Abstract: Drought is a natural occurrence which is a natural induce phenomenon and which cannot be, controlled by human being but it can be mitigated during and after its occurrence. It is a phenomenon which occurs after a prolong period of rainfall which brings about fast evapotranspiration as a result of high temperature. Indicator like SPI, SPEI, SMI and PCI are used to estimate the analysis of drought. These methods of analysis can give useful information about drought frequency and magnitude. Soil Moisture Index (SMI) shows that evenly distributed soil moisture was recorded from......
Keywords: Drought, SWN, Distribution, SMI, PCI, 2083 – 2022.
[1]
Asefjah, B. F., Fanian, Z., Feizi, A., Abolhasani, H., Paktinat, M., Naghilou, A., Molaei-Atani, M., Asadollahi, M., Babakhani, A., Kouroshinia, F. And Salehi, F. (2014). Drought Monitoring By Using Several Meteorological Drought Indices (Case Study: Salt Lake Basin Of Iran). Desert, 19, 155-165.
[2]
Azarakhshi, M., Mahdavi, M., Arzani, H. And Ahmadi, H. (2011). Assessment Of The Palmer Drought Severity Index In Arid And Semi-Arid Rangeland: (Case Study: Qom Province, Iran). Desert, 16, 77-85.
[3]
Bazrafshan, J And Khalil, A. (2013) . Spatia Analysis Of Meteorological Drought In Iran From 1965-2003. Desert 18 (1), 63-71
[4]
Dastorani, M. T. And Afkhami, H. (2011). Application Of Artificial Neural Networks On Drought Prediction In Yazd (Central Iran). Desert, 16, 39–48.
[5]
Du, L., Than, Q., Yu, T., Men, Q., Jansco, T., Udvardy, P. And Huang, A. T. (2013). A Comprehensive Drought Monitoring Method Integrating Modis And Trmm Data. International Journal Of Applied Earth Observation And Geoformation, 23, 245–253