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Gross, S. H.

Publications and source records attributed to Gross, S. H..

33 records · Page 2
All sourcesNASA NTRSDOE OSTI
NASA NTRS1974

Winds and the occultation experiment

A spacecraft orbiting about another planet, such as Mars or Venus, may be used to obtain data about the pressure, density, and temperature fields over the planet from multiple occultations if the orbit precesses or retrogresses. Under certain conditions successive occultations will provide mean dynamic information such as wind speeds over the time and spacing intervals. It is shown that data concerning winds may be found by comparing refractivity information rather than pressure or temperature.

Gross, S. H.↗
NASA NTRS1973

A study of the evolution of the atmosphere of Venus

The escape mechanism was studied which results in blow-off of an atmosphere. The planets and satellites were investigated in this respect from an evolutionary standpoint along with comets and the solar wind because of similarities. Both static and dynamic studies were made of upper atmospheric regions for neutral and for fully ionized media. It was found that variation with more than one dimension is essential.

Gross, S. H.↗
NASA NTRS1972

Errors incurred in profile reconstruction and methods for increasing inversion accuracies for occultation type measurements

A method for augmenting the occultation experiment is described for slightly refractive media. This method which permits separation of the components of the gradient of refractivity, appears applicable to most of the planets for a major portion of their atmospheres and ionospheres. The analytic theory is given, and the results of numerical tests with a radially and angularly varying model of an ionosphere are discussed.

Gross, S. H.↗
NASA NTRS1972

The evolution of water vapor in the atmosphere of Venus.

Examination of the feasibility of loss of water vapor from the Venus atmosphere, assuming H2O as the sole initial constituent. A steady-state model is constructed, and the photochemistry establishes the distribution of important products in the upper atmosphere. Calculations of exospheric temperatures yield values as high as 100,000 K. Such large temperatures result from the large abundance of atomic hydrogen in the exosphere, and imply a dynamic outflow of all constituents from the upper region of the atmosphere. Such an outflow would cause the escape of all hydrogen and some of the oxygen resulting from dissociation of H2O. Little loss of CO2 would result, due to its low abundance in the upper region, permitting its accumulation to the present observed value. It is concluded that if Venus formed from the same mix of materials as the earth, much tectonic activity and fairly rapid outgassing must have occurred during the early phase of its history to account for the loss of water vapor.

Smith, L. L.↗
NASA NTRS1972

On the exospheric temperature of hydrogen-dominated planetary atmospheres.

Results of studies of hydrogen-dominated atmospheres in which exospheric temperatures were calculated to estimate the evaporative loss rates of the constituents. Expressions are given for the exospheric temperature of a two-component diffusive equilibrium model which consists of a lighter molecule dominating the thermosphere and absorbing solar EUV, and a heavier constituent providing radiative cooling in the vicinity of the mesopause. The model approximates well the assumed atmospheres, but the resulting expressions may have wider application. The dynamics of an expanding atmosphere are discussed. A three-dimensional outflow against the back pressure of the solar wind may be configured like a comet's tail.

Gross, S. H.↗
NASA NTRS1966

The atmosphere of Mercury.

Mercury atmospheric temperature, composition and surface pressure and effect of nonsynchronous rotation

PLANETARY ATMOSPHERE↗
NASA NTRS1966

Mars - Upper atmosphere.

Mars upper atmosphere thermal structure from spectroscopic measurements and Mariner IV OCCULTATION experiment

ATMOSPHERIC TEMPERATURE↗
NASA NTRS1964

The upper atmosphere of jupiter.

Jovian upper atmospheric model and calculation of temperature profile, radiation flux and ionospheric structure

RADIATION EMISSION↗