Classic trend analysis methods' paradoxical results and innovative trend analysis methodology with percentile ranges

被引:20
作者
Birpinar, Mehmet Emin [1 ]
Kiziloz, Burak [2 ]
Sisman, Eyup [3 ]
机构
[1] Minist Environm & Urbanizat, TR-06510 Cankaya, Ankara, Turkiye
[2] Kocaeli Metropolitan Municipal Water & Sewerage A, Izmit, Kocaeli, Turkiye
[3] Yildiz Tech Univ, Dept Civil Engn, Hydraul Div, TR-34220 Istanbul, Turkiye
关键词
TIME-SERIES; RAINFALL; TEMPERATURE; PRECIPITATION; IDENTIFICATION; VARIABILITY; BASIN; RIVER; ASSAM; HALF;
D O I
10.1007/s00704-023-04449-6
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this study, spatial-temporal monotonic and non-monotonic trends in Assam, India, have been analyzed for annual precipitation data through the classical and innovative trend analysis (ITA) methodology. The results of the ITA method have been presented with percentile (quartile) intervals. Thus, within the scope of this study, piecewise trends (low; 25% < , medium; 25-75%, and high; 75% > categories) have been objectively analyzed and identified. The annual precipitation data that was measured in twenty stations in the Assam region from 1901 to 2002 is used for the analysis. According to the classical Modified Mann-Kendall (MMK) method results, only in one station of twenty stations, there is an increasing trend contrary to the decreasing trends in five stations; on the other hand, there is no trend in fourteen stations. As regards to the classical Sen's slope (SS) method calculation, a method which is frequently used together with the MMK method to calculate trend slopes, there are paradoxical results between the MMK and SS method. For instance, at the Cachar station, while there is not any significant trend according to the MMK methodology, the result of the SS methodology points out the largest decreasing trend magnitude. Also, the MMK and SS results are incompatible for the Hailakandi, Karimganj, Dhemaji, Nagaon, Barpeta, Golaghat, Kokrajhar, and Lakhimpur stations. On the other hand, there is little incompatibility between the results of the ITA and SS methods. Also, comprehensive information regarding piecewise trends has been obtained through the ITA model graphs with a quartile range.
引用
收藏
页码:1 / 18
页数:18
相关论文
共 54 条
[1]   Comparison of sub-series with different lengths using sen-innovative trend analysis [J].
Alashan, Sadik .
ACTA GEOPHYSICA, 2023, 71 (01) :373-383
[2]   An improved version of innovative trend analyses [J].
Alashan, Sadik .
ARABIAN JOURNAL OF GEOSCIENCES, 2018, 11 (03)
[3]   Temporal Analysis for Detection of Anomalies in Precipitation Patterns over a Selected Area in the Indus Basin of Pakistan [J].
Ali, Akhtar ;
Farid, Hafiz Umar ;
Khan, Zahid Mehmood ;
Ahmad, Ijaz ;
Anjum, Muhammad Naveed ;
Mubeen, Muhammad ;
Shakoor, Aamir .
PURE AND APPLIED GEOPHYSICS, 2021, 178 (02) :651-669
[4]  
[Arias P. IPCC IPCC], 2023, Synthesis report of the IPCC sixth assessment report (AR6)
[5]   Variability and time series trend analysis of rainfall and temperature in northcentral Ethiopia: A case study in Woleka sub-basin [J].
Asfaw, Amogne ;
Simane, Belay ;
Hassen, Ali ;
Bantider, Amare .
WEATHER AND CLIMATE EXTREMES, 2018, 19 :29-41
[6]   Trend detection of annual and seasonal rainfall in Calabria (Southern Italy) [J].
Caloiero, Tommaso ;
Coscarelli, Roberto ;
Ferrari, Ennio ;
Mancini, Marco .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2011, 31 (01) :44-56
[7]   Monotonic trends in spatio-temporal distribution and concentration of monsoon precipitation (1901-2002), West Bengal, India [J].
Chatterjee, Soumendu ;
Khan, Ansar ;
Akbari, Hashem ;
Wang, Yupeng .
ATMOSPHERIC RESEARCH, 2016, 182 :54-75
[8]   Understanding South Australian rainfall trends and step changes [J].
Chowdhury, Rezaul K. ;
Beecham, Simon ;
Boland, John ;
Piantadosi, Julia .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2015, 35 (03) :348-360
[9]   Climate change impacts on sea surface temperature (SST) trend around Turkey seashores [J].
Dabanli, Ismail ;
Sisman, Eyup ;
Guclu, Yavuz Selim ;
Birpinar, Mehmet Emin ;
Sen, Zekai .
ACTA GEOPHYSICA, 2021, 69 (01) :295-305
[10]  
Dabanli I, 2018, INT J GLOBAL WARM, V15, P19, DOI [10.1504/ijgw.2018.091951, 10.1504/ijgw.2018.10006669]