Circulation features of the stratosphere derived from radiometric temperature measurements with Tiros VII satellite.
Stratospheric circulation from Tiros 7 satellite radiometrically derived temperature patterns
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Stratospheric circulation from Tiros 7 satellite radiometrically derived temperature patterns
Evolution of Tiros meteorological satellite operational system noting orbital inclination, solar illumination, data storage ground stations, etc
Evolution of Tiros meteorological satellite operational system noting orbital inclination, solar illumination, data storage ground stations, etc
Tiros satellite microwave measurements together with radiosonde data are used to illustrate a method for deriving vertical temperature distributions in the atmosphere on the scale of 100 km. The method employs N equations in N unknowns. The unknowns are the N coefficients which are needed at each pressure level to multiply the measured N radiances in order to retrieve the vertical temperature distributions. As an example, the spatial variation of the tropopause characteristics is derived over a cyclone. Diurnal variations in the radiances and the consistency of radiosondes and satellite radiance data need further investigation.
Spacecraft and systems design for converting TIROS OT-2 from standard axial camera to wheel mode configuration for use in TIROS operational satellite system
Stratospheric temperature patterns based on radiometric measurements from Tiros VII SATELLITE
Circulation features of stratosphere derived from radiometric temperature measurements with Tiros VII satellite
There is a well-documented requirement for a comprehensive and accurate global moisture data set to assist many important studies in atmospheric science. Currently, atmospheric water vapor measurements are made from a variety of sources including radiosondes, aircraft and surface observations, and in recent years, by various satellite instruments. Creating a global data set from a single measuring system produces results that are useful and accurate only in specific situations and/or areas. Therefore, an accurate global moisture data set has been derived from a combination of these measurement systems. Under a NASA peer-reviewed contract, STC-METSAT produced two 5-yr (1988-1992) global data sets. One is the total column (integrated) water vapor data set and the other, a global layered water vapor data set using a combination of radiosonde observations, Television and Infrared Observation Satellite (TIROS) Operational Satellite (TOVS), and Special Sensor Microwave/Imager (SSM/I) data sets. STC-METSAT also produced a companion, global, integrated liquid water data set. The complete data set (all three products) has been named NVAP, an anachronym for NASA Water Vapor Project. STC-METSAT developed methods to process the data at a daily time scale and 1 x 1 deg spatial resolution.
Ability of human interpreters to analyze and describe cloud patterns in photographs obtained by Tiros satellites
Polarization characteristics of solar radio emission at 74 Mc/s during September 1963 noise storm
Comparisons are made between rawinsonde and satellite profiles in seven areas for a wide range of surface and weather conditions. Variables considered include temperature, dewpoint temperature, thickness, precipitable water, lapse rate of temperature, stability, geopotential height, mixing ratio, wind direction, wind speed, and kinematic parameters, including vorticity and the advection of vorticity and temperature. In addition, comparisons are made in the form of cross sections and synoptic fields for selected variables. Sounding data from the NIMBUS 6 and TIROS N satellites were used. Geostrophic wind computed from smoothed geopotential heights provided large scale flow patterns that agreed well with the rawinsonde wind fields. Surface wind patterns as well as magnitudes computed by use of the log law to extrapolate wind to a height of 10 m agreed with observations. Results of this study demonstrate rather conclusively that satellite profile data can be used to determine characteristics of large scale systems but that small scale features, such as frontal zones, cannot yet be resolved.
Compilation of the results of the radiation measurements made by the radiometers on the tiros satellites
Monthly variations in Southern Hemisphere heat budget calculated from Tiros satellite radiation measurements
Tiros i satellite system - background, design and development, operation plan, launch, performance, and evaluation
Political problems surrounding the development of weather, communications, and Earth resources satellites are discussed. Tiros satellites, LANDSAT satellites, and Nimbus satellites are discussed.
Data was obtained from the UVI imager, ground based magnetometers, incoherent scatter radars, HF radars (SuperDarn), DMSP satellites, and NOAA TIROS satellites. The data from these sources have been integrated into a consistent description of the ionosphere, using the AMIE technique.
Tracking, television, and infrared radiometer sub- systems of tiros satellites
Tiros i meteorological satellite system - design, development, operation, engineering evaluation, and meteorological uses of television data