Conceptual Design of the Lunar Crater Radio Telescope (LCRT) on the Far Side of the Moon

Author(s):  
Saptarshi Bandyopadhyay ◽  
Patrick Mcgarey ◽  
Ashish Goel ◽  
Ramin Rafizadeh ◽  
Melanie Delapierre ◽  
...  
1959 ◽  
Vol 9 ◽  
pp. 13-18 ◽  
Author(s):  
J. S. Hey ◽  
V. A. Hughes

This note describes some of the initial results derived from observations of radar echoes from the moon obtained at 10-cm wavelength at the Royal Radar Establishment, Malvern. The radar, which has been described elsewhere [1], has a transmitter of 2 megawatts peak power with a pulse length of 5 microseconds and a pulse recurrence frequency of 260 per second. The receiver is of conventional design and has a bandwidth of 500 kc/s and a noise factor of 7.5. The aerial used is the 45-foot diameter radio telescope shown in Fig. 1. The telescope is controlled from a mechanical computer that converts the lunar coordinates into azimuth and elevation, which are then fed into a servo drive.


Author(s):  
Saptarshi Bandyopadhyay ◽  
Joseph Lazio ◽  
Adrian Stoica ◽  
Paul Goldsmith ◽  
Brad Blair ◽  
...  
Keyword(s):  

1994 ◽  
Vol 140 ◽  
pp. 154-155
Author(s):  
J. Cernicharo ◽  
W. Brunswig ◽  
G. Paubert ◽  
S. Liechti

VLBI observations show that the SiO maser emitting regions in oxygen-rich stars are very clumpy and that these clumps extend over a few stellar radii (Mclntosh et al. 1987; Colomer et al. 1992). These observations indicate that the ideal instrument for the study of the SiO masers is an interferometer with baselines covering between a few and several hundreds/thousands km. Such an instrument is so far unavailable.A classical way to get high angular resolution and a full beam synthesis with a single telescope of moderate size is through lunar occultations. This observing technique provides the angular resolution of a single linear antenna several kilometers long. However, at millimeter wavelengths the Fresnel fringes produced by the Moon limb as the source under study is occulted have never been observed. We present here the observation with the 30-m IRAM radio telescope of the v=1 J=2-1 line of SiO during an occultation (and reappearance) of R Leo by the Moon.


Nuncius ◽  
2020 ◽  
Vol 35 (2) ◽  
pp. 300-332
Author(s):  
Louise E. Devoy

Abstract This article traces the story of three amateur astronomers who created relief models to help them depict the changing illumination of certain lunar craters, examples of which can be found in UK museum collections today. English chemist Henry Blunt (1806–1853) adopted the emerging technology of electrotyping to reproduce and distribute his plaster model of the Eratosthenes crater to a wider audience. Scottish industrial engineer James Nasmyth (1808–1890) used a combination of drawing, modelling and photography to support his thesis on the volcanic origin of lunar craters in his popular book The Moon Considered … (1874). Spanish sculptor Dionis Renart (1878–1946) produced a series of plaster models for the Exposición General De Estudios Lunares (1912) that eventually came to Greenwich via the British selenographer Hugh Percy Wilkins (1896–1960). These three case studies provide us with valuable insights into the rationale behind the production, use and distribution of lunar crater models within amateur and popular astronomy.


Leonardo ◽  
2016 ◽  
Vol 49 (5) ◽  
pp. 438-439 ◽  
Author(s):  
Daniela de Paulis

OPTICKS is an art project realized by interdisciplinary artist Daniela de Paulis, in collaboration with the CAMRAS radio amateur association based at the Dwingeloo radio telescope in The Netherlands. The project is presented as a live audio-visual performance during which digital images are transmitted as radio signals to the Moon from a radio station in Brazil, the U.K., Switzerland, Poland or Italy. The signals reflected by the Moon’s surface are received by the Dwingeloo radio telescope, converted back into the original images and projected live at an exhibition venue. The project uses Visual Moonbounce, an application of the Moonbounce technology, developed by the artist in collaboration with the CAMRAS team during her residency at the Dwingeloo radio telescope.


2020 ◽  
Vol 494 (3) ◽  
pp. 3464-3468
Author(s):  
J I Katz

ABSTRACT Does the Galaxy contain sources of micro-fast radio burst (FRB), lower energy events resembling the known FRB but detectable only at Galactic distances? The answer to this question is essential to determining the nature of FRB sources. At typical (10 kpc) Galactic distances a burst would be about 117 dB brighter than at a ‘cosmological’ (z = 1) distance. The radiation of Galactic micro-FRB, if they exist, could be detected after Lunar reflection, or an upper bound on their rate set, by a modest (20 m at 1.4 GHz) radio telescope staring at the Moon. It would have all-sky sensitivity. The delay between detection of direct (by STARE2 or dipoles) and Lunar-scattered radiation would restrict a burst’s position to a narrow arc.


This paper gives an account of the radar observations of the Russian earth satellites I and II and of the carrier rocket of satellite I, which have been made with the 250 ft. radio telescope at the Jodrell Bank Experimental Station. When the first satellite was launched on 4 October 1957, the radio telescope was still in an incomplete state. The instrument had already been tested in early August on the reception of the extragalactic radio emissions, but had never been used as a radar instrument. Emergency arrangements were made to connect it with the existing radar installations working in other parts of the establishment. By the night of 9 October the equipment was available for testing and with the telescope in auto­matic motion on the moon satisfactory lunar echoes were obtained. The first radar contacts with the rocket and satellite were obtained during the evening of 11 Octo­ber. The present paper is confined to a discussion of the results up to the date of burn-up of the carrier rocket of satellite I on 1 December 1957 2. Equipment The essential features of the radio telescope have been described by Lovell (1956, 1957 a ). On the frequencies used in the present work (36 and 120 Mc/s) the calculated beam widths and power gains are 8° to half power and 600 on 36 Mc/s, and 2.5° to half power and 6500 on 120 Mc/s. These values have not yet been established by experiment, but the equivalent measured values on frequencies of 160 and 408 Mc/s are very close to the calculated figures. Hence, it is unlikely that the values quoted for 36 and 120 Mc/s are in error. On each frequency the primary feed was a dipole with reflector, mounted at the focal point so that there was cross-polarization between the two feeds.


2021 ◽  
Author(s):  
Kathleen Mandt ◽  
Olivier Mousis ◽  
Dana Hurley ◽  
Alexis Bouquet ◽  
Kurt Retherford ◽  
...  

Abstract Returning humans to the Moon presents an unprecedented opportunity to determine the origin of volatiles stored in the permanently shaded regions (PSRs), which trace the history of lunar volcanic activity, solar wind surface chemistry, and volatile delivery to the Earth and Moon through impacts of comets, asteroids, and micrometeoroids. So far, the source of the volatiles sampled by the Lunar Crater Observation and Sensing Satellite (LCROSS) plume (1, 2) has remained undetermined. We show here that the source could not be volcanic outgassing and the composition is best explained by cometary impacts. Ruling out a volcanic source means that volatiles in the top 1–3 meters of the Cabeus PSR regolith may be younger than the latest volcanic outgassing event (~ 1 billion years ago; Gya) (3).


1962 ◽  
Vol 14 ◽  
pp. 469-471 ◽  
Author(s):  
William M. Sinton

Shorthill, Borough, and Conley discovered during the total eclipse of the Moon on 13 March 1960 that the floor of the crater Tycho did not cool as much as the surrounding area, but remained some 40 to 60° warmer [1]. They found that other rayed craters, specifically Copernicus and Aristarchus, also remained warmer than their surroundings.


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