2023
DOI: 10.1007/s11430-022-1081-4
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Cross-sectional rainfall observation on the central-western Tibetan Plateau in the warm season: System design and preliminary results

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Cited by 12 publications
(8 citation statements)
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“…The precipitation records from 23 independent rain gauges were also used for our evaluation. These rain gauges are completely independent of those gauges in CMPA (Yang et al., 2023). All these gauges are located above 4,000 m in the center of the TP where the ground gauges are sparsely distributed (31.40°N–32.51°N, 79.69°E–90.86°E).…”
Section: Study Area and Datasetsmentioning
confidence: 99%
“…The precipitation records from 23 independent rain gauges were also used for our evaluation. These rain gauges are completely independent of those gauges in CMPA (Yang et al., 2023). All these gauges are located above 4,000 m in the center of the TP where the ground gauges are sparsely distributed (31.40°N–32.51°N, 79.69°E–90.86°E).…”
Section: Study Area and Datasetsmentioning
confidence: 99%
“…They include 1) a New Integrated Observational System over the TP (NIOST) (Xu et al 2008), 2) the Third TP Atmospheric Scientific Experiment (TIPEX-III) (Zhao et al 2018), 3) the Third Pole Environment Integrated Three-dimensional Observation and Research Platform (TPEITORP) (Ma et al 2008(Ma et al , 2023a, 4) the TP-River (Wang et al 2021), and 5) the cross-sectional rainfall observation on the central-western TP (Yang et al 2023). Parallelly, various networks concentrate on local or basin-specific scales, including the Heihe Watershed Allied Telemetry Experimental Research (HiWATER) by Li et al (2013), the multiscale Soil Moisture and Temperature Monitoring Network on the central TP (CTP-SMTMN) developed by Yang et al (2013), and the Cryospheric Hydrometeorology Observation in the Hulu Catchment (CHOICE) initiated by Han et al (2018). Additional efforts encompass the Qinghai Lake Basin Critical Zone Observatory (Li et al 2018), meteorology-cryosphere-hydrology observations in the upper Brahmaputra basin (Wang et al 2022), the Qomolangma Special Atmospheric Processes and Environmental Changes (QOMS) observation network (Ma et al 2023b), and the Soil Moisture Monitoring Network and in situ observations of soil hydraulic properties on the northeastern TP (upstream regions of Heihe River basin) (Tian et al 2023).…”
Section: E443mentioning
confidence: 99%
“…Two observation transects running south-north and west-east across this region were used to obtain hourly rainfall data during the warm season (May-September). The south-north transect extends from Yadong Valley to Shuanghu County; the west-east transect extends from Shiquanhe to Naqu in the central TP [11]. We downloaded the hourly rain gauge data for the warm season (May-September) in the central and western Tibetan Plateau in 2018 from the National Tibetan Plateau Data Center DOI: 10.11888/Atmos.tpdc.272983 (accessed on 21 December 2023) and calculated total precipitation during the warm season for 19 stations along the south-north transect and for 20 stations along the west-east transect.…”
Section: High-resolution Precipitation Product Materials 241 Gauge Ra...mentioning
confidence: 99%
“…PR3(SMAI, EDI) = R(SMAI i,j , EDI i,j ) + R(NDV I A i,j , EDI i,j ) 2 (11) where PR1, PR2, PR3 is the correlation predictor, and i and j are the pixel column and line serial number, respectively.…”
Section: Pr1(smai Edi) =mentioning
confidence: 99%
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