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Models of the structure of the atmosphere of Venus from the surface to 100 kilometers altitude
Authors:A Seiff  JT Schofield  AJ Kliore  FW Taylor  SS Limaye  HE Revercomb  LA Sromovsky  VV Kerzhanovich  VI Moroz  MYa Marov
Institution:1. NASA, Ames Research Center, Moffet Field, CA 94035, U.S.A.;2. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, U.S.A.;3. Clarendon Laboratory, Oxford University, Oxford OX1 3PU, U.K.;4. Space Science and Engineering Center, University of Wisconsin —Madison, Madison, WI 53706, U.S.A.;5. Space Research Institute, U.S.S.R. Academy of Sciences, Moscow 117810, U.S.S.R.;6. Institute of Applied Mathematics, U.S.S.R. Academy of Sciences, Moscow 125047, U.S.S.R.
Abstract:From a critical comparison and synthesis of data from the four Pioneer Venus Probes, the Pioneer Venus Orbiter, and the Venera 10, 12, and 13 landers, models of the lower and middle atmosphere of Venus are derived. The models are consistent with the data sets within the measurement uncertainties and established variability of the atmosphere. The models represent the observed variations of state properties with latitude, and preserve the observed static stability. The rationale and the approach used to derive the models are discussed, and the remaining uncertainties are estimated.
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