya was not analysed for trend anaysis.
Data and Methodology 2. • Evapotranspiration time series were generated by Turc formula (Turc, 1961) • Kolmogrov-Smirnov normality test was performed for 90% confidence interval. Results are presented in table 1. • The pearson’s correlation r was used in order to detect linear trend in homogenous on normally distributed time series
Data and Methodology 3. • Significance of pearson’s r was checked by the student’s t test (95%) • The other method non parametric Man Kendall test was applied to all homogenious time series.
FINDINGS • If the Kendall test z values bigger than 20, at that time regression trend test gave the same result. • The value of 0,02 value for the slope temperature regression equation can be evaluated as a reference level for upward evapotranspiration trends (Table 5). • Majority of stations shows upward trend on temperature and evapotranspiration. One except all stations shows no trend on precipitation.