Abstract: No Abstract Available.

Abstract: A new PPI map is made up of 600 radial lines, each of 100 dots. Each dot is in one of six shades of grey, thus indicating target intensity, and dot size varies somewhat with shade. Each dot combines k independent data, ...

Abstract: A characteristic ?mares' tail? pattern of falling snow (observed in vertical section by radar) suggests that the snow is generated continuously, in compact generating elements; the pattern results from the snow's falling ...

Abstract: Fields of temperature, thickness and precipitable water, derived from common sets of Tiros Operational Vertical Sounder (TOVS) radiance data have been intercompared. These fields were produced by a variety of institutions ...

Abstract: tract

Abstract: Radar maps of precipitation at a height of 6 km have been studied for the thunderstorms of one July day. Regions on these maps within which the intensity level exceeds 30 dBZ (corresponding to a rainfall rate of 2.8 mm ...

Abstract: A bounded vortex flow is generated by a nozzle with a central suction outlet surrounded by inlet jets with a 15 deg inclination in the azimuthal direction. The jets impinge on a flat surface called the impingement surface. ...

Abstract: Theories which associate atmospheric blocking with isolated ?free mode? solutions of the equations of motion are reviewed and the central role played by the potential function ? ≡ dq/d? (where q is the is the quasi-geostrophic ...

Abstract: For the summer of 1964, precipitation intensity in the vicinity of Montreal, observed by CPS-9 radar, was recorded on constant-altitude maps at six heights. To allow for attenuation (at ??=?3.2 cm) and other radar ...

Abstract: Using a CPS-9 radar (wavelength 3.2 cm, beamwidth 1°) in dry snow, radar returns from a layer at an average height of 5000 ft were converted to snowfall rates (taking Z?R2.0) and summed over 36 hr to obtain a map of snowfall ...