Raindrop size distribution (DSD) data observed with disdrometers at Dari and Delingha in the northeast of the Tibetan Plateau (TP) (summer 2019)

Raindrop size distribution (DSD) data observed with disdrometers at Dari and Delingha in the northeast of the Tibetan Plateau (TP) (summer 2019)


We provided the raindrop size distribution (DSD) observations with OTT PARSIVEL2 disdrometers at Dari (4096 m a.s.l., 33.55°N, 99.95°E) and Delingha (3137 m a.s.l., 37.47°N, 96.81°E) in the northeast of the Tibetan Plateau (TP) during summer 2019. The disdrometers adopted in the data are manufactured by OTT HydroMet. The process of the Data Quality Control (QC) are described in the paper Microphysical Characteristics of Raindrop Size Distribution and Implications for Radar Rainfall Estimation over the Northeastern Tibetan Plateau. Several rainfall integral parameters calculated from the disdrometer observation were provided. The parameters concluded NT (total number concentration of raindrops, m−3), W (liquid water content, g m−3), R (rain rate, mm h−1), Z (radar reflectivity, mm6 m−3), D0 (median volume diameter, mm), and σm (mass spectrum standard deviation). The gamma parameters (N0, μ, and λ) estimated using the moment method (MM), the maximum likelihood method (ML) are provided. The standardized gamma distribution parameters Nw and Dm are also provided. The measurement of microphysical characteristics of precipitation is very essential to the study of the physical and dynamic processes of rainfall over the TP.


File naming and required software

The files are stored in xlsx format with the file names DariDSD2019summer.xlsx and DelinghaDSD2019summer.xlsx. Each data item in the file is for each minute of the observed data. R(rainrate,mm h−1)
NT (total number concentration of raindrops, m−3),
W (liquid water content, g m−3),
Z (radar reflectivity, mm6 m−3)
dbZ (radar reflectivity,dbZ)
D0 (median volume diameter, mm)
Dm ( mass-weighted mean diameter,mm)
Nw (the normalized intercept parameter, m−3 mm−1)
σm (mass spectrum standard deviation, unitless)
N0 ( intercept parameter, m−3 mm−1−μ)
μ (shape parameter, unitless)
λ (slope parameter, mm−1)


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Cite as:

Wei, J., Li, Q. (2021). Raindrop size distribution (DSD) data observed with disdrometers at Dari and Delingha in the northeast of the Tibetan Plateau (TP) (summer 2019). A Big Earth Data Platform for Three Poles, DOI: 10.11888/Atmos.tpdc.271900. CSTR: 18406.11.Atmos.tpdc.271900. (Download the reference: RIS | Bibtex )

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Support Program

National Natural Science Foundation of China (No:51909130)

National Key Research and Development Program (No:2017YFC0403600)

National Key Research and Development Program (No:2016YFE0201900)

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License: This work is licensed under an Attribution 4.0 International (CC BY 4.0)


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Keywords
Geographic coverage
East: 99.95 West: 96.82
South: 33.55 North: 37.48
Details
  • Temporal resolution: --
  • Spatial resolution: --
  • File size: 5 MB
  • Views: 116
  • Downloads: 133
  • Access: Open Access
  • Temporal coverage: 2019-05-01 To 2019-09-30
  • Updated time: 2022-04-15
Contacts
: WEI Jiahua   LI Qiong  

Distributor: A Big Earth Data Platform for Three Poles

Email: poles@itpcas.ac.cn

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