Evaluation of the AFWA WRF 4-KM Moving Nest Model Predictions for Western North Pacific Tropical Cyclones

Abstract

The Air Force Weather Agency (AFWA) version of the Advanced Research Weather Research and Forecasting (ARW) model with a moving 4-km nested grid is examined for 10 track and intensity predictions of six western North Pacific tropical cyclones during 2005. In three of the 10 integrations the ARW vortex tracker algorithm based on the 500-mb height minimum failed to appropriately move the nest and thus lost track of the storm vortex. For the other seven cases the ARW track forecasts are more skillful than the AFWA MM5 forecasts and (except at 12 h) the CLI PER-type forecasts. The ARW intensity forecasts were less skillful than the MM5 and CLI PER-type forecasts at all forecast intervals and were severely degraded by a large negative bias at the initial time. The deficiency in these intensity forecasts is shown to be related to model spin-up (lasting 12-54 h) problems caused by the lack of a bogus vortex and a cold start initialization from the interpolation of the NOEP Global Forecast System (GFS) analysis to the 12- km and 4-km grids. Thus a more appropriate initial vortex representation will be required to improve intensity forecasts.

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Document Details

Document Type
Technical Report
Publication Date
Mar 01, 2006
Accession Number
ADA445292

Entities

People

  • William R. Ryerson

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Energy and Power Technologies
  • Space

DTIC Thesaurus Topics

  • Air Force
  • Air Force Facilities
  • Algorithms
  • Boundaries
  • Boundary Layer
  • Convection
  • Department Of Defense
  • Fluid Dynamics
  • Geography
  • Grids
  • High Resolution
  • Intensity
  • Meteorology
  • Tropical Cyclones
  • Two Dimensional
  • United States
  • United States Pacific Command

Fields of Study

  • Environmental science

Readers

  • Inertial Navigation Systems.
  • Mathematics or Statistics
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers