James B. Pollack
About
In The Last Decade
James B. Pollack
306 papers receiving 18.5k citations
Hit Papers
Peers
Comparison fields: 5 of 166
- Astronomy and Astrophysics 15.6k
- Atmospheric Science 6.9k
- Global and Planetary Change 4.7k
- Aerospace Engineering 2.2k
- Earth-Surface Processes 1.6k
Countries citing papers authored by James B. Pollack
This map shows the geographic impact of James B. Pollack'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 James B. Pollack with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites James B. Pollack more than expected).
Fields of papers citing papers by James B. Pollack
This network shows the impact of papers produced by James B. Pollack. 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 James B. Pollack. The network helps show where James B. Pollack may publish in the future.
Co-authorship network of co-authors of James B. Pollack
This figure shows the co-authorship network connecting the top 25 collaborators of James B. Pollack. A scholar is included among the top collaborators of James B. Pollack 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 James B. Pollack. James B. Pollack is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Impact of the CO2 and H2O clouds of the Martian polar hood on the polar energy balance | 1 |
| 2 | The H 2 O Abundance in the Lower Atmosphere of Venus from NIMS-Galileo | 1 |
| 3 | Simulations of the Seasonal Pressure Changes on Mars with a General Circulation Model | 1 |
| 4 | Saltation thresholds and entrainment of fine particles at Earth and Martian pressures | 5 |
| 5 | Diurnal variations in optical depth at Mars: Observations and interpretations | 4 |
| 6 | Origin and evolution of the Saturn system | 14 |
| 7 | Venus aeolian processes: saltation studies and the Venusian wind tunnel. | 3 |
| 8 | An Origin by Capture for the Martian Satellites | 24 |
| 9 | Climatic change on Mars: inferences based on Viking and Mariner data. | 1 |
| 10 | 79 | |
| 11 | Physical Properties of the Particles Composing the Great Martian Dust Storm of 1971 | 4 |
| 12 | Estimates of the Minimum Wind Needed to Raise Dust on Mars | 1 |
| 13 | Models of temperature structure and general circulation | 2 |
| 14 | Simulations of Martian Eolian Phenomena in the Atmospheric Wind Tunnel | 16 |
| 15 | High Altitude Aircraft Infrared Spectrometric Observations of Water of Hydration on Mars | 1 |
| 16 | A reexamination of the stability of goethite on Mars. | 2 |
| 17 | Goethite on Mars: a Laboratory Study of Physically and Chemically Bound Water in Ferric Oxides | 1 |
| 18 | Elevation differences on Mars. | 1 |
| 19 | A Windblown Dust Model of Martian Surface Features and Seasonal Changes. | 9 |
| 20 | Radar Doppler Spectroscopy of Mars. I. Elevation Differences Between Bright and Dark Areas | 2 |
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.