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Fuladipanah, et al.

                global warming, urbanization, and land degradation – is   trend analysis, do not require strict distributional
                amplifying shifts in these variables, exacerbating risks   assumptions. Both model classes have been extensively
                such as floods, droughts, and disruptions to hydrological   employed by researchers to conduct trend analyses in
                cycles.  According  to  the  Intergovernmental  Panel   various fields. 16-25  A brief list of trend analysis models is
                on  Climate  Change,  anthropogenic  activities  have   presented in Table 1.
                accelerated these changes, with projections indicating   This study introduces a comprehensive comparative
                a global temperature rise of 1.0 – 5.7°C, a sea-level   analysis of long-term trends in monthly groundwater
                increase of 0.5 – 1.0  m, and an increased frequency   levels across 16 provinces in the Republic of
                of  extreme  weather  events  by  2100.  Trend  analysis,   Karakalpakstan, Uzbekistan, spanning the period from
                particularly  through non-parametric  methods, has   1990 to  2023. By integrating  innovative  statistical
                become indispensable for evaluating temporal patterns   techniques, including the innovative polygon trend
                in hydroclimatic data. These methods bypass restrictive   analysis (IPTA), the MK test, and Sen’s slope estimator,
                assumptions (e.g., normality  and independence)     this research uniquely captures the temporal and spatial
                and  are  widely  applied  to  detect  trends  in  variables   dynamics  of  groundwater  variations.  The  novelty  of
                such as rainfall, evapotranspiration,  and wind speed.   this study lies in the combined use of these advanced
                Such analyses help reveal how  climate  change alters   methodologies, providing deeper insights into regional
                hydrological  systems, impacting  water availability,   hydrometeorological patterns and their implications for
                quality,  and  ecosystem  resilience.  For instance,   sustainable water resource management in a climatically
                precipitation anomalies – linked to both droughts and   sensitive region.
                floods – are increasingly destabilizing economies and   It is important to note that the present study does not
                ecosystems worldwide. 1-7                           incorporate precipitation time series analysis, as long-
                  Trend analysis is a fundamental  approach  for    term  records  show  no  significant  temporal  variations
                detecting and forecasting future patterns in data using
                objective, systematic, and quantitative methodologies.   Table 1. Summary of literature review on trend
                It is particularly effective for examining the impacts of   analysis models
                climate change on hydrometeorological variables, which
                are inherently complex and stochastic, often exhibiting   References      Model name    Trend subject
                significant variability and random fluctuations around   Gaddikeri et al. 26  MK        Meteorological
                an underlying  trend. In this context,  trend analysis                                  variables
                serves as a valuable tool for gaining insights into the   Çelebioğlu and Tayanç 27  RM, MK  Precipitation
                behavior  of hydroclimatic  variables.  However, the   Qadem and Tayfur 28  MK, ITA     Temperature
                stochastic  nature  and intrinsic  properties  of these   Alashan 29      MK            Precipitation
                variables necessitate specialized analytical techniques.   San 30         ITA           Groundwater
                Traditional  statistical  methods commonly used for                                     level
                trend detection  are often constrained  by assumptions   Kessabi et al. 31  MK, ITA, SSE Rainfall
                such as normality, independence, and sufficient record   Likinaw et al. 32  MK, ITA     Extreme
                length.  These assumptions are frequently violated in                                   precipitation
                      7-9
                hydroclimatic datasets. To overcome these limitations,        33
                non-parametric  statistical  tests – characterized  by   Agbo et al.      MK, ITA       Climatic
                                                                                                        parameters
                minimal  distributional  assumptions  – have  become
                increasingly prevalent in recent years. These methods   Sanogo et al. 34  MK            Temperature
                are better suited to accommodate the inherent variability                               and rainfall
                and irregularities of hydrometeorological datasets. 10-15  Gul and Ren 35  ITA          Precipitation
                  Trend analysis models are broadly categorized into   Nguyen et al. 36   MK, ITA       Sea level
                two primary  classes:  Parametric  and  non-parametric.   Seenu and Jayakumar 37  MK, ITA  Extreme
                Parametric models, such as regression models and time                                   rainfall
                series models, rely on specific assumptions regarding   Güçlü 38          MK, ITA       Rainfall
                the underlying data distribution  and relationships.   Caloiero et al. 39  ITA          Seasonal and
                In contrast, non-parametric  models, including the                                      annual rainfall
                Mann–Kendall  (MK) test,  Sen’s slope  estimator,    Abbreviations: ITA: Innovative trend analysis; MK: Mann–Kendall
                Spearman’s rank (SR) correlation test, and innovative   test; SSE: Sen’s slope estimator.



                Volume 22 Issue 3 (2025)                       120                           doi: 10.36922/AJWEP025080052
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