Short- and medium-range prediction of tropical and transitioning cyclone tracks within the NCEP Global Ensemble Forecasting System
Short- and medium-range prediction of tropical and transitioning cyclone tracks within the NCEP Global Ensemble Forecasting System
The NCEP Global Ensemble Forecasting System (GEFS) is examined in its ability to predict tropical cyclone and extratropical transition (ET) positions. Forecast and observed tracks are compared in Atlantic and western North Pacific basins for 2006?08, and the accuracy and consistency of the ensemble are examined out to 8 days. Accuracy is quantified by the average absolute and along- and cross-track errors of the ensemble mean. Consistency is evaluated through the use of dispersion diagrams, missing rate error, and probability within spread. Homogeneous comparisons are made with the NCEP Global Forecasting System (GFS). The average absolute track error of the GEFS mean increases linearly at a rate of 50 n mi day?1 {$[$}where 1 nautical mile (n mi) = 1.852 km{$]$} at early lead times in the Atlantic, increasing to 150 n mi day?1 at 144 h (100 n mi day?1 when excluding ET tracks). This trend is 60 n mi day?1 at early lead times in the western North Pacific, increasing to 150 n mi day?1 at longer lead times (130 n mi day?1 when excluding ET tracks). At long lead times, forecasts illustrate left- and right-of-track biases in Atlantic and western North Pacific basins, respectively; bias is reduced (increased) in the Atlantic (western North Pacific) when excluding ET tracks. All forecasts were found to lag behind observed cyclones, on average. The GEFS has good dispersion characteristics in the Atlantic and is underdispersive in the western North Pacific. Homogeneous comparisons suggest that the ensemble mean has value relative to the GFS beyond 96 h in the Atlantic and less value in the western North Pacific; a larger sample size is needed before conclusions can be made.
Storm tracks, Tropical cyclones, Extratropical cyclones, Forecasting, Ensembles
1736-1754
Buckingham, Christian
dba7c776-a8c6-4617-ad40-7919dd4ab3dc
Marchok, Timothy
6635132a-eb50-4c5b-aba0-fda51516537d
Ginis, Isaac
2537d67f-1400-4601-a27b-48a15b12aa69
Rothstein, Lewis
077e8a8c-0147-437a-a74b-6af7a15e9855
Rowe, Dail
6589b94d-6cfa-4740-9fb1-df95f49aedc3
29 July 2010
Buckingham, Christian
dba7c776-a8c6-4617-ad40-7919dd4ab3dc
Marchok, Timothy
6635132a-eb50-4c5b-aba0-fda51516537d
Ginis, Isaac
2537d67f-1400-4601-a27b-48a15b12aa69
Rothstein, Lewis
077e8a8c-0147-437a-a74b-6af7a15e9855
Rowe, Dail
6589b94d-6cfa-4740-9fb1-df95f49aedc3
Buckingham, Christian, Marchok, Timothy, Ginis, Isaac, Rothstein, Lewis and Rowe, Dail
(2010)
Short- and medium-range prediction of tropical and transitioning cyclone tracks within the NCEP Global Ensemble Forecasting System.
Weather and Forecasting, 25 (6), .
(doi:10.1175/2010WAF2222398.1).
Abstract
The NCEP Global Ensemble Forecasting System (GEFS) is examined in its ability to predict tropical cyclone and extratropical transition (ET) positions. Forecast and observed tracks are compared in Atlantic and western North Pacific basins for 2006?08, and the accuracy and consistency of the ensemble are examined out to 8 days. Accuracy is quantified by the average absolute and along- and cross-track errors of the ensemble mean. Consistency is evaluated through the use of dispersion diagrams, missing rate error, and probability within spread. Homogeneous comparisons are made with the NCEP Global Forecasting System (GFS). The average absolute track error of the GEFS mean increases linearly at a rate of 50 n mi day?1 {$[$}where 1 nautical mile (n mi) = 1.852 km{$]$} at early lead times in the Atlantic, increasing to 150 n mi day?1 at 144 h (100 n mi day?1 when excluding ET tracks). This trend is 60 n mi day?1 at early lead times in the western North Pacific, increasing to 150 n mi day?1 at longer lead times (130 n mi day?1 when excluding ET tracks). At long lead times, forecasts illustrate left- and right-of-track biases in Atlantic and western North Pacific basins, respectively; bias is reduced (increased) in the Atlantic (western North Pacific) when excluding ET tracks. All forecasts were found to lag behind observed cyclones, on average. The GEFS has good dispersion characteristics in the Atlantic and is underdispersive in the western North Pacific. Homogeneous comparisons suggest that the ensemble mean has value relative to the GFS beyond 96 h in the Atlantic and less value in the western North Pacific; a larger sample size is needed before conclusions can be made.
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2010waf2222398%2E1.pdf
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Published date: 29 July 2010
Keywords:
Storm tracks, Tropical cyclones, Extratropical cyclones, Forecasting, Ensembles
Organisations:
Physical Oceanography
Identifiers
Local EPrints ID: 388265
URI: http://eprints.soton.ac.uk/id/eprint/388265
ISSN: 0882-8156
PURE UUID: 0d765a4f-6832-4305-88cc-22074e639192
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Date deposited: 23 Feb 2016 13:59
Last modified: 14 Mar 2024 22:55
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Author:
Christian Buckingham
Author:
Timothy Marchok
Author:
Isaac Ginis
Author:
Lewis Rothstein
Author:
Dail Rowe
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