Two-Dimensional Modeling for Lineal and Areal Probabilities of Weather Conditions.

Abstract

Single-point probabilities of weather conditions, which are easily estimated from climatic records, have been extended to lines and areas by means of Monte Carlo simulation. Simulation was accomplished using the Boehm Sawtooth Wave (BSW) model. This model was chosen because of its speed and simplicity, and because it has a spatial correlation function similar to that of many weather elements. The BSW model generates fields (or maps) of normally distributed values called Equivalent Normal Deviates (ENDs). The procedure was to obtain the cumulative probability distribution for threshold END values. To do this, a large number of maps had to be generated, 25,000 in all, to approximate the true probability distributions. This was done for 12 different sized square areas and lines. The results were put in graphical form by plotting the probabilities as a function of areal and lineal size, and fitting them to curves through hand analysis. The curves were then fitted by equations, making it possible to obtain solutions quickly by computer. Thus, a model has been produced that can be used to estimate the probability that a certain weather condition will cover a given area or length, or fraction of an area or length.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Apr 10, 1984
Accession Number
ADA147970

Entities

People

  • C. F. Burger
  • I. I. Gringorten

Organizations

  • Air Force Research Laboratory

Tags

Communities of Interest

  • Air Platforms
  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Atmospheric Sciences
  • Classification
  • Cloud Cover
  • Coefficients
  • Computer Programming
  • Computer Programs
  • Computers
  • Data Science
  • Equations
  • Information Science
  • Monte Carlo Method
  • New England
  • Numerical Analysis
  • Probability
  • Probability Distributions
  • Simulations
  • Statistics

Readers

  • Climatology
  • Geodesy
  • Statistical inference.