2017
DOI: 10.1002/rra.3147
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Comparison of IDW and Physically Based IDEW Method in Hydrological Modelling for a Large Mountainous Watershed, Northwest China

Abstract: Topography and spatial patterns of landscape significantly affect spatial distribution of precipitation and, in turn, hydrological modelling, especially in high elevation, mountainous watersheds of arid regions. This study incorporates a physically based inverse distance and elevation weighted (PBIDEW) method into a distributed conceptual hydrological model, distributed large basin runoff model, and compared with an inverse distance weighted (IDW) method to assess the performances of both methods in precipitat… Show more

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Cited by 14 publications
(13 citation statements)
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“…The upper reach of the Heihe River Watershed is located in the Qilian Mountain ranges (Figure 1), with a length of 313 km and a drainage area of 10,009 km 2 , producing the majority of runoff for the entire Heihe River Watershed [25]. The local climate is influenced by both the continental climate and the Qinghai-Tibet plateau climate [26], the mean annual temperature ranges from −3.1 to 3.6 • C with the minimum temperature of −28 • C. Mean annual precipitation ranges from 250 mm below 1900 m asl (meters above sea level) to 700 mm above 3600 m asl, and most precipitation (over 60%) falls between June and September.…”
Section: Study Areamentioning
confidence: 99%
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“…The upper reach of the Heihe River Watershed is located in the Qilian Mountain ranges (Figure 1), with a length of 313 km and a drainage area of 10,009 km 2 , producing the majority of runoff for the entire Heihe River Watershed [25]. The local climate is influenced by both the continental climate and the Qinghai-Tibet plateau climate [26], the mean annual temperature ranges from −3.1 to 3.6 • C with the minimum temperature of −28 • C. Mean annual precipitation ranges from 250 mm below 1900 m asl (meters above sea level) to 700 mm above 3600 m asl, and most precipitation (over 60%) falls between June and September.…”
Section: Study Areamentioning
confidence: 99%
“…The local climate is influenced by both the continental climate and the Qinghai-Tibet plateau climate [26], the mean annual temperature ranges from −3.1 to 3.6 • C with the minimum temperature of −28 • C. Mean annual precipitation ranges from 250 mm below 1900 m asl (meters above sea level) to 700 mm above 3600 m asl, and most precipitation (over 60%) falls between June and September. The elevation in the region ranges from 1674 to 5584 m asl [25,27]. In the upper reach of the Heihe River Watershed, the major vegetation types include coniferous forest (Picea crassifolia), shrub (Potentilla fruticosa), steppe (Stipa purpurea Griseb), alpine meadow (Kobresia pygmaea Clarke), alpine sparse vegetation (Saussurea medusa Maxim), and desert (Sympegma regelii Bunge) [28].…”
Section: Study Areamentioning
confidence: 99%
“…In order to reduce the excessive segmentation of watershed technology, several methods have been proposed in relevant foreign literatures. We can refer to labeling-based technology, region merging method [18], scale space method [19], image denoising or edge enhancement based on partial differential equation [20], wavelet technology combined with watershed transform [21], etc. In addition, other scholars have also put forward some suggestions to improve the over-segmented watershed, using space constraint technology to apply to the watershed (SCOW) [22].…”
Section: Related Workmentioning
confidence: 99%
“…then the quantum superposition state structure be defined as: indicate the probability that l  takes 1 and takes 0, that is, the probability that the structural element of the 1st point whose coordinate position is X is "1" and "0". Equation (28) can be expanded according to formula (19) as:…”
mentioning
confidence: 99%
“…TS analysis plays an important role in hydrological research studies, which are handled by mathematical models to predict new records and identify trends. In recent times, mathematical models have taken over most of the important tasks in problem solving in hydrology (Borgonovo, Lu, Plischke, Rakovec, & Hill, 2017;Zhang, He, Li, Wang, & Wang, 2017;Fonesca, Santos, & Santos, 2018;Martin &McCutcheon, 2018 andKavetski, 2018). In TS analysis, it is assumed that the data consist of a systematic pattern with a set of identifiable components and random noise (error).…”
Section: Introductionmentioning
confidence: 99%