Modeling and predicting of the spatial variations Precipitation cores in Iran

This research was carried out with the aim of understanding the spatial displacement of rainfall nuclei as an effective factor in the future hydrological conditions in Iran. Two types of databases were used to conduct this research. The first type of data is the monthly precipitation of 86 synoptic...

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Main Authors: hossein naserzadeh, fariba sayadi, meysam toulabi nejad
Format: Article
Language:fas
Published: Kharazmi University 2019-12-01
Series:تحقیقات کاربردی علوم جغرافیایی
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Online Access:http://jgs.khu.ac.ir/article-1-3101-en.pdf
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author hossein naserzadeh
fariba sayadi
meysam toulabi nejad
author_facet hossein naserzadeh
fariba sayadi
meysam toulabi nejad
author_sort hossein naserzadeh
collection DOAJ
description This research was carried out with the aim of understanding the spatial displacement of rainfall nuclei as an effective factor in the future hydrological conditions in Iran. Two types of databases were used to conduct this research. The first type of data is the monthly precipitation of 86 synoptic stations with the statistical period of 1986-1989 and the second type of predicted data from the output of the CCSM4 model under the three scenarios (RCP2.6, RCP4.5, and RCP6) from 2016 to 2036. After collecting and modeling the data, the maps were mapped to the ARCGIS environment. The results of the study showed that the terrestrial nuclei in the whole of Iran's zone in the four seasons will have changes with a negative trend in the future. The coefficient of rainfall variation in the spring, summer, autumn and winter seasons will be 61.4, 101.4, 58.9 and 55.8 percent, respectively. The results of the triple scenario study showed that the displacement of the spring core from all north north of the country to the northwest of the country is limited to the common borders of Iran, Turkey and Armenia (the Maku and Jolfa region), but in summer, the high core The northern shores and parts of the northwest of the country will be transported to the south of the country (around Khash and Saravan). In the autumn, the high-lying zone, which is located throughout the northern part of the country, will move to two distinct nuclei in the central Zagros (Dena and Zadkouh areas) and southwest Khazars (Anzali and Astara areas), and the core of winter from the central Zagros And the Caspian region will be transferred to the northwest of Kurdistan and southwest of West Azarbaijan, which will be seen in all scenarios. Another point is that, in addition to reducing the boulders, in the future, drought areas will cover more of the country.
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series تحقیقات کاربردی علوم جغرافیایی
spelling doaj-art-39c959c7cec74359910d95d40ac6f6e62025-01-31T17:26:10ZfasKharazmi Universityتحقیقات کاربردی علوم جغرافیایی2228-77362588-51382019-12-011955117133Modeling and predicting of the spatial variations Precipitation cores in Iranhossein naserzadeh0fariba sayadi1meysam toulabi nejad2 Assistant Professor of climatology , Kharazmi University PhD student of climatology, Kharazmi University, Tehran, Iran PhD student of climatology, Kharazmi University, Tehran, Iran This research was carried out with the aim of understanding the spatial displacement of rainfall nuclei as an effective factor in the future hydrological conditions in Iran. Two types of databases were used to conduct this research. The first type of data is the monthly precipitation of 86 synoptic stations with the statistical period of 1986-1989 and the second type of predicted data from the output of the CCSM4 model under the three scenarios (RCP2.6, RCP4.5, and RCP6) from 2016 to 2036. After collecting and modeling the data, the maps were mapped to the ARCGIS environment. The results of the study showed that the terrestrial nuclei in the whole of Iran's zone in the four seasons will have changes with a negative trend in the future. The coefficient of rainfall variation in the spring, summer, autumn and winter seasons will be 61.4, 101.4, 58.9 and 55.8 percent, respectively. The results of the triple scenario study showed that the displacement of the spring core from all north north of the country to the northwest of the country is limited to the common borders of Iran, Turkey and Armenia (the Maku and Jolfa region), but in summer, the high core The northern shores and parts of the northwest of the country will be transported to the south of the country (around Khash and Saravan). In the autumn, the high-lying zone, which is located throughout the northern part of the country, will move to two distinct nuclei in the central Zagros (Dena and Zadkouh areas) and southwest Khazars (Anzali and Astara areas), and the core of winter from the central Zagros And the Caspian region will be transferred to the northwest of Kurdistan and southwest of West Azarbaijan, which will be seen in all scenarios. Another point is that, in addition to reducing the boulders, in the future, drought areas will cover more of the country.http://jgs.khu.ac.ir/article-1-3101-en.pdfprecipitation modelingprecipitation coresccsm modelrcpiran.
spellingShingle hossein naserzadeh
fariba sayadi
meysam toulabi nejad
Modeling and predicting of the spatial variations Precipitation cores in Iran
تحقیقات کاربردی علوم جغرافیایی
precipitation modeling
precipitation cores
ccsm model
rcp
iran.
title Modeling and predicting of the spatial variations Precipitation cores in Iran
title_full Modeling and predicting of the spatial variations Precipitation cores in Iran
title_fullStr Modeling and predicting of the spatial variations Precipitation cores in Iran
title_full_unstemmed Modeling and predicting of the spatial variations Precipitation cores in Iran
title_short Modeling and predicting of the spatial variations Precipitation cores in Iran
title_sort modeling and predicting of the spatial variations precipitation cores in iran
topic precipitation modeling
precipitation cores
ccsm model
rcp
iran.
url http://jgs.khu.ac.ir/article-1-3101-en.pdf
work_keys_str_mv AT hosseinnaserzadeh modelingandpredictingofthespatialvariationsprecipitationcoresiniran
AT faribasayadi modelingandpredictingofthespatialvariationsprecipitationcoresiniran
AT meysamtoulabinejad modelingandpredictingofthespatialvariationsprecipitationcoresiniran