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Development of Threshold Levels and a Climate-Sensitivity Model of the Hydrological Regime of the High-Altitude Catchment of the Western Himalayas, Pakistan

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Development of Threshold Levels and a Climate-Sensitivity Model of the Hydrological Regime of the High-Altitude Catchment of the Western Himalayas, Pakistan Civil & Environmental Engineering and Civil & Environmental Engineering and Construction Faculty Publications Construction Engineering 7-14-2019 Development of Threshold Levels and a Climate-Sensitivity Model of the Hydrological Regime of the High-Altitude Catchment of the Western Himalayas, Pakistan Muhammad Saifullah Yunnan University Shiyin Liu Yunnan University, [email protected] Adnan Ahmad Tahir COMSATS University Islamabad Muhammad Zaman University of Agriculture, Faisalabad FSajjadollow thisAhmad and additional works at: https://digitalscholarship.unlv.edu/fac_articles University of Nevada, Las Vegas, [email protected] Part of the Environmental Engineering Commons, and the Hydraulic Engineering Commons See next page for additional authors Repository Citation Saifullah, M., Liu, S., Tahir, A. A., Zaman, M., Ahmad, S., Adnan, M., Chen, D., Ashraf, M., Mehmood, A. (2019). Development of Threshold Levels and a Climate-Sensitivity Model of the Hydrological Regime of the High-Altitude Catchment of the Western Himalayas, Pakistan. Water, 11(7), 1-39. MDPI. http://dx.doi.org/10.3390/w11071454 This Article is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Article in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Article has been accepted for inclusion in Civil & Environmental Engineering and Construction Faculty Publications by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. Authors Muhammad Saifullah, Shiyin Liu, Adnan Ahmad Tahir, Muhammad Zaman, Sajjad Ahmad, Muhammad Adnan, Dianyu Chen, Muhammad Ashraf, and Asif Mehmood This article is available at Digital Scholarship@UNLV: https://digitalscholarship.unlv.edu/fac_articles/685 water Article Development of Threshold Levels and a Climate-Sensitivity Model of the Hydrological Regime of the High-Altitude Catchment of the Western Himalayas, Pakistan Muhammad Saifullah 1,2 , Shiyin Liu 1,* , Adnan Ahmad Tahir 3, Muhammad Zaman 4, Sajjad Ahmad 5 , Muhammad Adnan 6,7 , Dianyu Chen 1, Muhammad Ashraf 8,9 and Asif Mehmood 10 1 Institute of International Rivers and Eco-Security, Yunnan University, Kunming 650500, China 2 Department of Agricultural Engineering, Muhammad Nawaz Shareef University of Agriculture, Multan 66000, Pakistan 3 Department of Environmental Sciences, COMSATS University Islamabad, Abbottabad campus, Abbottabad 22060, Pakistan 4 Department of Irrigation and Drainage, University of Agriculture, Faisalabad 380000, Pakistan 5 Department of Civil and Environmental Engineering and Construction, University of Nevada, Las Vegas, NV 89154, USA 6 State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences (CAS), Lanzhou 730000, China 7 University of Chinese Academy of Sciences, Beijing 100049, China 8 Department of Agricultural Engineering, Khwaja Fareed University of Engineering and Information Technology, Rahim Yar Khan 64200, Pakistan 9 Common Wealth Scientific and Industrial Research Organization Land and Water, Canberra 2601, Australia 10 Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China * Correspondence: [email protected]; Tel.: +86-15288108498 Received: 18 May 2019; Accepted: 9 July 2019; Published: 14 July 2019 Abstract: Water shortages in Pakistan are among the most severe in the world, and its water resources are decreasing significantly due to the prevailing hydro-meteorological conditions. We assessed variations in meteorological and hydrological variables using innovative trend analysis (ITA) and traditional trend analysis methods at a practical significance level, which is also of practical interest. We developed threshold levels of hydrological variables and developed a non-parametric climate-sensitivity model of the high-altitude catchment of the western Himalayas. The runoff of Zone I decreased, while the temperature increased and the precipitation increased significantly. In Zone II, the runoff and temperature increased but the precipitation decreased. A two-dimensional visualization of the Pardé coefficient showed extreme drought events, and indicated greater sensitivity of the hydrological regime to temperature than to precipitation. The threshold levels of runoff for Zones I and II were 320 and 363 mm using the Q80 fixed method, while the mean runoff amounts were estimated to be 79.95 and 55.61 mm, respectively. The transient threshold levels varied by month, and the duration of droughts in Zones I and II ranged from 26.39 to 78.98 days. The sensitivity of the hydrological regime was estimated based on a modified climate-elasticity model ("p = 0.11–0.23, "t = 0.04–2.39) for Zones I and II, respectively. These results highlight the sensitivity − of the hydrological regime to temperature, which influences the melting process. However, it is important to establish thresholds for hydrological variables and understand the climate sensitivity of the hydrological regime of the entire basin, so that policy makers and water managers can make sustainable water-resource-management decisions for this region. Water 2019, 11, 1454; doi:10.3390/w11071454 www.mdpi.com/journal/water Water 2019, 11, 1454 2 of 39 Keywords: drought severity; drought duration; precipitation sensitivity; temperature sensitivity; climate change 1. Introduction Water is extremely important to all human beings, and is also necessary for a country’s agricultural, industrial, and socioeconomic development. There is a discontinuous layer of water on the surface of the Earth, known as the hydrosphere. Concentrations of greenhouse gases in the atmosphere are increasing, causing global warming and affecting precipitation [1]. These principle factors, i.e., precipitation and temperature, affect the hydrosphere due to their influence on snow [2] and glacial melt [3], which in turn affect runoff to major rivers [4–6], the levels of which have changed significantly [7–10]. The increase in water shortage crises has led to a number of water-related disasters around the world [11,12]. Motivated by these extreme events, the threshold levels of runoff have been determined by various researchers worldwide [13,14]. The duration and severity of droughts is determined based on fixed and monthly thresholds for a given time series [15]. The sensitivity of runoff to climate variation [16], and the runoff thresholds [14], have been analyzed to identify drought events [17] according to the hydrological regime. This has been a major area of interest for global hydrology researchers over the last decade [6,18,19]. The authors of [20] described a hydrological drought as “a significant decrease in the availability of water in all its forms, appearing in the land phase of the hydrological cycle.” Different approaches are widely used in drought analyses [14,17,21–24]. The authors of [25] used variable thresholds to analyze seasonal, monthly, and daily stream flows. Similarly, the authors of [14] reported that the stream-flow threshold is a key variable for describing hydrological droughts, based on each component of the hydrological cycle. The threshold levels at Q80,Q70 and Q90 have been evaluated to identify drought events with different durations. Stream flow is the main water source for several water-dependent activities, such as hydropower generation, recreation, and irrigation for agriculture. For the purpose of sustainable water-resource management, it is necessary to establish threshold levels and understand the relationship between precipitation and temperature within a hydrological regime [26,27]. Precipitation and temperature are considered to contribute significantly to variations in a given hydrological regime [28,29]. Different methods have been applied to assess the climate sensitivity of hydrological regimes using both parametric and non-parametric approaches [5,30,31]. These methods can be classified as follows: paired-catchment, statistical, and hydrological modeling methods. The drawback of the paired-catchment method is that it is difficult and expensive to identify two catchments with similar characteristics. A large set of parameters is required to apply the hydrological-modeling method, in which these parameters are used to calibrate and validate the model. This makes it difficult to model basins in data-scarce regions [32–34]. The Budyko framework is considered an effective tool for assessing the sensitivity of a hydrological regime to precipitation and temperature [35–37]. This framework has been used successfully for different rivers globally [6,38]. The non-parametric approach shows a clear relationship between precipitation and temperature within a hydrological regime [39]. Hydrological regimes are sensitive to precipitation and temperature in different regions [5,40]. As it is based directly on long-term observational records, climate-sensitivity analysis is generally reliable. Pakistan’s economy is highly dependent on agriculture, for which water resources are essential. The main tributaries to the Indus river system (IRS) are a number of streams originating from the Tibetan Plateau,
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