W. D. Smythe
About
In The Last Decade
W. D. Smythe
118 papers receiving 3.2k citations
Peers
Comparison fields: 5 of 105
- Astronomy and Astrophysics 2.6k
- Atmospheric Science 953
- Ecology 607
- Geophysics 390
- Global and Planetary Change 375
Countries citing papers authored by W. D. Smythe
This map shows the geographic impact of W. D. Smythe's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by W. D. Smythe with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites W. D. Smythe more than expected).
Fields of papers citing papers by W. D. Smythe
This network shows the impact of papers produced by W. D. Smythe. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by W. D. Smythe. The network helps show where W. D. Smythe may publish in the future.
Co-authorship network of co-authors of W. D. Smythe
This figure shows the co-authorship network connecting the top 25 collaborators of W. D. Smythe. A scholar is included among the top collaborators of W. D. Smythe based on the total number of citations received by their joint publications. Widths of edges represent the number of papers authors have co-authored together. Node borders signify the number of papers an author published with W. D. Smythe. W. D. Smythe is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Anhydrous Ammonia Frost on Titan | 1 |
| 2 | Validity of Regolith Reflectance Models Based on the Radiative Transfer Equation and Coherent Backscatter Theory | 1 |
| 3 | Size-dependent Measurements of the Scattering Properties of Planetary Regolith Analogs: A Challenge to Theory | 5 |
| 4 | Io Science Opportunities From the JIMO Mission | 1 |
| 5 | Evidence for a topographically controlled sulfur dioxide deposit at Chaac caldera, Io | 1 |
| 6 | 108 | |
| 7 | The Coherent Backscattering Opposition Effect: Search for Wavelength Dependent Changes in the Shape of the Phase Curve | 2 |
| 8 | Evidence for Massive Sulfur Dioxide Deposit on Io | 8 |
| 9 | The Opposition Effect in Simulated Planetary Regoliths: Circular and Linear Polarization Ratio Change with Phase Angle | 1 |
| 10 | Deconvolution of Galileo NIMS Day-Side Spectra of Io into Thermal, SO2, and Non-SO2 Components | 5 |
| 11 | The Temporal Activity of Io's Hot Spots | 2 |
| 12 | Absorption Bands in the Spectrum of Europa Detected by the Galileo NIMS Instrument | 12 |
| 13 | Galileo Remote Sensing Compositional Studies of the Tyre Region of Europa | 3 |
| 14 | Coherent Backscatter in Particulate Materials: Variation of the Circular Polarization Ratio with Particle Size and Phase Angle | 2 |
| 15 | Monitoring of Io's Volcanic Activity Using Galileo's Near Infrared Mapping Spectrometer (NIMS) | 2 |
| 16 | A Synergistic Imaging Spectroscopy View of 951 Gaspra | 2 |
| 17 | The Opposition Effect of the Moon: Coherent Backscatter | 1 |
| 18 | Laboratory Study of the Opposition Effect | 1 |
| 19 | The detectability of clathrate hydrates in the outer solar system | 4 |
| 20 | Spectra of Possible Galilean Satellite Materials: T and d Effects. | 1 |
Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive bibliographic database. While OpenAlex provides broad and valuable coverage of the global research landscape, it—like all bibliographic datasets—has inherent limitations. These include incomplete records, variations in author disambiguation, differences in journal indexing, and delays in data updates. As a result, some metrics and network relationships displayed in Rankless may not fully capture the entirety of a scholar's output or impact.