DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX

Drought is one of the most common natural phenomena. Many indices using multiple data types have been created, and their success at recognizing periods of extreme wetness and dryness has been well documented. The merit of the method is the utilization of terrestrial water storage (TWS) variations fr...

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Main Authors: I. Kordpour, S. Farzaneh, R. Shahhoseini
Format: Article
Language:English
Published: Copernicus Publications 2019-10-01
Series:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Online Access:https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-4-W18/659/2019/isprs-archives-XLII-4-W18-659-2019.pdf
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spelling doaj-9eaf166c0822476599863f0ab471a2332020-11-25T02:35:51ZengCopernicus PublicationsThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences1682-17502194-90342019-10-01XLII-4-W1865966310.5194/isprs-archives-XLII-4-W18-659-2019DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEXI. Kordpour0S. Farzaneh1R. Shahhoseini2School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, IranSchool of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, IranSchool of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, IranDrought is one of the most common natural phenomena. Many indices using multiple data types have been created, and their success at recognizing periods of extreme wetness and dryness has been well documented. The merit of the method is the utilization of terrestrial water storage (TWS) variations from Gravity Recovery and Climate Experiment (GRACE) quantification of drought intensity. Alongside with these observations, we add precipitation data to equations. In this study, we analyze Merged-dataset Drought index (MDI) using GRACE-derived TWSA and precipitation in Iran, where most of the area is desert and mountain in the middle and South of the country. Our sample period is from January 2003 to December 2014. MDI shows a strong correlation with existing drought indices, especially with the Palmer Drought Severity Index (PDSI). Based on the obtained results, MDI indicates a moderate Drought event in 2008 and 2012–2015, which is compatible with the recorded result of PDSI. The longest drought took 22 months (from January 2008 to October 2009). Interestingly, the coefficient of correlation between MDI and PDSI is 0.67.https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-4-W18/659/2019/isprs-archives-XLII-4-W18-659-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Kordpour
S. Farzaneh
R. Shahhoseini
spellingShingle I. Kordpour
S. Farzaneh
R. Shahhoseini
DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
author_facet I. Kordpour
S. Farzaneh
R. Shahhoseini
author_sort I. Kordpour
title DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
title_short DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
title_full DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
title_fullStr DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
title_full_unstemmed DROUGHT ASSESSMENT OF IRAN USING THE MDI INDEX
title_sort drought assessment of iran using the mdi index
publisher Copernicus Publications
series The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
issn 1682-1750
2194-9034
publishDate 2019-10-01
description Drought is one of the most common natural phenomena. Many indices using multiple data types have been created, and their success at recognizing periods of extreme wetness and dryness has been well documented. The merit of the method is the utilization of terrestrial water storage (TWS) variations from Gravity Recovery and Climate Experiment (GRACE) quantification of drought intensity. Alongside with these observations, we add precipitation data to equations. In this study, we analyze Merged-dataset Drought index (MDI) using GRACE-derived TWSA and precipitation in Iran, where most of the area is desert and mountain in the middle and South of the country. Our sample period is from January 2003 to December 2014. MDI shows a strong correlation with existing drought indices, especially with the Palmer Drought Severity Index (PDSI). Based on the obtained results, MDI indicates a moderate Drought event in 2008 and 2012–2015, which is compatible with the recorded result of PDSI. The longest drought took 22 months (from January 2008 to October 2009). Interestingly, the coefficient of correlation between MDI and PDSI is 0.67.
url https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLII-4-W18/659/2019/isprs-archives-XLII-4-W18-659-2019.pdf
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