World's Best Scientists 2026 revealed!

D-Index & Metrics

Environmental Sciences

D-Index
44
Citations
9892
World Ranking
6637
National Ranking
669

Rucong Yu publication distribution in Environmental Sciences in 2026

The chart shows the distribution of publications by all Research.com ranked scientists in the field of Environmental Sciences in 2026. The highlighted bar marks where Rucong Yu sits on this spectrum.

41–50 publications: 21 scientists 51–60 publications: 62 scientists 61–70 publications: 133 scientists 71–80 publications: 257 scientists 81–90 publications: 361 scientists 91–100 publications: 440 scientists 101–110 publications: 492 scientists 111–120 publications: 541 scientists 121–130 publications: 617 scientists 131–140 publications: 544 scientists 141–150 publications: 541 scientists 151–160 publications: 539 scientists 161–170 publications: 444 scientists 171–180 publications: 444 scientists 181–190 publications: 400 scientists 191–200 publications: 377 scientists 201–210 publications: 318 scientists 211–220 publications: 282 scientists 221–230 publications: 263 scientists 231–240 publications: 220 scientists 241–250 publications: 217 scientists 251–260 publications: 180 scientists 261–270 publications: 181 scientists 271–280 publications: 155 scientists 281–290 publications: 130 scientists 291–300 publications: 127 scientists 301–310 publications: 130 scientists 311–320 publications: 85 scientists 321–330 publications: 106 scientists 331–340 publications: 80 scientists 341–350 publications: 83 scientists 351–360 publications: 75 scientists 361–370 publications: 69 scientists 371–380 publications: 52 scientists 381–390 publications: 54 scientists 391–400 publications: 56 scientists 401–410 publications: 44 scientists 411–420 publications: 40 scientists 421–430 publications: 36 scientists 431–440 publications: 25 scientists 441–450 publications: 25 scientists 451–460 publications: 32 scientists 461–470 publications: 29 scientists 471–480 publications: 21 scientists 481–490 publications: 26 scientists 491–500 publications: 26 scientists 501–510 publications: 17 scientists 511–520 publications: 19 scientists 521–530 publications: 15 scientists 531–540 publications: 22 scientists 541–550 publications: 12 scientists 551–560 publications: 15 scientists 561–570 publications: 11 scientists 571–580 publications: 19 scientists 581–590 publications: 9 scientists 591–600 publications: 9 scientists 601–610 publications: 7 scientists 611–620 publications: 11 scientists 621–630 publications: 5 scientists 631–640 publications: 5 scientists 641–650 publications: 6 scientists 651–660 publications: 3 scientists 661–670 publications: 3 scientists 671–680 publications: 4 scientists 681–689 publications: 4 scientists 690+ publications: 100 scientists
41 publications 690+

This scientist: 115 publications — 21st percentile

21% of scientists in this discipline score the same or lower.

The last bar groups every scientist with 690 publications or more.

Rucong Yu D-index placement in Environmental Sciences in 2026

The chart shows the D-index (discipline H-index) distribution of Environmental Sciences scientists ranked by Research.com in 2026. The highlighted bar marks where Rucong Yu sits on this spectrum.

30 D-Index: 12 scientists 31 D-Index: 26 scientists 32 D-Index: 51 scientists 33 D-Index: 88 scientists 34 D-Index: 123 scientists 35 D-Index: 163 scientists 36 D-Index: 206 scientists 37 D-Index: 267 scientists 38 D-Index: 265 scientists 39 D-Index: 275 scientists 40 D-Index: 321 scientists 41 D-Index: 343 scientists 42 D-Index: 305 scientists 43 D-Index: 336 scientists 44 D-Index: 330 scientists 45 D-Index: 348 scientists 46 D-Index: 291 scientists 47 D-Index: 275 scientists 48 D-Index: 272 scientists 49 D-Index: 273 scientists 50 D-Index: 263 scientists 51 D-Index: 232 scientists 52 D-Index: 266 scientists 53 D-Index: 217 scientists 54 D-Index: 198 scientists 55 D-Index: 177 scientists 56 D-Index: 202 scientists 57 D-Index: 204 scientists 58 D-Index: 166 scientists 59 D-Index: 177 scientists 60 D-Index: 166 scientists 61 D-Index: 152 scientists 62 D-Index: 143 scientists 63 D-Index: 150 scientists 64 D-Index: 124 scientists 65 D-Index: 119 scientists 66 D-Index: 120 scientists 67 D-Index: 118 scientists 68 D-Index: 82 scientists 69 D-Index: 98 scientists 70 D-Index: 94 scientists 71 D-Index: 105 scientists 72 D-Index: 74 scientists 73 D-Index: 84 scientists 74 D-Index: 70 scientists 75 D-Index: 67 scientists 76 D-Index: 78 scientists 77 D-Index: 60 scientists 78 D-Index: 59 scientists 79 D-Index: 52 scientists 80 D-Index: 47 scientists 81 D-Index: 38 scientists 82 D-Index: 48 scientists 83 D-Index: 42 scientists 84 D-Index: 42 scientists 85 D-Index: 43 scientists 86 D-Index: 29 scientists 87 D-Index: 37 scientists 88 D-Index: 29 scientists 89 D-Index: 30 scientists 90 D-Index: 34 scientists 91 D-Index: 20 scientists 92 D-Index: 22 scientists 93 D-Index: 17 scientists 94 D-Index: 19 scientists 95 D-Index: 24 scientists 96 D-Index: 21 scientists 97 D-Index: 20 scientists 98 D-Index: 24 scientists 99 D-Index: 17 scientists 100 D-Index: 17 scientists 101 D-Index: 21 scientists 102 D-Index: 25 scientists 103 D-Index: 18 scientists 104 D-Index: 26 scientists 105 D-Index: 20 scientists 106 D-Index: 15 scientists 107 D-Index: 10 scientists 108 D-Index: 13 scientists 109 D-Index: 15 scientists 110 D-Index: 12 scientists 111 D-Index: 8 scientists 112 D-Index: 7 scientists 113 D-Index: 9 scientists 114 D-Index: 6 scientists 115 D-Index: 12 scientists 116 D-Index: 7 scientists 117 D-Index: 8 scientists 118 D-Index: 3 scientists 119 D-Index: 5 scientists 120 D-Index: 7 scientists 121 D-Index: 2 scientists 122 D-Index: 4 scientists 123 D-Index: 8 scientists 124 D-Index: 7 scientists 125 D-Index: 9 scientists 126+ D-Index: 92 scientists
30 D-Index 126+

This scientist: 44 D-Index — 32nd percentile

32% of scientists in this discipline score the same or lower.

The last bar groups every scientist with 126 D-Index or more.

Overview

Rucong Yu is affiliated with the China Meteorological Administration in China and has contributed extensively to the fields of Earth and Planetary Sciences and Environmental Science. Their research primarily focuses on Atmospheric Science and Global and Planetary Change, engaging with several topics within these domains.

The main areas of study for Rucong Yu include:

  • Meteorological Phenomena and Simulations
  • Climate variability and models
  • Tropical and Extratropical Cyclones Research
  • Cryospheric studies and observations
  • Hydrology and Drought Analysis
  • Precipitation Measurement and Analysis
  • Atmospheric and Environmental Gas Dynamics

Rucong Yu has coauthored multiple publications with a set of frequent collaborators. These include:

  • Jian Li
  • Yi Zhang
  • Yihui Zhou
  • Xuelin Hu
  • Weihua Yuan

The scientist has published in a variety of journals, with recurring appearances in the following venues:

  • Climate Dynamics
  • Atmospheric Research
  • Advances in Atmospheric Sciences
  • Geoscientific model development
  • Advances in Climate Change Research

Selected recent papers by Rucong Yu include:

  • "BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model," 2021, Geoscientific model development
  • "Evaluation of CMIP6 HighResMIP models in simulating precipitation over Central Asia," 2021, Advances in Climate Change Research
  • "A Multiscale Dynamical Model in a Dry-Mass Coordinate for Weather and Climate Modeling: Moist Dynamics and Its Coupling to Physics," 2020, Monthly Weather Review
  • "AMIP Simulations of a Global Model for Unified Weather-Climate Forecast: Understanding Precipitation Characteristics and Sensitivity Over East Asia," 2021, Journal of Advances in Modeling Earth Systems
  • "Configuration and evaluation of a global unstructured mesh atmospheric model (GRIST-A20.9) based on the variable-resolution approach," 2020, Geoscientific model development

Best Publications

  • Atmospheric water vapor transport associated with typical anomalous summer rainfall patterns in China

    Tian-Jun Zhou;Ru-Cong Yu

  • Why the Western Pacific Subtropical High Has Extended Westward since the Late 1970s

    Tianjun Zhou;Rucong Yu;Jie Zhang;Helge Drange

  • Tropospheric cooling and summer monsoon weakening trend over East Asia

    Rucong Yu;Bin Wang;Bin Wang;Tianjun Zhou

  • Twentieth-Century Surface Air Temperature over China and the Globe Simulated by Coupled Climate Models

    Tianjun Zhou;Rucong Yu

  • Diurnal variations of summer precipitation over contiguous China

    Rucong Yu;Tianjun Zhou;Anyuan Xiong;Yanjun Zhu

  • Summer Precipitation Frequency, Intensity, and Diurnal Cycle over China: A Comparison of Satellite Data with Rain Gauge Observations

    Tianjun Zhou;Rucong Yu;Haoming Chen;Aiguo Dai

  • Seasonality and Three-Dimensional Structure of Interdecadal Change in the East Asian Monsoon

    Rucong Yu;Tianjun Zhou

  • The Beijing Climate Center atmospheric general circulation model: description and its performance for the present-day climate

    Tongwen Wu;Rucong Yu;Fang Zhang;Zaizhi Wang

  • Relation between rainfall duration and diurnal variation in the warm season precipitation over central eastern China

    Rucong Yu;Youping Xu;Tianjun Zhou;Jian Li

  • Ocean Forcing to Changes in Global Monsoon Precipitation over the Recent Half-Century

    Tianjun Zhou;Rucong Yu;Hongmei Li;Bin Wang

  • Drought in Late Spring of South China in Recent Decades

    Xiaoge Xin;Rucong Yu;Tianjun Zhou;Bin Wang

  • Long-Term Changes in Rainfall over Eastern China and Large-Scale Atmospheric Circulation Associated with Recent Global Warming

    Ping Zhao;Song Yang;Rucong Yu

  • Climate Effects of the Deep Continental Stratus Clouds Generated by the Tibetan Plateau

    Rucong Yu;Bin Wang;Tianjun Zhou

  • Why Nocturnal Long-Duration Rainfall Presents an Eastward-Delayed Diurnal Phase of Rainfall down the Yangtze River Valley

    Haoming Chen;Rucong Yu;Jian Li;Weihua Yuan

  • Design of a new dynamical core for global atmospheric models based on some efficient numerical methods

    Bin Wang;Hui Wan;Zhongzhen Ji;Xin Zhang

  • Teleconnection between NAO and Climate Downstream of the Tibetan Plateau

    Jian Li;Rucong Yu;Tianjun Zhou

  • Why Is There an Early Spring Cooling Shift Downstream of the Tibetan Plateau

    Jian Li;Rucong Yu;Tianjun Zhou;Bin Wang

  • Seasonal Variation of the Diurnal Cycle of Rainfall in Southern Contiguous China

    Jian Li;Rucong Yu;Tianjun Zhou

  • Tower mast of precipitation over the central Tibetan Plateau summer

    Yunfei Fu;Yunfei Fu;Guosheng Liu;Guoxiong Wu;Rucong Yu

  • Regimes of Diurnal Variation of Summer Rainfall over Subtropical East Asia

    Weihua Yuan;Rucong Yu;Minghua Zhang;Wuyin Lin

  • Impacts of winter‐NAO on March cooling trends over subtropical Eurasia continent in the recent half century

    Rucong Yu;Tianjun Zhou

Frequent Co-Authors

Tianjun Zhou
Tianjun Zhou Chinese Academy of Sciences
Yunfei Fu
Yunfei Fu University of Science and Technology of China
Bin Wang
Bin Wang University of Hawaii at Manoa
Minghua Zhang
Minghua Zhang Stony Brook University
Laurent Li
Laurent Li École Normale Supérieure
Deliang Chen
Deliang Chen Tsinghua University
Peijun Shi
Peijun Shi Beijing Normal University
Guoxiong Wu
Guoxiong Wu Chinese Academy of Sciences
Xuemei Bai
Xuemei Bai Australian National University
Yimin Liu
Yimin Liu Chinese Academy of Sciences

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