Long-term decline in rainfall causing depletion in groundwater aquifer storage sustaining the springflow in the middle-Himalayan headwaters

This paper is an attempt to study the cause and effect of the reported widespread decline in spring-flow from a catchment in the middle Himalaya in the Garhwal region. A range of statistical tests to the long rainfall data series is applied to the two gauge-based interpolated gridded data. A decline...

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Veröffentlicht in:Journal of Earth System Science 2023-09, Vol.132 (3), p.124, Article 124
Hauptverfasser: Tarafdar, Soukhin, Dutta, Subhashis
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description This paper is an attempt to study the cause and effect of the reported widespread decline in spring-flow from a catchment in the middle Himalaya in the Garhwal region. A range of statistical tests to the long rainfall data series is applied to the two gauge-based interpolated gridded data. A decline in annual and seasonal rainfall with a rising frequency of moderate to severe drought in the subseries (1961–2018) is observed compared to the first half of the 20th century. A sudden shift of declining trend is observed in IMD4 gridded data in the early to mid-sixties. Prolonged post-monsoon and winter recession characteristics are analysed through a single nonlinear model and a power-law model. The nonlinear model and event-based power-law recession analysis showed nonlinearity ( B ≠1) in a storage–discharge relationship at the spring catchment scale as well as the intercept ( A ) highlights a very fast-draining aquifer with a very short recession timescale. The log-transformed fitted single nonlinear modelled recession data revealed control of antecedent storage over the rate of outflow as parallel offset was observed in interannual prolonged recession curve in –dQ/dt vs . Q plot. Groundwater reservoir contributing to Ayal springflow is very vulnerable to reservoir storage changes. Research highlights In recent time, threat to water sustainability in middle Himalaya is widely reported. However, a clear understanding of the cause is not being investigated in a systematic manner. The present study highlights that deficient monsoon years as well as dry winter months, are causing multi-year drought in middle Himalaya basins. Higher frequency of moderate drought is observed in the long-term rainfall data after the early to mid-sixties and may have caused the decline in springflow. Recession characteristics of springflow showed nonlinearity in storage–discharge relationship as well as very short recession time scale and springflow are extremely vulnerable to aquifer storage change.
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The log-transformed fitted single nonlinear modelled recession data revealed control of antecedent storage over the rate of outflow as parallel offset was observed in interannual prolonged recession curve in –dQ/dt vs . Q plot. Groundwater reservoir contributing to Ayal springflow is very vulnerable to reservoir storage changes. Research highlights In recent time, threat to water sustainability in middle Himalaya is widely reported. However, a clear understanding of the cause is not being investigated in a systematic manner. The present study highlights that deficient monsoon years as well as dry winter months, are causing multi-year drought in middle Himalaya basins. Higher frequency of moderate drought is observed in the long-term rainfall data after the early to mid-sixties and may have caused the decline in springflow. 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A range of statistical tests to the long rainfall data series is applied to the two gauge-based interpolated gridded data. A decline in annual and seasonal rainfall with a rising frequency of moderate to severe drought in the subseries (1961–2018) is observed compared to the first half of the 20th century. A sudden shift of declining trend is observed in IMD4 gridded data in the early to mid-sixties. Prolonged post-monsoon and winter recession characteristics are analysed through a single nonlinear model and a power-law model. The nonlinear model and event-based power-law recession analysis showed nonlinearity ( B ≠1) in a storage–discharge relationship at the spring catchment scale as well as the intercept ( A ) highlights a very fast-draining aquifer with a very short recession timescale. The log-transformed fitted single nonlinear modelled recession data revealed control of antecedent storage over the rate of outflow as parallel offset was observed in interannual prolonged recession curve in –dQ/dt vs . Q plot. Groundwater reservoir contributing to Ayal springflow is very vulnerable to reservoir storage changes. Research highlights In recent time, threat to water sustainability in middle Himalaya is widely reported. However, a clear understanding of the cause is not being investigated in a systematic manner. The present study highlights that deficient monsoon years as well as dry winter months, are causing multi-year drought in middle Himalaya basins. Higher frequency of moderate drought is observed in the long-term rainfall data after the early to mid-sixties and may have caused the decline in springflow. 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A range of statistical tests to the long rainfall data series is applied to the two gauge-based interpolated gridded data. A decline in annual and seasonal rainfall with a rising frequency of moderate to severe drought in the subseries (1961–2018) is observed compared to the first half of the 20th century. A sudden shift of declining trend is observed in IMD4 gridded data in the early to mid-sixties. Prolonged post-monsoon and winter recession characteristics are analysed through a single nonlinear model and a power-law model. The nonlinear model and event-based power-law recession analysis showed nonlinearity ( B ≠1) in a storage–discharge relationship at the spring catchment scale as well as the intercept ( A ) highlights a very fast-draining aquifer with a very short recession timescale. The log-transformed fitted single nonlinear modelled recession data revealed control of antecedent storage over the rate of outflow as parallel offset was observed in interannual prolonged recession curve in –dQ/dt vs . Q plot. Groundwater reservoir contributing to Ayal springflow is very vulnerable to reservoir storage changes. Research highlights In recent time, threat to water sustainability in middle Himalaya is widely reported. However, a clear understanding of the cause is not being investigated in a systematic manner. The present study highlights that deficient monsoon years as well as dry winter months, are causing multi-year drought in middle Himalaya basins. Higher frequency of moderate drought is observed in the long-term rainfall data after the early to mid-sixties and may have caused the decline in springflow. Recession characteristics of springflow showed nonlinearity in storage–discharge relationship as well as very short recession time scale and springflow are extremely vulnerable to aquifer storage change.</abstract><cop>New Delhi</cop><pub>Springer India</pub><doi>10.1007/s12040-023-02136-8</doi><orcidid>https://orcid.org/0000-0001-8520-3103</orcidid></addata></record>
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source Indian Academy of Sciences; Springer Nature - Complete Springer Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals
subjects Aerosols
Annual rainfall
Aquifer storage
Aquifers
Catchment area
Catchment scale
Climate change
Discharge
Drought
Earth and Environmental Science
Earth Sciences
Freshwater resources
Groundwater
Groundwater depletion
Groundwater reservoirs
Groundwater storage
Headwaters
Hydrologic data
Monsoons
Nonlinear systems
Nonlinearity
Outflow
Power law
Precipitation
Rain
Rainfall
Rainfall data
Recession curve
Recession curves
Recessions
Reservoir storage
Reservoirs
Seasonal rainfall
Space Exploration and Astronautics
Space Sciences (including Extraterrestrial Physics
Spring
Spring (season)
Statistical analysis
Statistical tests
Stream flow
Summer
Temperature
Trends
Wind
Winter
title Long-term decline in rainfall causing depletion in groundwater aquifer storage sustaining the springflow in the middle-Himalayan headwaters
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