A Smart Climatology of Evaporation Duct Height and Surface Radar Propagation in the Indian Ocean

Abstract

Surface electromagnetic propagation over the ocean is highly sensitive to near-surface atmospheric variability, particularly the height of the evaporation duct. Seasonal variation in near-surface metrological factors and sea surface temperatures impact the evaporation duct height (EDH). Present U.S. Navy EDH climatology is based on sparse ship observations over a relatively short time period and an outdated evaporation duct (ED) model. This EDH climatology does not utilize smart, or modern, climatology datasets or methods and provides only long term mean (LTM) values of EDH. We have used existing, civilian, dynamically balanced reanalysis data, for 1970 to 2006, and a state-of-the-art ED model, to produce a spatially and temporally refined EDH climatology for the Indian Ocean (10) and nearby seas. Comparisons of the present U.S. Navy EDH climatology with our climatology show a number of differences. These differences, and the differences in the methods used to generate the two climatologies, indicate that the EDH climatology we have generated provides a more accurate depiction of EDH.

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Document Details

Document Type
Technical Report
Publication Date
Sep 01, 2007
Accession Number
ADA474357

Entities

People

  • Katherine L. Twigg

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Energy and Power Technologies
  • Human Systems
  • Materials and Manufacturing Processes
  • Sensors
  • Weapons Technologies

DTIC Thesaurus Topics

  • Air Temperature
  • Climate
  • Climate Change
  • Correlation Analysis
  • Detection
  • Electromagnetic Radiation
  • Environment
  • Humidity
  • Indian Ocean
  • Meteorology
  • Naval Warfare
  • Oceans
  • Ridges
  • Sea Surface Temperature
  • Statistical Analysis
  • Surface Properties
  • Surface Temperature

Fields of Study

  • Environmental science

Readers

  • Atmospheric Remote Sensing.
  • Nanofabrication and Microfabrication.
  • Oceanography.