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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Spatial statistics analysis of precipitation in the Urmia Lake Basin</dc:title><dc:creator>Aghamohammadi,	Hossein	(Avtor)
	</dc:creator><dc:creator>Behzadi,	Saeed	(Avtor)
	</dc:creator><dc:creator>Moshtaghinejad,	Fatemeh	(Avtor)
	</dc:creator><dc:subject>precipitation estimation</dc:subject><dc:subject>geostatistics</dc:subject><dc:subject>spatial relationship modeling</dc:subject><dc:subject>hydrology</dc:subject><dc:subject>kriging interpolation</dc:subject><dc:description>Most of the world's population lives in areas facing a severe water crisis. Climatology researchers need
precipitation information, pattern analysis, modeling of spatial relationships, and more to cope with these
conditions. Therefore, in this paper, a comprehensive approach is developed for describing geographic
phenomenon using various geostatistical techniques. Two main methods of interpolation (Inverse Distance
Weighting and Kriging) are used and their results are compared. The Urmia Lake Basin in Iran was selected
as a case-study area that has faced critical conditions in recent years. Precipitation was initially modeled using
both conventional, non-statistical approaches and advanced geo-statistical methods. The result of the
comparison shows that ordinary Kriging is the best interpolation method for precipitation, with an RMS of
4.15, and Local Polynomial Interpolation with the exponential kernel function is the worst method, with an
RMS of 5.02. Finally, a general regression analysis was conducted on precipitation data to examine its
relationship with other variables. The results show that the latitude variable was identified as the dependent
variable with the most influence on precipitation, with an impact factor of 81%, and that the slope has the
lowest impact on precipitation, at nearly zero percent. The influence of latitude on precipitation appears to be
localized, suggesting that it may not be a significant variable for predicting global environmental threats.</dc:description><dc:date>2023</dc:date><dc:date>2024-10-03 14:09:28</dc:date><dc:type>Članek v reviji</dc:type><dc:identifier>163186</dc:identifier><dc:identifier>UDK: 502/504:551.577.5(55)(078.7)</dc:identifier><dc:identifier>ISSN pri članku: 0352-3551</dc:identifier><dc:identifier>DOI: 10.15292/acta.hydro.2023.09</dc:identifier><dc:identifier>COBISS_ID: 210122499</dc:identifier><dc:language>sl</dc:language></metadata>
