A double monochromator for the extreme ultraviolet.
Optical design of double monochromator for use in EUV, describing astigmatism and transmission properties
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Optical design of double monochromator for use in EUV, describing astigmatism and transmission properties
Javelin rocket measurements of ultraviolet radiation in airglow
Photoelectric emission properties of iron, copper, nickel, aluminum, and molybdenum
Solar active regions in chromosphere and corona observed by EUV spectroheliometer aboard OSO-4 spacecraft, discussing ion formation and temperatures
EUV solar spectrometer in orbiting solar observatory /OSO-1/, describing satellite, optics and detector, data coding, etc
OSO far UV solar spectroheliograms atlas, describing instrumentation, data aquisition, etc
Oso-4 far UV observations of solar chromosphere and corona active regions
Solar UV radiation measurements by OSO-3, obtaining flux variation over solar rotation period
Paraterphenyl coated photomultiplier as detector in far UV spectra, detailing efficiency range and sensitivity
High intensity ultraviolet radiation source was developed which is suitable for emission below 500 A. Source, useful for 100 to 1000 A range, is simple and inexpensive to construct, easy to operate, and very stable. Because of sufficiently intense output spectrum, source can be used with monochromator at wavelengths as low as 160 A.
Properties of solar-flare EUV flashes are described as inferred from ionospheric events called sudden frequency deviation (SFD). SFD's are sensitive to bursts of radiation in the 1-1030 A wavelength range. He II 303.8 A, O V 629.7 A, H L-gamma 972.5 A and C III 977.0 A have essentially the same impulsive time dependence as the 1-1030 A flash responsible for SFD's. Soft X-rays (2-20 A) and certain EUV lines have a much slower time dependence than the 1-1030 A flash. Most SFD's have some fine structure, but marked quasi-periodicity in EUV flashes is quite rare. EUV flashes are closely associated with hard X-ray bursts, white-light emission, microwave radio bursts and small bright impulsive kernels in the H-alpha flare. The intensity of EUV flashes depends on the central meridian distance of the H-alpha flare location; the intensity decreases at the limb.
Observation of a flare surge at the limb in C III 977 A by the Harvard OSO 6 spectroheliometer. The kinematic behavior of the surge is the same in C III and in H alpha. The amount of C III emission is consistent with a model in which the C III ions occupy sheaths with a thickness of about 100 km surrounding the cooler H alpha-emitting threads. The mass of the material containing C III ions is about 0.01 times that emitting H alpha.
Five new aluminum lines in the region from 35 to 50 A have been produced by focusing the radiation of a 460-MW, Q-spoiled ruby laser on an aluminum target. Characteristics of the new lines, including their observed and predicted wavelength, intensity, and transition, are tabulated.
Identifications and classifications of spectral lines in the lithium-like spectra of the elements K through Mn is presented for the first time. The extrapolation procedures used to calculate these spectra are presented in detail. The excellent agreement between the predicted and measured lines establish the long-range extrapolation.
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A description is given of the results of an analysis of EUV observations of a large coronal hole observed by the Harvard College Observatory (HCO) experiment on OSO-4 in 1967, November. Models were constructed for the chromospheric-coronal transition and coronal layers of the two types of regions. A comparison of the model of the hole and the normal quiet sun indicates that the electron pressure in the hole is reduced by a factor of three and the coronal temperature is lower by 600,000 K.
Two ultraviolet photometers were flown on a Javelin sounding rocket launched from Fort Churchill, Canada, on February 18, 1970, into a weak auroral breakup. The photometers covered the wavelength bands 300-1000 A and 1050-1500 A and observed the aurora while the rocket was above the emitting regions. The observed radiations were found to originate from the visible and X-ray auroral forms recorded by ground-based all-sky cameras and onboard gas proportional X-ray counters. The intensities in the 1050- to 1500-A band were compatible with previous experimental data and available theoretical intensity calculations.