Engineering Papers⌕ Search

Engineering topics

Mccormick, M. P.

Publications and source records attributed to Mccormick, M. P..

180 records · Page 10
All sourcesNASA NTRSDOE OSTI
NASA NTRS1978

Post-volcanic stratospheric aerosol decay as measured by lidar

The paper summarizes and discusses results of lidar observations, at Hampton (Virginia), of the stratospheric aerosol vertical distribution for a period of 22 months (October 1974 to July 1976) after the volcanic eruption of the Volcan de Fuego in Guatemala. Data are presented in terms of lidar scattering ratio, vertically integrated aerosol backscattering, layer structure and location, and rawinsonde temperature profiles as a function of time. The results reveal a sudden increase in the stratospheric aerosol content after the volcanic eruption as well as its subsequent decline. There exists a high degree of correlation between the integrated aerosol backscattering and the tropopause height such that as one decreases the other increases and vice versa. Rapid decay of the stratospheric aerosol is found to occur over the late winter to early spring period.

Mccormick, M. P.↗
NASA NTRS1978

SAM-2 ground-truth plan: Correlative measurements for the Stratospheric Aerosol Measurement-2 (SAM 2) sensor on the Nimbus G satellite

The SAM-2 will fly aboard the Nimbus-G satellite for launch in the fall of 1978 and measure stratospheric vertical profiles of aerosol extinction in high latitude bands. The plan gives details of the location and times for the simultaneous satellite/correlative measurements for the nominal launch time, the rationale and choice of the correlative sensors, their characteristics and expected accuracies, and the conversion of their data to extinction profiles. The SAM-2 expected instrument performance and data inversion results are presented. Various atmospheric models representative of polar stratospheric aerosols are used in the SAM-2 and correlative sensor analyses.

Russell, P. B.↗
NASA NTRS1977

The use of lidar for stratospheric measurements

Stratospheric measurements possible with ground-based, airborne, and satellite-borne lidar systems are reviewed. The instruments, basic equations, and formats normally used for various scattering and absorption phenomena measurements are presented including a discussion of elastic, resonance, Raman, and fluorescence scattering techniques.

Mccormick, M. P.↗
NASA NTRS1977

The use of lidar for stratospheric measurements

This paper reviews stratospheric measurements possible with ground-based, airborne, and satellite-borne lidar systems. The instruments, basic equations, and formats normally used for various scattering and absorption phenomena measurements are presented including a discussion of elastic, resonance, Raman, and fluorescence scattering techniques.

Mccormick, M. P.↗
NASA NTRS1976

Stratospheric aerosol measurement experiment MA-007

The Apollo Soyuz Test Project Stratospheric Aerosol Measurement Experiment was flown to demonstrate that direct solar occultation measurements by photometers and photographs can be used for defining stratospheric aerosol concentrations. Supporting ground truth data were provided by laser radar and balloon borne dustsonde. Initial results show a significant difference in aerosol concentrations between the Northern and Southern Hemispheres.

Pepin, T. J.↗
NASA NTRS1975

Mission analysis for satellite measurements of stratospheric constituents by solar occultation

Orbital characteristics and launch vehicle requirements for a solar occultation experiment measuring atmospheric constituents, such as aerosols or ozone, during the Nimbus-G and Applications Explorer Missions are analyzed. The experiment to be flown is basically a sun photometer which measures the spectral attenuation of solar radiation by the earth's atmosphere during spacecraft sunrise and sunset, yielding two aerosol and/or ozone stratospheric profiles per orbit. The tangent latitudes and longitudes as well as frequency of these measurements are analyzed for various spacecraft orbits to define maximum geographical coverage capability. Results indicate that a 50 deg inclined orbit for Applications Explorer provides latitude coverage from approximately 70 deg north to 70 deg south every 2-1/2 weeks. A high-moon, sun-synchronous orbit with an inclination of 99 deg for Nimbus-G will provide for coverage of occultation measurements at high latitudes near the polar regions (i.e., 64 to 80 deg north and south). The solar pointing requirements of the experiment in terms of yaw and pitch angles are also defined.

Harrison, E. F.↗
NASA NTRS1975

Lidar measurements of two intense stratospheric dust layers

Lidar measurements were made of two stratospheric dust layers on November 26, 1974, using the NASA 48-inch laser radar system. The dust was probably of volcanic origin. The measurements, made at a wavelength of 0.6943 micron, indicated a 6-km thick layer centered at an altitude of 16 km, and a 1.5-km thick layer centered at 20.25 km. The abnormal scattering ratios, scattering functions, and particle concentrations were evaluated. Measurements made on November 28 showed that both layers had considerably diminished.

Mccormick, M. P.↗
NASA NTRS1974

Dustsonde and lidar measurements of stratospheric aerosols - A comparison

Comparison of lidar and in situ measurements of stratospheric aerosol profiles obtained by backscattered ruby laser light and by direct in situ sampling over Laramie, Wyoming, on two nights in mid-September 1972. The lidar backscattering and the particle number density profiles correlated well. Based on these initial comparative experiments, the ground-based lidar coupled with temperature soundings appears to be a possible method for determining the relative aerosol profile under given stratospheric loading conditions.

Northam, G. B.↗
NASA NTRS1974

The use of lidar for atmospheric measurements

The present work discusses basic lidar theory and the analysis of lidar return signals in tropospheric and stratospheric measurements. An example of the determination of water vapor mixing height through aerosol and molecular scattering functions is given.

Mccormick, M. P.↗
NASA NTRS1972

Mixing-height measurement by lidar, particle counter, and rawinsonde in the Williamette Valley, Oregon

The feasibility of using laser radar (lidar) to measure the spatial distribution of aerosols and water vapor in the earth's mixing or boundary layer is shown. From these data the important parameter of actual mixing height was determined, that is, the maximum height to which particulate pollutants actually mix. Data are shown for simultaneous lidar, rawinsonde, and aircraft-mounted condensation nuclei counter and temperature measurements. The synoptic meteorology is also presented. The Williamette Valley, Oregon, was chosen for the measurements because of its unique combination of meteorology, terrain, and pollutant source, along with an ongoing Oregon State University study of the natural ventilation of this valley.

Mccormick, M. P.↗
NASA NTRS1972

Mie scattering by three polydispersions.

Review of the results of aerosol scattering calculations using models representative of the atmospheric aerosol for three laser wavelengths and two kinds of materials. These calculations show that measurements of scattering and polarization parameters can help significantly in characterizing the earth's aerosol.

Harris, F. S., Jr.↗
NASA NTRS1971

Lidar applications to pollution studies.

This paper discusses the application of lidar (laser radar) to the measurement of air pollution. Lidar techniques and instrumentation utilizing elastic, Raman, and fluorescence scattering are discussed. Data showing measurements of the mixing of particulate pollutants in the atmosphere are presented. These data include: simultaneous two-wavelength results, isopleths showing the temporal dynamics of particulate mixing, measurements of the top of the earth's mixing layer, and measurements in a valley with restricted circulation and mixing. All measurements are compared with simultaneous radiosonde and/or aircraft-mounted temperature probe support. In addition, a second generation lidar system presently under development is described.

Mccormick, M. P.↗
NASA NTRS1968

Optical radar studies of the atmosphere.

Optical radar studies of lower atmosphere, giving Mie theory calculations of clear atmosphere volume backscattering cross sections for four laser wavelengths

Lawrence, J. D., Jr.↗