Evaluating Tropical Cyclone Forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast Version 2
Tropical cyclone (TC) forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast version 2 (1985–2012) were evaluated from the climate perspective, with a focus on tropical cyclogenesis. Although the GEFS captures the climatological seasonality of tropical cyclogenesis over differe...
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description | Tropical cyclone (TC) forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast version 2 (1985–2012) were evaluated from the climate perspective, with a focus on tropical cyclogenesis. Although the GEFS captures the climatological seasonality of tropical cyclogenesis over different ocean basins reasonably well, large errors exist on the regional scale. As different genesis pathways are dominant over different ocean basins, genesis biases are related to biases in different aspects of the large-scale or synoptic-scale circulations over different basins. The negative genesis biases over the western North Pacific are associated with a weaker-than-observed monsoon trough in the GEFS, the erroneous genesis pattern over the eastern North Pacific is related to a southward displacement of the ITCZ, and the positive genesis biases near the Cape Verde islands and negative biases farther downstream over the Atlantic can be attributed to the hyperactive Africa easterly waves in the GEFS. The interannual and subseasonal variability of TC activity in the reforecasts was also examined to evaluate the potential skill of the GEFS in providing subseasonal and seasonal predictions. The GEFS skillfully captures the interannual variability of TC activity over the North Pacific and the North Atlantic, which can be attributed to the modulation of TCs by the El Niño–Southern Oscillation (ENSO) and the Atlantic meridional mode (AMM). The GEFS shows promising skill in predicting the active and inactive periods of TC activity over the Atlantic. The skill, however, has large fluctuations from year to year. The analysis presented herein suggests possible impacts of ENSO, the Madden–Julian oscillation (MJO), and the AMM on the TC subseasonal predictability. |
doi_str_mv | 10.1175/WAF-D-15-0176.1 |
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Although the GEFS captures the climatological seasonality of tropical cyclogenesis over different ocean basins reasonably well, large errors exist on the regional scale. As different genesis pathways are dominant over different ocean basins, genesis biases are related to biases in different aspects of the large-scale or synoptic-scale circulations over different basins. The negative genesis biases over the western North Pacific are associated with a weaker-than-observed monsoon trough in the GEFS, the erroneous genesis pattern over the eastern North Pacific is related to a southward displacement of the ITCZ, and the positive genesis biases near the Cape Verde islands and negative biases farther downstream over the Atlantic can be attributed to the hyperactive Africa easterly waves in the GEFS. The interannual and subseasonal variability of TC activity in the reforecasts was also examined to evaluate the potential skill of the GEFS in providing subseasonal and seasonal predictions. The GEFS skillfully captures the interannual variability of TC activity over the North Pacific and the North Atlantic, which can be attributed to the modulation of TCs by the El Niño–Southern Oscillation (ENSO) and the Atlantic meridional mode (AMM). The GEFS shows promising skill in predicting the active and inactive periods of TC activity over the Atlantic. The skill, however, has large fluctuations from year to year. The analysis presented herein suggests possible impacts of ENSO, the Madden–Julian oscillation (MJO), and the AMM on the TC subseasonal predictability.</description><identifier>ISSN: 0882-8156</identifier><identifier>EISSN: 1520-0434</identifier><identifier>DOI: 10.1175/WAF-D-15-0176.1</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Annual variations ; Basins ; Climate ; Climatology ; Cyclogenesis ; Cyclones ; Easterly waves ; El Nino ; El Nino phenomena ; El Nino-Southern Oscillation event ; Ensemble forecasting ; Forecasting ; Gravitational waves ; Hurricanes ; Interannual variability ; Islands ; Laboratories ; Madden-Julian oscillation ; Marine ; Monsoon trough ; Monsoons ; Ocean basins ; Physics ; Predictions ; Remote sensing systems ; Seasonal variations ; Seasonality ; Southern Oscillation ; Tropical climate ; Tropical cyclogenesis ; Tropical cyclones ; Variability ; Weather forecasting</subject><ispartof>Weather and forecasting, 2016-06, Vol.31 (3), p.895-916</ispartof><rights>Copyright American Meteorological Society 2016</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c343t-97a5097194f2e2ed24a0a20e70006c4bf9a6fb1f981fbc0ed5cd78963bdcf2763</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,3669,27906,27907</link.rule.ids></links><search><creatorcontrib>Li, Weiwei</creatorcontrib><creatorcontrib>Wang, Zhuo</creatorcontrib><creatorcontrib>Peng, Melinda S</creatorcontrib><title>Evaluating Tropical Cyclone Forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast Version 2</title><title>Weather and forecasting</title><description>Tropical cyclone (TC) forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast version 2 (1985–2012) were evaluated from the climate perspective, with a focus on tropical cyclogenesis. Although the GEFS captures the climatological seasonality of tropical cyclogenesis over different ocean basins reasonably well, large errors exist on the regional scale. As different genesis pathways are dominant over different ocean basins, genesis biases are related to biases in different aspects of the large-scale or synoptic-scale circulations over different basins. The negative genesis biases over the western North Pacific are associated with a weaker-than-observed monsoon trough in the GEFS, the erroneous genesis pattern over the eastern North Pacific is related to a southward displacement of the ITCZ, and the positive genesis biases near the Cape Verde islands and negative biases farther downstream over the Atlantic can be attributed to the hyperactive Africa easterly waves in the GEFS. The interannual and subseasonal variability of TC activity in the reforecasts was also examined to evaluate the potential skill of the GEFS in providing subseasonal and seasonal predictions. The GEFS skillfully captures the interannual variability of TC activity over the North Pacific and the North Atlantic, which can be attributed to the modulation of TCs by the El Niño–Southern Oscillation (ENSO) and the Atlantic meridional mode (AMM). The GEFS shows promising skill in predicting the active and inactive periods of TC activity over the Atlantic. The skill, however, has large fluctuations from year to year. The analysis presented herein suggests possible impacts of ENSO, the Madden–Julian oscillation (MJO), and the AMM on the TC subseasonal predictability.</description><subject>Annual variations</subject><subject>Basins</subject><subject>Climate</subject><subject>Climatology</subject><subject>Cyclogenesis</subject><subject>Cyclones</subject><subject>Easterly waves</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>El Nino-Southern Oscillation event</subject><subject>Ensemble forecasting</subject><subject>Forecasting</subject><subject>Gravitational waves</subject><subject>Hurricanes</subject><subject>Interannual variability</subject><subject>Islands</subject><subject>Laboratories</subject><subject>Madden-Julian oscillation</subject><subject>Marine</subject><subject>Monsoon trough</subject><subject>Monsoons</subject><subject>Ocean basins</subject><subject>Physics</subject><subject>Predictions</subject><subject>Remote sensing systems</subject><subject>Seasonal variations</subject><subject>Seasonality</subject><subject>Southern Oscillation</subject><subject>Tropical climate</subject><subject>Tropical cyclogenesis</subject><subject>Tropical cyclones</subject><subject>Variability</subject><subject>Weather 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oscillation</topic><topic>Marine</topic><topic>Monsoon trough</topic><topic>Monsoons</topic><topic>Ocean basins</topic><topic>Physics</topic><topic>Predictions</topic><topic>Remote sensing systems</topic><topic>Seasonal variations</topic><topic>Seasonality</topic><topic>Southern Oscillation</topic><topic>Tropical climate</topic><topic>Tropical cyclogenesis</topic><topic>Tropical cyclones</topic><topic>Variability</topic><topic>Weather forecasting</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Li, Weiwei</creatorcontrib><creatorcontrib>Wang, Zhuo</creatorcontrib><creatorcontrib>Peng, Melinda S</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Career & Technical Education Database</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources 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forecasting</jtitle><date>2016-06-01</date><risdate>2016</risdate><volume>31</volume><issue>3</issue><spage>895</spage><epage>916</epage><pages>895-916</pages><issn>0882-8156</issn><eissn>1520-0434</eissn><abstract>Tropical cyclone (TC) forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast version 2 (1985–2012) were evaluated from the climate perspective, with a focus on tropical cyclogenesis. Although the GEFS captures the climatological seasonality of tropical cyclogenesis over different ocean basins reasonably well, large errors exist on the regional scale. As different genesis pathways are dominant over different ocean basins, genesis biases are related to biases in different aspects of the large-scale or synoptic-scale circulations over different basins. The negative genesis biases over the western North Pacific are associated with a weaker-than-observed monsoon trough in the GEFS, the erroneous genesis pattern over the eastern North Pacific is related to a southward displacement of the ITCZ, and the positive genesis biases near the Cape Verde islands and negative biases farther downstream over the Atlantic can be attributed to the hyperactive Africa easterly waves in the GEFS. The interannual and subseasonal variability of TC activity in the reforecasts was also examined to evaluate the potential skill of the GEFS in providing subseasonal and seasonal predictions. The GEFS skillfully captures the interannual variability of TC activity over the North Pacific and the North Atlantic, which can be attributed to the modulation of TCs by the El Niño–Southern Oscillation (ENSO) and the Atlantic meridional mode (AMM). The GEFS shows promising skill in predicting the active and inactive periods of TC activity over the Atlantic. The skill, however, has large fluctuations from year to year. The analysis presented herein suggests possible impacts of ENSO, the Madden–Julian oscillation (MJO), and the AMM on the TC subseasonal predictability.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/WAF-D-15-0176.1</doi><tpages>22</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Annual variations Basins Climate Climatology Cyclogenesis Cyclones Easterly waves El Nino El Nino phenomena El Nino-Southern Oscillation event Ensemble forecasting Forecasting Gravitational waves Hurricanes Interannual variability Islands Laboratories Madden-Julian oscillation Marine Monsoon trough Monsoons Ocean basins Physics Predictions Remote sensing systems Seasonal variations Seasonality Southern Oscillation Tropical climate Tropical cyclogenesis Tropical cyclones Variability Weather forecasting |
title | Evaluating Tropical Cyclone Forecasts from the NCEP Global Ensemble Forecasting System (GEFS) Reforecast Version 2 |
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