P
Paul B. Hays
Researcher at University of Michigan
Publications - 199
Citations - 10639
Paul B. Hays is an academic researcher from University of Michigan. The author has contributed to research in topics: Thermosphere & Airglow. The author has an hindex of 55, co-authored 199 publications receiving 10149 citations. Previous affiliations of Paul B. Hays include Goddard Space Flight Center.
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Journal ArticleDOI
A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature
TL;DR: In this article, it is suggested that the partial pressure of carbon dioxide in the atmosphere is buffered, over geological time scales, by a negative feedback mechanism, in which the rate of weathering of silicate minerals (followed by deposition of carbonate minerals) depends on surface temperature, which in turn depends on the carbon dioxide partial pressure through the greenhouse effect.
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An empirical model of the Earth's horizontal wind fields: HWM07
Douglas P. Drob,J. T. Emmert,Geoff Crowley,J. M. Picone,Gordon G. Shepherd,Wilbert R. Skinner,Paul B. Hays,Rick J. Niciejewski,Miguel Larsen,Chiao-Yao She,John W. Meriwether,G. Hernandez,Martin J. Jarvis,D. P. Sipler,Craig A. Tepley,M. S. O'Brien,J. R. Bowman,Qian Wu,Yasuhiro Murayama,Seiji Kawamura,Iain M. Reid,Robert A. Vincent +21 more
TL;DR: The Horizontal Wind Model (HWM07) as mentioned in this paper provides a statistical representation of the horizontal wind fields of the Earth's atmosphere from the ground to the exosphere (0-500 km).
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The high-resolution Doppler imager on the Upper Atmosphere Research Satellite
Paul B. Hays,Vincent J. Abreu,Michael E. Dobbs,David A. Gell,Heinz J. Grassl,Wilbert R. Skinner +5 more
TL;DR: The high-resolution Doppler imager (HRDI) on the Upper Atmosphere Research Satellite is a triple-etalon Fabry-Perot interferometer designed to measure winds in the stratosphere, mesosphere, and lower thermosphere.
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The auroral 6300 Å emission: Observations and modeling
TL;DR: In this article, a tomographic inversion is used to analyze measurements of the auroral atomic oxygen emission line at 6300 A made by the atmosphere explorer visible airglow experiment.
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Long-term variability in the solar diurnal tide observed by HRDI and simulated by the GSWM
TL;DR: The global scale wave model (GSWM) as mentioned in this paper represents the first numerical modeling attempt at simulating this seasonal variability, and a preliminary comparison of the GSWM tidal results with HRDI measurements is presented.