J. Röttger
About
In The Last Decade
J. Röttger
176 papers receiving 3.2k citations
Peers
Comparison fields: 5 of 40
- Astronomy and Astrophysics 3.4k
- Atmospheric Science 2.0k
- Geophysics 863
- Aerospace Engineering 806
- Oceanography 792
Countries citing papers authored by J. Röttger
This map shows the geographic impact of J. Röttger'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 J. Röttger with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites J. Röttger more than expected).
Fields of papers citing papers by J. Röttger
This network shows the impact of papers produced by J. Röttger. 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 J. Röttger. The network helps show where J. Röttger may publish in the future.
Co-authorship network of co-authors of J. Röttger
This figure shows the co-authorship network connecting the top 25 collaborators of J. Röttger. A scholar is included among the top collaborators of J. Röttger 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 J. Röttger. J. Röttger is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | Horizontal wavelength of gravity waves in the lower atmosphere measured by the SOUSY Svalbard Radar | 4 |
| 2 | Observations of the Arctic troposphere and lower stratosphere with the SOUSY Svalbard Radar | 1 |
| 3 | 6 | |
| 4 | Polar Mesosphere Summer Echoes: Dynamics and aeronomy of the mesosphere | 3 |
| 5 | Creation of artificial periodic inhomogeneities for studies of the middle atmosphere and lower thermosphere | 2 |
| 6 | EISCAT stratosphere-troposphere experiment performance | 1 |
| 7 | The new ionospheric backscatter system of the Chung-Li VHF radar: Basic design and some first results | 1 |
| 8 | Plans for the EISCAT Svalbard Radar | 1 |
| 9 | On the use of colour reflectivity plots to monitor the structure of the troposphere and stratosphere | 1 |
| 10 | Observations of mesoscale vertical velocities around frontal zones | 1 |
| 11 | A comparison of thunderstorm reflectivities measured at VHF and UHF | 2 |
| 12 | UHF and VHF radar observations of thunderstorms | 2 |
| 13 | Investigations of the lower and middle atmosphere at the Arecibo Observatory and a description of the new VHF radar project | 2 |
| 14 | The use of the experimentally deduced Brunt-Väisälä frequency and turbulent velocity fluctuations to estimate the eddy diffusion coefficient | 2 |
| 15 | A cooperative synchronous observation of winds and tides in the tropical lower stratosphere and mesosphere using VHF radars at Jicamarca and Arecibo. | 1 |
| 16 | Comparison of reflectivity and wind profiles measured on 46.8 MHz and 430 MHz at the Arecibo Observatory | 1 |
| 17 | Determination of the Brunt-Väisälä frequency from vertical velocity spectra | 9 |
| 18 | The capabilities of VHF radars for meteorological observations | 4 |
| 19 | VHF-radar echoes from the troposphere and stratosphere | 2 |
| 20 | Einflüße des äquatorialen Spread-F auf die Kurzwellenausbreitung | 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.