has been cited by the following article(s):
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[1]
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پیشبینی فصلی بارش بر مبنای ارتباط با سیگنالهای هواشناسی در ایستگاه سینوپتیک یزد
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2020 |
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[2]
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Seasonal Precipitation Forecasting Based on the Teleconnection with Weather Signals in Yazd Synoptic Station
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2020 |
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[3]
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Influence of cut-off irrigation on seed quality and physiological indices of various safflower (Carthamus tinctorius L.) genotypes.
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2019 |
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[4]
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Influence of cut-off irrigation on seed quality and physiological indices of various safflower (Carthamus tinctorius L.) genotypes
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2019 |
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[5]
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Exploring the effects of climatic variables on monthly precipitation variation using a continuous wavelet-based multiscale entropy approach
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Environmental Research,
2018 |
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[6]
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Hybrid MARMA-NARX model for flow forecasting based on the large-scale climate signals, sea-surface temperatures, and rainfall
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2018 |
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[7]
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Is Climate Variability a Problem in Semi-arid Eastern Kenya?
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Journal of Geography, Environment and Earth Science International,
2017 |
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[8]
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Assessment of dust activity and dust-plume pathways over Jazmurian Basin, southeast Iran
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2017 |
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[9]
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The influence of Atlantic-Eurasian teleconnection patterns on temperature regimes in South Caspian Sea coastal areas: a study of Golestan Province, North Iran
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Pollution,
2015 |
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[10]
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Growth and yield parameters of safflower (Carthamus tinctorius) as influenced by foliar methanol application under well-watered and water deficit conditions
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Environmental and Experimental Biology,
2015 |
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[11]
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Meteorological aspects associated with dust storms in the Sistan region, southeastern Iran
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Climate Dynamics,
2014 |
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[1]
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Exploring the effects of climatic variables on monthly precipitation variation using a continuous wavelet-based multiscale entropy approach
Environmental Research,
2018
DOI:10.1016/j.envres.2018.04.017
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[2]
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Assessment of dust activity and dust-plume pathways over Jazmurian Basin, southeast Iran
Aeolian Research,
2017
DOI:10.1016/j.aeolia.2017.01.002
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[3]
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Meteorological aspects associated with dust storms in the Sistan region, southeastern Iran
Climate Dynamics,
2015
DOI:10.1007/s00382-014-2208-3
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