Automated Author ProfileWang, Shuang
Laboratory for Climate and Ocean-Atmosphere Studies, Dept. of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, People's Republic of China0000-0002-9406-1781
Wang, Shuang
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 2.2 (sum of 6 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
The ZIP file contains x–z cross-sections along y=0 for all non-rotating simulations.The remaining files provide y-averaged fields from the rotating simulations, which were used to generate the cross-section figures in the main text.Because the full dataset (including three-dimensional fields) is too large to be archived here, these data are available from the authors upon reasonable request.The two scripts are the Oceananigans scripts for simulating non-rotating (rF) and rotating (rT) plumes in this study.
Authors
- Wang, Shuang
Averaged (along y-axis) buoyancy field for rotating point plumes in XX. Any other large stored data supporting this work are available upon reasonable request. Please contact the corresponding author.
Authors
- Wang, Shuang
Averaged (along y-axis) buoyancy field for rotating point plumes in XX. Any other large stored data supporting this work are available upon reasonable request. Please contact the corresponding author.
Authors
- Wang, Shuang
The ZIP file contains x–z cross-sections along y=0 for all non-rotating simulations.The remaining files provide y-averaged fields from the rotating simulations, which were used to generate the cross-section figures in the main text.Because the full dataset (including three-dimensional fields) is too large to be archived here, these data are available from the authors upon reasonable request.
Authors
- Wang, Shuang
The data are for the article "Lorenz Energy Cycle: Another Way to Understand the Atmospheric Circulation on Tidally Locked Terrestrial Planets". The data are simulated by the general circulation model ExoCAM. The horizontal resolution is 4°x5°. Note: ST: in standard coordinates; TL: in the tidally locked coordinates. The simulation data is daily-mean (i.e., '.daily.nc'), including: ST_5d_tidally_locked.cam.daily.nc, ST_60d_tidally_locked.cam.daily.nc (in the standard coordinates), and TL_60d_tidally_locked.cam.daily.nc (in the tidally locked coordinates). The LEC data are calculated by the LEC code released at https://doi.org/10.5281/zenodo.7472396, including: Earth: LEC_energy.1979-.nc and LEC_converse_rate.1979-*.nc Rapidly rotating tidally locked planet (in standard coordinates): ST_LEC_energy_5d_tidally_locked.nc and ST_LEC_conv-rate_5d_tidally_locked.nc Slowly rotating tidally locked planet (in tidally locked coordinates): TL_LEC_energy_60d_tidally_locked.nc and TL_LEC_conv-rate_60d_tidally_locked.nc Slowly rotating tidally locked planet (in standard coordinates): ST_LEC_energy_60d_tidally_locked.nc and ST_LEC_conv-rate_60d_tidally_locked.nc
Authors
- Wang, Shuang
The data are for the article "Lorenz Energy Cycle: Another Way to Understand the Atmospheric Circulation on Tidally Locked Terrestrial Planets". The data are simulated by the general circulation model ExoCAM. The horizontal resolution is 4°x5°. Note: ST: in standard coordinates; TL: in the tidally locked coordinates. The simulation data is daily-mean (i.e., '.daily.nc'), including: ST_5d_tidally_locked.cam.daily.nc, ST_60d_tidally_locked.cam.daily.nc (in the standard coordinates), and TL_60d_tidally_locked.cam.daily.nc (in the tidally locked coordinates). The LEC data are calculated by the LEC code released at https://doi.org/10.5281/zenodo.7472396, including: Earth: LEC_energy.1979-.nc and LEC_converse_rate.1979-*.nc Rapidly rotating tidally locked planet (in standard coordinates): ST_LEC_energy_5d_tidally_locked.nc and ST_LEC_conv-rate_5d_tidally_locked.nc Slowly rotating tidally locked planet (in tidally locked coordinates): TL_LEC_energy_60d_tidally_locked.nc and TL_LEC_conv-rate_60d_tidally_locked.nc Slowly rotating tidally locked planet (in standard coordinates): ST_LEC_energy_60d_tidally_locked.nc and ST_LEC_conv-rate_60d_tidally_locked.nc
Authors
- Wang, Shuang