A High-Resolution Urban Canopy/Land-Surface Modeling System

Abstract

Heterogeneities in land-surface characteristics that occur in transitions from a large coastal city to the suburbs and then to the rural countryside can significantly alter the lower portion of the atmosphere through mechanical and thermodynamical interactions. For example, urban-rural interfaces, both upwind and downwind of the urban region, are often preferred zones for the initiation of atmospheric convection or modification of ongoing convection. Changes in the vertical profile of atmospheric static stability in the lowest portion of the atmosphere due to such heterogeneous surface forcing can have an important impact on transport and dispersion of potentially harmful chemical/biological agents. Thus, with a large percentage of the world's population living in coastal urban areas and an increasing emphasis of Naval fleet operations in coastal regions, an accurate characterization of high-resolution processes in numerical weather prediction models will greatly improve local forecasts for populations at risk as well as military operations.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 2006
Accession Number
ADA523954

Entities

People

  • T. R. Holt

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Energy and Power Technologies
  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Atmospheres
  • Atmospheric Sciences
  • Biological Factors
  • Convection
  • Department Of Homeland Security
  • High Resolution
  • Marine Meteorology
  • Meteorology
  • Military Operations
  • New York
  • Regions
  • Sea Breeze
  • Sea Surface Temperature
  • Security
  • Surface Temperature
  • Urban Areas
  • Weather Forecasting

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Urban Planning and Geography.