Communications of the Lunar and Planetary Laboratory, volume 9, part 3
Galilean satellites, Venus clouds, and astronomical observatories
Kuiper, G. P.↗
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Arizona-nasa Atlas of the Infrared Solar Spectrum, Report 10
The Arizona-NASA Infrared Solar Spectrum Atlas is concluded. The wavelength interval covered is 13350-34100 A.
Benner, D. C.↗
Very long baseline interferometer observations of Taurus A and other sources at 121.6 MHz.
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Erickson, W. C.↗
Comets: Scientific data and missions; Proceedings of the Tucson Comet Conference, University of Arizona, Tucson, Ariz., April 8, 9, 1970.
Current knowledge of comets is surveyed, and comet-rendezvous mission constraints, opportunities, modes, and spacecraft capabilities are discussed. Attention is given to cometary nuclei, infrared measurements of comets, the nature and origin of the cometary head, L-alpha photometry of Comet Bennett, Types I and II tails, comet spectra and orbits, and evidence from stream meteoroids. Some scientific criteria for a cometary mission are considered. Individual items are announced in this issue.
Kuiper, G. P.↗
Water vapor in the atmosphere of Venus.
Infrared spectra of Venus produced by a Fourier spectrometer flown aboard the NASA CV 990 jet aircraft were analyzed for water-vapor content by comparison with calculated model spectra. The reflecting layer model gave an abundance of 1.6 plus or minus 0.4 micron of precipitable water for the two-way transmission of the Venus atmosphere. The scattering model resulted in a value of 0.25 plus or minus 0.10 micron of water per scattering mean free path. Neither is regarded as a definitive model, but derived mixing ratios will not be significantly in error. An abundance of CO2 using a number of bands, was determined for both models. The volume mixing ratios of H2O to CO2 obtained were 0.0000006 and 0.000001 for the reflecting layer and scattering model, respectively.
Fink, U.↗
Detailed correlation of type III radio bursts with H alpha activity. I - Active region of 22 May 1970.
Comparison of observations of type III impulsive radio bursts made at the Clark Lake Radio Observatory with high-spatial-resolution cinematographic observations taken at the Big Bear Solar Observatory. Use of the log-periodic radio interferometer makes it possible to localize the radio emission uniquely. This study concentrates on the particularly active region close to the limb on May 22, 1970. Sixteen of the 17 groups were associated with some H alpha activity, 11 of them with the start of such activity.
Kuiper, T. B. H.↗
Arizona-NASA Atlas of the Infrared Solar Spectrum. X.
Second and last set of the B-spectrometer records, concluding the series of the Arizona-NASA Infrared Solar Spectrum Atlas. The value of the presented series lies primarily in serving as reference to high-altitude planetary spectra taken with similar resolution, 6-10,000. The wavelength interval covered is 13350-34100 A.
Benner, D. C.↗
The Lunar and Planetary Laboratory and its telescopes.
The campus and observatory facilities of the Lunar and Planetary Laboratory at the University of Arizona are described, with particular reference to the Space Sciences Building and its Optical Shop. The Catalina Observatory (located on a peak of the Catalina Mountains, 36 miles from the University) and its facilities intended for planetary photography, near-infrared spectroscopy and interferometry, far-infrared broadband photometry and image scanning, and studies of asteroids, comets, and other stellar studies are discussed. The layout, facilities, and telescopes of the Mount Lemmon Observatory intended for infrared astronomical research are also covered.
Kuiper, G. P.↗
Interpretation of the Jupiter red spot. I.
The LPL research programs on Jupiter include continuing photographic coverage of the planet in color and in several wavelength bands; IR image scans especially around 5 microns; medium and high-resolution spectral studies in the photographic and the lead-sulfide regions, with laboratory comparisons; photometric and polarimetric studies; far-IR measurements at high altitudes; chemical studies designed to match formation of Jovian cloud particles; and participation in the NASA Pioneer missions. Some preliminary interpretative remarks are given which are in part suggested by the remarkable IR spectra and IR images of the earth and Mars obtained at NASA-Goddard. This leads to a discussion of the Red Spot and the White Ovals.
Kuiper, G. P.↗
Communications of the Lunar and Planetary Laboratory, volume 10, part 1
Research reports and observational summaries prepared by the laboratory staff are presented.
Kuiper, G. P.↗
Comments on the Galilean satellites
The surface deposits of the Galilean satellites, especially Io, are examined in the light of some early and some very recent observations. Io, with probably a thin sulfur deposit in the lower latitudes and orange polar caps presumably composed of sulfur compounds, stands apart from the other three satellites.
Kuiper, G. P.↗
High resolution planetary observation
High-resolution ground-based planetary observations, visual and photographic, have, for several decades, seemed to have reached a rather firm limit. The causes for this restriction are briefly reviewed. At the time when space probes make major advances possible, at incomparably higher levels of expenditure, the need arises to re-examine the limiting factors of earth-based planetary resolution. In addition to familiar refinements (of which seven are listed) carried somewhat further, a specific approach, yet insufficiently developed, is the study of the atmospheric boundary layer over the observatory site and the use of an appropriately elevated station.
Kuiper, G. P.↗
Water-vapor measures, Mt. Lemmon area
Daytime atmospheric water-vapor measures were continued for Mt. Lemmon, the Catalina Observatory, and Tucson. As before (LPL Comm. No. 158), the three sets are closely related in terms of their altitude differences, with the average empirically-determined scale-height value, 2.3 km. During the winter and spring of 1971 observations were made for more than 90% of the days. The measures are listed in tables and for comparison, the 1969-70 data published in LPL Communication No. 158 are given. The averages for the stations are also shown.
Kuiper, G. P.↗
On the density of the corona in regions of type 3 activity
The east-west positions of 190 type 3 bursts were measured between 30 and 65 MHz with the log-periodic array at Clark Lake. A method is described to find the intrinsic variation of position with frequency of type 3 bursts based on the comparison of the positions of the bursts measured at any two arbitrary frequencies. It is found that the variation of position frequency agrees with the behaviour expected from coronal density models. This suggests that the measured positions were not seriously affected by scattering in the corona. Knowing the functional form of the variation of position with frequency for type 3 bursts, it is shown that the observed burst positions can be corrected for the effects of ionospheric refraction.
Kuiper, T. B. H.↗
Communications of the Lunar and Planetary Laboratory: Communications nos. 173-183, volume 9, part 5
Short discussions are presented on: (1) multicolor photography of Jupiter; (2) narrow band photography of Jupiter and Saturn; (3) photographic observations of the occulation of Beta Scorpii by Jupiter; (4) development of the June 1971 South Equatorial Belt Disturbance on Jupiter; (5) rotation period for subsurface source in the NNTeB of Jupiter; (6) correlation between color of Jovian clouds and their 5 micron temperatures; (7) and observations of Jupiter's North North Temperature Belt Current B.
Kuiper, G. P.↗
Interpretation of the Jupiter Red Spot, 1
With the aid of 8900 micron CH4 filter photographs it is shown that the Red Spot is normally the highest cloud feature in the Jovian atmosphere, located squarely on the South Tropical Zone at 22 deg. S. The Red Spot is a rising column, obviously having its own energy source; it spreads outward at the top level, in anticyclonic rotation. It is concluded that the large and persistent Jovian cloud masses, of which the Red Spot is the largest, are major organized storm arrays embedded in a near stagnant atmosphere, each probably possessing numerous short-lived rising hot columns driven by released latent heat; and covered by a horizontally-expanding gigantic cirrus cloud system, in anti-cyclonic rotation. The meteorological theory of Organized Cumulus Convection is applied to the Red Spot and the White Ovals. Evidence exists that the array of hot towers under the Red Spot is eccentric. The 90-day and the occassional 5-8 year fluctuations in the motion of the Red Spot may be due to processes analogous to those found in the Earth's Tropical Convergence. The 90-day oscillation has been observed for 8 years.
Kuiper, G. P.↗
The log-periodic array at the Clark Lake Radio Observatory
A log-periodic array, 3 km in length, is operating at Clark Lake Radio Observatory. It makes one-dimensional sweeps of the solar brightness distribution in the frequency range 20 to 65 MHz once per sec. The phasing of the array and the receiving system are described, as well as how the dynamic spectra are analyzed for the positions of solar radio sources. Simultaneous measurements at many frequencies enable the observer to remove the effects of ionospheric refraction and to obtain fundamental positions to an accuracy of about one arc min at decametric wavelengths. Fundamental positions are given for Cassiopeia A.
Erickson, W. C.↗
Water-vapor measures - Mt. Lemmon area
Daytime atmospheric water-vapor measures were continued for Mt. Lemmon, the Catalina Observatory, and Tucson. As before (Lunar and Planetary Laboratory Communications, No. 158), the three sets are closely related in terms of their altitude differences, with the average empirically-determined scale-height value, 2.3 km. During the winter and spring of 1971 observations were made for more than 90% of the days. The measures are tabulated and reduced to Mt. Lemmon. The calibration was continued to higher values by means of atmospheric radiosonde data.
Kuiper, G. P.↗