Relationships Between Vertical Motion on Isentropic Surfaces from 3-Hr Rawinsonde Data and Radar Echoes.

Abstract

Vertical motion on isentropic surfaces obtained at 3-h intervals from NASA's second Atmospheric Variability (Pilot) Experiment (AVE IIP) conducted on 11 and 12 May 1974 is related to convection indicated by radar echoes. Temporal and spatial changes in vertical motion are shown and demonstrated to be associated with areas of convection. Vertical motion as large as 22 cm/s was calculated and it is shown that vertical motion changes as much as 20 cm/s in a horizontal distance of 300 km. The rate of change of vertical motion is demonstrated to be as large as 8 cm/s/h from data taken at 3-h intervals while data taken at 12-h intervals the same day displayed a maximum rate of change of 2 cm/s/h. Radar observations confirmed that the intensity of convection varies as a result of the atmospheric variability as detected by 3-h data but is invisible in data taken at 12-h intervals.

Document Details

Document Type
Technical Report
Publication Date
May 01, 1975
Accession Number
ADA018905

Entities

People

  • James W. Overall

Organizations

  • Air Force Institute of Technology

Tags

DTIC Thesaurus Topics

  • Acquisition
  • Communication Equipment
  • Convection
  • Data Acquisition
  • Instrumentation
  • Intensity
  • Intervals
  • Measuring Instruments
  • Observation
  • Radiosondes

Fields of Study

  • Environmental science

Readers

  • Atmospheric Remote Sensing.
  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Radar Systems Engineering.