A numerical scheme for the prediction of hurricane and typhoon movement

The vector motion of severe tropical cyclones (including storm, hurricane/typhoon stages) is forecasted by a numerical scheme which involves two steps: a . Numerical geostrophic steering of the center of the cyclone using the U.S. Navy Fleet Numerical Weather Facility's (FNWF) operationally­ pr...

Full description

Bibliographic Details
Main Author: Renard, Robert J.
Other Authors: Naval Postgraduate School (U.S.), Meteorology and Oceanography
Format: Report
Language:unknown
Published: 1967
Subjects:
Online Access:https://hdl.handle.net/10945/53687
id ftnavalpschool:oai:calhoun.nps.edu:10945/53687
record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/53687 2024-06-09T07:48:18+00:00 A numerical scheme for the prediction of hurricane and typhoon movement Renard, Robert J. Naval Postgraduate School (U.S.) Meteorology and Oceanography 1967-12 59 p. application/pdf https://hdl.handle.net/10945/53687 unknown https://hdl.handle.net/10945/53687 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Report 1967 ftnavalpschool 2024-05-15T00:27:57Z The vector motion of severe tropical cyclones (including storm, hurricane/typhoon stages) is forecasted by a numerical scheme which involves two steps: a . Numerical geostrophic steering of the center of the cyclone using the U.S. Navy Fleet Numerical Weather Facility's (FNWF) operationally­ produced smoothed isobaric height fields, called SR. The tropical perturbations are steered in one-hour time steps up to 72 hours, using winds derived from the SR analysis dated closest to warning time. SR500 mb. in the Pacific and SR 700 mb . in the Atlantic gave the most accurate forecasts on tests of ten northwest Pacific typhoons and all five north Atlantic tropical storms and hurricanes in the period 15 August-1 November 1965. Forecasts were made twice daily, 0600 and 1800 GMT, during this period using best­ track information. b . Next, the numerical-steering prediction is objectively modified to adjust for bias (i e ., deficiency in both zonal and meridonal motion) by utilizing errors made in the most recent l2- and 24-hour numerical-steering forecasts. Several modes of adjustment are employed; the·most recent 12-(12- and 24-) hour numerical-steering bias yields the most accurate correction of subsequent Atlantic (Pacific) forecasts out to periods of 72 hours. The optimal Naval Postgraduate School (NPGS) technique produces forecast errors ranging from an average of 4.2 knots for 12-hour forecasts to 6.2 knots for 72-hour forecasts. The U .S. Navy 's official forecast accuracy is excelled by the NPGS scheme for all. time periods. Stratification of error statistics by area, trajectory and stage of storm, intercomparison with ESSA 's NHC-64 technique, discussion of merits and deficiencies of the research program relative to operational forecasts and current experiments at FNWF, are discussed. Naval Weather Research Facility, Norfolk, VA Report North Atlantic Naval Postgraduate School: Calhoun Pacific
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language unknown
description The vector motion of severe tropical cyclones (including storm, hurricane/typhoon stages) is forecasted by a numerical scheme which involves two steps: a . Numerical geostrophic steering of the center of the cyclone using the U.S. Navy Fleet Numerical Weather Facility's (FNWF) operationally­ produced smoothed isobaric height fields, called SR. The tropical perturbations are steered in one-hour time steps up to 72 hours, using winds derived from the SR analysis dated closest to warning time. SR500 mb. in the Pacific and SR 700 mb . in the Atlantic gave the most accurate forecasts on tests of ten northwest Pacific typhoons and all five north Atlantic tropical storms and hurricanes in the period 15 August-1 November 1965. Forecasts were made twice daily, 0600 and 1800 GMT, during this period using best­ track information. b . Next, the numerical-steering prediction is objectively modified to adjust for bias (i e ., deficiency in both zonal and meridonal motion) by utilizing errors made in the most recent l2- and 24-hour numerical-steering forecasts. Several modes of adjustment are employed; the·most recent 12-(12- and 24-) hour numerical-steering bias yields the most accurate correction of subsequent Atlantic (Pacific) forecasts out to periods of 72 hours. The optimal Naval Postgraduate School (NPGS) technique produces forecast errors ranging from an average of 4.2 knots for 12-hour forecasts to 6.2 knots for 72-hour forecasts. The U .S. Navy 's official forecast accuracy is excelled by the NPGS scheme for all. time periods. Stratification of error statistics by area, trajectory and stage of storm, intercomparison with ESSA 's NHC-64 technique, discussion of merits and deficiencies of the research program relative to operational forecasts and current experiments at FNWF, are discussed. Naval Weather Research Facility, Norfolk, VA
author2 Naval Postgraduate School (U.S.)
Meteorology and Oceanography
format Report
author Renard, Robert J.
spellingShingle Renard, Robert J.
A numerical scheme for the prediction of hurricane and typhoon movement
author_facet Renard, Robert J.
author_sort Renard, Robert J.
title A numerical scheme for the prediction of hurricane and typhoon movement
title_short A numerical scheme for the prediction of hurricane and typhoon movement
title_full A numerical scheme for the prediction of hurricane and typhoon movement
title_fullStr A numerical scheme for the prediction of hurricane and typhoon movement
title_full_unstemmed A numerical scheme for the prediction of hurricane and typhoon movement
title_sort numerical scheme for the prediction of hurricane and typhoon movement
publishDate 1967
url https://hdl.handle.net/10945/53687
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation https://hdl.handle.net/10945/53687
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
_version_ 1801379960482430976