trend analysis of minimum, maximum, and mean daily temperature extremes in several climatic regions of iran

نویسندگان

وحید ورشاویان

دانش آموختة کارشناسی ارشد هواشناسی کشاورزی، گروه مهندسی آبیاری و آبادانی، دانشکدة مهندسی و فناوری کشاورزی، دانشگاه تهران، ایران علی خلیلی

استاد، گروه مهندسی آبیاری و آبادانی، دانشکدة مهندسی و فناوری کشاورزی، دانشگاه تهران، ایران نوذر قهرمان

استادیار، گروه مهندسی آبیاری و آبادانی، دانشکدة مهندسی و فناوری کشاورزی، دانشگاه تهران، ایران سهراب حجام

دانشیار، گروه هواشناسی، دانشگاه آزاد اسلامی واحد علوم و تحقیقات، تهران، ایران

چکیده

an increase, even moderate, in global temperature is expected to result in a change in frequency of extreme weather events like drought, heavy rainfall and storms. the study of extreme events is difficult due to the fact that it is difficult to find long-term homogeneous data series. also the delimitation of extreme events is not univocal since a parameter value that would be defined as an extreme event in one place, might still be considered a normal event in another. in this study, maximum, minimum and mean daily air temperature (tmax, tmin, and tmean) data over a 44 years period (1961-2004) of four synoptic stations of iran namely; kerman, kermanshah, mashhad, and shiraz were collected. these stations represent different climates of iran based on koppen climatic classification. required data were obtained from the islamic republic of iran meteorological organization (irimo). data were used to calculate extreme temperature values including the magnitudes of the lower (1st, 5th, 10th) and upper (90th, 95th, 99th) percentile threshold values for each year and number of days below the lower threshold values and above the upper threshold values. all time series were checked for normality with the kolmogorov-smirnov test. time trends for all variables were analyzed using parametric and nonparametric techniques (least squares linear regression, pearson, spearman and kendall's ?-significance test). kerman (desert climate) showed significant positive trend in all minimum temperature percentile threshold values except the 95th percentile and a number of upper percentiles (90th and 95th). in maximum temperature, except 1st percentile and the number of days above 90th percentile, other percentiles and the number of days were significant. results for mean temperature trend were similar to minimum temperature. mashhad (temperate humid climate) showed a significant positive trend in all minimum temperature percentile threshold values and the number of days below the 10th, upper 90th and 99th percentile threshold values. maximum temperature showed a significant positive trend just in upper thresholds and all number of days except the number of days below the 1st and upper 95th percentile threshold values. in mean temperature, results were also similar to the minimum temperature.

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عنوان ژورنال:
فیزیک زمین و فضا

جلد ۳۷، شماره ۱، صفحات ۰-۰

کلمات کلیدی
an increase even moderate in global temperature is expected to result in a change in frequency of extreme weather events like drought heavy rainfall and storms. the study of extreme events is difficult due to the fact that it is difficult to find long term homogeneous data series. also the delimitation of extreme events is not univocal since a parameter value that would be defined as an extreme event in one place might still be considered a normal event in another. in this study maximum minimum and mean daily air temperature (tmax tmin and tmean) data over a 44 years period (1961 2004) of four synoptic stations of iran namely; kerman kermanshah mashhad and shiraz were collected. these stations represent different climates of iran based on koppen climatic classification. required data were obtained from the islamic republic of iran meteorological organization (irimo). data were used to calculate extreme temperature values including the magnitudes of the lower (1st 5th 10th) and upper (90th 95th 99th) percentile threshold values for each year and number of days below the lower threshold values and above the upper threshold values. all time series were checked for normality with the kolmogorov smirnov test. time trends for all variables were analyzed using parametric and nonparametric techniques (least squares linear regression pearson spearman and kendall's ? significance test). kerman (desert climate) showed significant positive trend in all minimum temperature percentile threshold values except the 95th percentile and a number of upper percentiles (90th and 95th). in maximum temperature except 1st percentile and the number of days above 90th percentile other percentiles and the number of days were significant. results for mean temperature trend were similar to minimum temperature. mashhad (temperate humid climate) showed a significant positive trend in all minimum temperature percentile threshold values and the number of days below the 10th upper 90th and 99th percentile threshold values. maximum temperature showed a significant positive trend just in upper thresholds and all number of days except the number of days below the 1st and upper 95th percentile threshold values. in mean temperature results were also similar to the minimum temperature.

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