This map shows the geographic impact of M. W. Pharo'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 M. W. Pharo with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites M. W. Pharo more than expected).
This network shows the impact of papers produced by M. W. Pharo. 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 M. W. Pharo. The network helps show where M. W. Pharo may publish in the future.
Co-authorship network of co-authors of M. W. Pharo
This figure shows the co-authorship network connecting the top 25 collaborators of M. W. Pharo.
A scholar is included among the top collaborators of M. W. Pharo 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 M. W. Pharo. M. W. Pharo is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Brace, L. H., et al.. (1972). The electron heating rate and ion chemistry in the thermosphere above Wallops Island during the solar eclipse of.3 indexed citations
Pharo, M. W., et al.. (1971). Observations of thermospheric ion composition above Wallops Island during the 7 March 1970 solar eclipse. NASA Technical Reports Server (NASA).1 indexed citations
10.
Brinton, H. C., M. W. Pharo, & H. A. Taylor. (1969). Evidence of contraction of the earth's thermal plasmasphere subsequent to the solar flare events of 7 and 9 July 1966.. NASA Technical Reports Server (NASA).4 indexed citations
Mayr, H. G., et al.. (1969). A study of ion composition and chemistry in a quiet, midday, midlatitude F-region from 130 to 306 kilometers. NASA Technical Reports Server (NASA).1 indexed citations
Brinton, H. C., et al.. (1968). A Direct Measurement of Ion Composition and Concentration in the Daytime F2-region. NASA STI Repository (National Aeronautics and Space Administration).3 indexed citations
16.
Brinton, H. C., M. W. Pharo, N. K. Rahman, & H. A. Taylor. (1968). Latitudinal variation of the composition of the topside ionosphere, first results of the OGO-2 ion spectrometer. NASA Technical Reports Server (NASA).6 indexed citations
Brinton, H. C., M. W. Pharo, Charles R. Smith, & H. A. Taylor. (1966). Positive ion composition and density in the lower E-region, from 87 to 114 kilometers. NASA Technical Reports Server (NASA).1 indexed citations
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.