E. F. Tedesco

ORCID: 0000-0001-5907-3245
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About
Contact & Profiles
Research Areas
  • Astro and Planetary Science
  • Planetary Science and Exploration
  • Isotope Analysis in Ecology
  • Stellar, planetary, and galactic studies
  • Astronomical Observations and Instrumentation
  • Astronomy and Astrophysical Research
  • Space Exploration and Technology
  • Astronomical and nuclear sciences
  • Space Satellite Systems and Control
  • Spacecraft and Cryogenic Technologies
  • History and Developments in Astronomy
  • Calibration and Measurement Techniques
  • Geology and Paleoclimatology Research
  • Geological and Geochemical Analysis
  • Astrophysics and Star Formation Studies
  • Adaptive optics and wavefront sensing
  • Gamma-ray bursts and supernovae
  • Solar and Space Plasma Dynamics
  • High-pressure geophysics and materials
  • Geophysics and Gravity Measurements
  • Historical Astronomy and Related Studies
  • Nuclear Physics and Applications
  • Laser-induced spectroscopy and plasma
  • Spacecraft Design and Technology
  • Atmospheric Ozone and Climate

Planetary Science Institute
1982-2020

Centre Hospitalier Universitaire de Saint-Étienne
2013

California Institute of Technology
1984-2008

Jet Propulsion Laboratory
1982-2008

University of New Hampshire
2004-2007

University of New Hampshire at Manchester
2004-2006

Terra
2005

University of Hawaiʻi at Mānoa
1995

University of Hawaii System
1994-1995

Space Information Laboratories (United States)
1989

We present additional and revised IRAS diameters albedos for the 1992 Minor Planet Survey (IMPS). Using orbital elements 26,791 numbered asteroids, we found 2228 different multiply observed asteroids associated with sources, an increase of 432 (24%) over IMPS. The sample small D < 20.0 km, has increased by 72% (from 306 to 526), Jupiter Trojan 77% 39 69), (D 80 km) nearly a factor 3 nine 26). entire Supplemental data set, describe how it was created, compare IMPS estimate many more remain be in data.

10.1086/338320 article EN The Astronomical Journal 2002-02-01

Every three years the IAU/IAG Working Group on Cartographic Coordinates and Rotational Elements revises tables giving directions of poles rotation prime meridians planets, satellites, minor comets. This report introduces improved values for pole rate Pluto, Charon, Phoebe, Jupiter, sizes shapes Saturn satellites poles, rates, some planets A high precision realization Moon is provided. The expression Sun's has been changed to be consistent with account light travel time

10.1007/s10569-007-9072-y article EN cc-by-nc Celestial Mechanics and Dynamical Astronomy 2007-07-01

Infrared photometry is reported for 22 Aten, Apollo, and Amor asteroids. Thermal models are used to derive the corresponding radiometric albedos diameters. Several of these asteroids appear have surfaces relatively high thermal inertia due exposure bare rock or a coarse regolith. The Apollo asteroid 3103, 1982 BB, recognized as class E. Jupiter-crossing 3552, 1983 SA, confirmed D, but low remain rare near-earth

10.1086/115064 article EN The Astronomical Journal 1989-04-01

Broadband U, V, and x photometry together with IRAS asteroid albedos have been used to construct an classification system. The system is based on three parameters (U-V v-x color indices visual geometric albedo), it able place 96 percent of the present sample 357 asteroids into 11 taxonomic classes. It noted that all but one these classes are analogous those previously found using other schemes. algorithm shown account for observational uncertainties in each parameters.

10.1086/115007 article EN The Astronomical Journal 1989-02-01

This chapter describes the contents and organization of IRAS Minor Planet Survey Data Base tells how to obtain hard-copy machine-readable versions data.

10.1017/s0074180900046726 article EN Symposium - International Astronomical Union 1994-01-01

We present a new extensive analysis of the old problem finding satisfactory calibration relation between geometric albedo and some measurable polarization properties asteroids. To achieve our goals, we use all polarimetric data at disposal. For purposes calibration, limited sample objects for which can be confident to know with good accuracy, according previous investigations other authors. find set updated coefficients classical slope–albedo relation, but generalize consider also...

10.1093/mnras/stv1188 article EN Monthly Notices of the Royal Astronomical Society 2015-06-25

Compositionally diagnostic information regarding the spectral reflectance of faint asteroids and planetary satellites, obtained using a photometric system, is presented. Standard UBV range in effective wavelength from 0.34 to 1.04 microns are among eight broadband filters relative study. An InGaAsP photomultiplier high quantum efficiencies employed for longer wavelengths, allows work magnitude 17 fainter when used conjunction with 2 m telescope. Magnitudes color indices mean uncertainty + or...

10.1086/113248 article EN The Astronomical Journal 1982-11-01

We describe the creation of a model main asteroid belt whose purpose is to main-belt size frequency distribution and simulate number asteroids their fluxes at visual through mid-infrared (∼0.3–70 μm) wavelengths in any area sky for an arbitrary date. This based on population ∼1.9 × 106 obtained from complete known sample, plus extrapolation size-frequency distributions 15 dynamical families three background populations, diameter limit 1 km. The compared with data other models, example...

10.1086/429734 article EN The Astronomical Journal 2005-05-20

Abstract— We present Markov‐Chain Monte‐Carlo methods (MCMC) for the derivation of empirical model parameters photometric and polarimetric phase curves asteroids. Here we two jointly at angles ≤25° using a linear‐exponential model, accounting opposition effect in disk‐integrated brightness negative branch degree linear polarization. apply MCMC to V‐band asteroids 419 Aurelia (taxonomic class F), 24 Themis (C), 1 Ceres (G), 20 Massalia (S), 55 Pandora (M), 64 Angelina (E). show that can be...

10.1111/j.1945-5100.2009.tb02003.x article EN Meteoritics and Planetary Science 2009-12-01
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