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An empirical model of the Earth's horizontal wind fields: HWM07

  • D. P. Drob
  • , J. T. Emmert
  • , G. Crowley
  • , J. M. Picone
  • , G. G. Shepherd
  • , W. Skinner
  • , P. Hays
  • , R. J. Niciejewski
  • , M. Larsen
  • , C. Y. She
  • , J. W. Meriwether
  • , G. Hernandez
  • , M. J. Jarvis
  • , D. P. Sipler
  • , C. A. Tepley
  • , M. S. O'Brien
  • , J. R. Bowman
  • , Q. Wu
  • , Y. Murayama
  • , S. Kawamura
  • I. M. Reid, R. A. Vincent
  • Naval Research Laboratory
  • Atmospheric and Space Technology Research Associates
  • York University Toronto
  • University of Michigan, Ann Arbor
  • Clemson University
  • Colorado State University
  • University of Washington
  • British Antarctic Survey
  • Massachusetts Institute of Technology
  • Cornell University
  • SAIC
  • Japan National Institute of Information and Communications Technology
  • University of Adelaide

Research output: Contribution to journalArticlepeer-review

532 Scopus citations

Abstract

The new Horizontal Wind Model (HWM07) provides a statistical representation of the horizontal wind fields of the Earth's atmosphere from the ground to the exosphere (0-500 km). It represents over 50 years of satellite, rocket, and ground-based wind measurements via a compact Fortran 90 subroutine. The computer model is a function of geographic location, altitude, day of the year, solar local time, and geomagnetic activity. It includes representations of the zonal mean circulation, stationary planetary waves, migrating tides, and the seasonal modulation thereof. HWM07 is composed of two components, a quiet time component for the background state described in this paper and a geomagnetic storm time component (DWM07) described in a companion paper.

Original languageEnglish
Article numberA12304
JournalJournal of Geophysical Research: Space Physics
Volume113
Issue number12
DOIs
StatePublished - Dec 1 2008

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