Detection of homogeneous precipitation regions at seasonal and annual time scales, northwest Iran Mohammad Arab Amiri, Mohammad Saadi Mesgari and Christian Conoscenti ABSTRACT Detection of homogeneous climate areas is a challenging issue, which can be affected by different criteria. One of the most prominent factors is choosing the time scale, which can lead to different spatial and temporal patterns. Total precipitation is a key factor in climatological studies, and studying its distribution is of utmost importance. The combination of principal components analysis and cluster analysis is used for homogeneous precipitation areasdetection. Hence, the spatial pattern of total precipitation was investigated in northwestern Iran during the past two decades (19912010) on seasonal and annual time scales. The results of clustering on each time scale were validated, and well-dened clusters were investigated and compared with each other. Two homogeneous sub-regions were recognized in spring, the best period for depicting homogeneous precipitation clusters at seasonal resolution. The annual pattern of precipitation delineated three clusters in the study region. Finally, the characteristics of the well-clustered maps reveal the importance of time scale in detection of homogeneous precipitation sub-zones. Mohammad Arab Amiri (corresponding author) Department of Geographic Information System, Faculty of Geodesy and Geomatics Eng., K. N. Toosi University of Technology, Tehran, Iran E-mail: mohamadamiri89@yahoo.com Mohammad Saadi Mesgari Department of Geographic Information System, Faculty of Geodesy and Geomatics Eng., and Center of Excellence in Geospatial Information Technology (CEGIT), K. N. Toosi University of Technology, Tehran, Iran Christian Conoscenti Department of Earth and Marine Sciences, University of Palermo, Palermo, Italy Key words | cluster analysis, GIS, principal component analysis, time scale, total precipitation INTRODUCTION Regional studies on spatial and temporal climate variability are as vital as those of global studies, especially in large countries with different climate regimes (Türkeş et al. ). Moreover, the changing spatio-temporal patterns of the individual climatic variables are region specic, and vary from one region to another (Qian & Qin ) because climate variables vary in time and space, and their spatio- temporal behavior depends on spatial and temporal scales. Some researchers have incorporated spatial and temporal information, and have found that trends for different climate variables differ signicantly from region to region (Ada- mowski et al. ). Therefore, studying the spatial and temporal variability of climate variables at regional scale is of utmost importance. Temporal trend analysis and spatial interpolation methods have been widely used in spatio-temporal climate variability studies (Shahid ; Santos et al. ; Martins et al. ). The majority of the previously performed researches in climate trend analysis focused on long-term trend detection of the main climate variables such as pre- cipitation and temperature (Haylock & Nicholls ; Griffiths et al. ; Qian & Qin ; Shahid ; Martins et al. ; Taxak et al. ; Arab Amiri et al. ). Regard- ing spatial variability, a set of possible local and regional factors can contribute to the delineation of homogeneous climatic sub-zones (Adamowski et al. ). Moreover, homogeneous regions with similar behavior in terms of cli- matological variables can play an important role in decision-making procedures. This is because identication of homogeneous climate areas at regional scale can be con- sidered an important issue in spatial and temporal analysis of climate time series, and have been proved to be extremely 701 © IWA Publishing 2017 Journal of Water and Climate Change | 08.4 | 2017 doi: 10.2166/wcc.2017.088 Downloaded from http://iwaponline.com/jwcc/article-pdf/8/4/701/239714/jwc0080701.pdf by guest on 04 June 2022