Analyses of meteorological drought and its impacts on groundwater fluctuations, a case study: Marand Plain (Iran)
Abstract
Meteorological drought
is one specific type of drought that occurs when precipitation is less than the
long-term averages in a particular area. One of the hazardous impacts of this
phenomenon observed on subsurface waters is the decline of water level in response
to droughts. In this study, the climatic and groundwater data were used to
analyze their trends in Marand plain, NW Iran, over the past decades to
understand the likely relationship between them. To this, groundwater level
data were first analyzed and its temporal trends were extracted. Then, the
climatic condition of the region studied using the Ombrothermic diagram.
Finally, drought analyses were conducted through drought index (SPI). Based on
the results of the study, a descending trend was detected in both monthly and
annual fluctuations of the groundwater level. It's also found that the region
had a partially dry climate with a period of dry months between May and
October. The SPI values showed extremely dry periods in 2001 and 2002 and
months of July and June during the study period. The joint analysis of
groundwater level and SPI values revealed that the impacts of drought were
evident on groundwater level changes. Accordingly, the region's groundwater
fluctuations found to be mostly under the control of monthly droughts where
water level responds to wet and dry months in an expected manner. However, it's
also found that the yearly changes in the groundwater level of the study area
were not directly correlated to drought periods, suggesting that other factors
might be effective in this phenomenon.
Keywords
References
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Details
Primary Language
English
Subjects
Engineering
Journal Section
Research Article
Publication Date
November 25, 2019
Submission Date
August 21, 2018
Acceptance Date
-
Published in Issue
Year 2019 Volume: 25 Number: 6