Using SeaRad and MODTRAN to Improve the Ocean Background Model of the Electro-Optical Tactical Decision Aid (EOTDA)

Abstract

This report compares the predictions of ocean radiance and detection range from the unmodified Electro-optical Tactical Decision Aid (EOTDA) version 3.0 with a modified version. The original EOTDA was developed by the U. S. Air Force, with only minimal attention applied to the complexities of the marine environment. The objective of this comparative study was to evaluate whether modifying the EOTDA would improve ocean background radiance predictions and ultimately improve detection range performance. The modifications involved replacing the original semi-empirical water background model with a rigorous geometric ocean radiance model, called SeaRad, and replacing the sky radiance model with the sky model from the MODTRAN 3 code. A significant difference in behavior was noted between the original and modified EOTDA when comparing the zero-range ocean background temperature predictions of both models. Because sufficient improvement was realized with the modified EOTDA employing the SeaRad ocean radiance model in combination with the MODTRAN sky radiance model, transition to the navy fleet-ready version is recommended.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1998
Accession Number
ADA336500

Entities

People

  • C. P. Mcgrath

Organizations

  • Naval Information Warfare Systems Command

Tags

Communities of Interest

  • Ground and Sea Platforms
  • Materials and Manufacturing Processes
  • Sensors
  • Weapons Technologies

DTIC Thesaurus Topics

  • Air Force
  • Altitude
  • Atmospheres
  • Body Temperature
  • Computer Programs
  • Computers
  • Detection
  • Detectors
  • Environment
  • Military Research
  • Naval Warfare
  • Operating Systems
  • Scattering
  • Solar Radiation
  • Standards
  • Tactical Decision Aids
  • Warfare

Readers

  • Aerospace Research.
  • Computational Modeling and Simulation
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers