What people are saying - Write a review
We haven't found any reviews in the usual places.
INTRODUCTION AND BACKGROUND
PERIODS CHOSEN FOR STUDY
STATISTICAL RELATIONSHIPS BETWEEN MESO
7 other sections not shown
Other editions - View all
21 September 23 March adiabatic method advection and divergence advection occurs ambient and dew-point analysis for 12Z area of radar areas of positive areas of thermal barotropic Ceiling/no ceiling ceilings and ceilings Ceilings Frequency ceilings were present clouds Compensation Principle composite radar summary conditional instability convective convergence at 850 correlation coefficients curvature analysis dew-point temperatures echoes are present expected area Figure frequency distributions ft within 100 gradient of height gradient of temperature height at 850 level for 12Z low-level convergence mesoscale systems mid-troposphere moisture objective method point temperatures positive vertical motion primitive equation radar chart radar echoes Results of curvature Scatter diagrams selected stations versus September 1969 shown in Fig shows sign of vertical skill score solid lines superimposed southeastern United space-mean contours spread stations versus gradients synoptic synoptic-scale temperature and height temperatures at 850 Texas thermal advection trough upper levels 500 upper-level divergence vorticity equation warm advection