Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis

We analyze, using Poisson regressions, the main climate influences on North Atlantic tropical cyclone activity. The analysis is performed using not only various time series of basin-wide storm counts but also various series of regional clusters, taking into account shortcomings of the hurricane data...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Boudreault, Mathieu, Caron, Louis-Philippe, Camargo, Suzana J.
Other Authors: Barcelona Supercomputing Center
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2017
Subjects:
Online Access:http://hdl.handle.net/2117/104581
https://doi.org/10.1002/2016JD026103
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record_format openpolar
spelling ftupcatalunya:oai:upcommons.upc.edu:2117/104581 2023-05-15T17:33:36+02:00 Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis Boudreault, Mathieu Caron, Louis-Philippe Camargo, Suzana J. Barcelona Supercomputing Center 2017-04-25 23 p. http://hdl.handle.net/2117/104581 https://doi.org/10.1002/2016JD026103 eng eng American Geophysical Union (AGU) http://onlinelibrary.wiley.com/doi/10.1002/2016JD026103/full info:eu-repo/grantAgreement/MINECO/1PE/CGL2014-55764-R Open Access Àrees temàtiques de la UPC::Desenvolupament humà i sostenible::Política i gestió ambiental Cyclone forecasting Climate--Research Cluster analysis--Computer programs Tropical cyclones Hurricanes Climate variability North Atlantic ocean Storm tracks Trend Poisson regression Model selection Clima--Observacions Ciclons Article 2017 ftupcatalunya https://doi.org/10.1002/2016JD026103 2019-09-29T09:17:12Z We analyze, using Poisson regressions, the main climate influences on North Atlantic tropical cyclone activity. The analysis is performed using not only various time series of basin-wide storm counts but also various series of regional clusters, taking into account shortcomings of the hurricane database through estimates of missing storms. The analysis confirms that tropical cyclones forming in different regions of the Atlantic are susceptible to different climate influences. We also investigate the presence of trends in these various time series, both at the basin-wide and cluster levels, and show that, even after accounting for possible missing storms, there remains an upward trend in the eastern part of the basin and a downward trend in the western part. Using model selection algorithms, we show that the best model of Atlantic tropical cyclone activity for the recent past is constructed using Atlantic sea surface temperature and upper tropospheric temperature, while for the 1878–2015 period, the chosen covariates are Atlantic sea surface temperature and El Niño–Southern Oscillation. We also note that the presence of these artificial trends can impact the selection of the best covariates. If the underlying series shows an upward trend, then the mean Atlantic sea surface temperature captures both interannual variability and the upward trend, artificial or not. The relative sea surface temperature is chosen instead for stationary counts. Finally, we show that the predictive capability of the statistical models investigated is low for U.S. landfalling hurricanes but can be considerably improved when forecasting combinations of clusters whose hurricanes are most likely to make landfall. The authors would like to thank all the people and organizations who made their data available: the National Hurricane Center, the Earth System Research Laboratory (NOAA), the Climate Prediction Center (NOAA), the Hadley Centre, the National Climatic Data Center, the Joint Institute for the Study of the Atmosphere and Ocean at the University of Washington, the Climatic Research Unit of East Anglia, and the Solar Influences Data Analysis Center (SIDC) of the Royal Observatory of Belgium. Data sources are detailed in sections 2.1 and 2.2. We are also grateful to Phil Klotzbach for his helpful input and Jean-Philippe Baudouin for helping develop the R code used to produce the heatmaps. S.J.C. acknowledges support from NSF grant AGS 1143959 and NOAA grants NA15OAR43100095 and NA16OAR43100079. M.B. acknowledges support from the Natural Sciences and Engineering Research Council of Canada. L.P.C. acknowledges financial support from the Ministerio de Economía y Competitividad (MINECO; project CGL2014-55764-R). Peer Reviewed Postprint (published version) Article in Journal/Newspaper North Atlantic Universitat Politècnica de Catalunya (UPC): Theses and Dissertations Online (TDX) Canada Journal of Geophysical Research: Atmospheres 122 8 4258 4280
institution Open Polar
collection Universitat Politècnica de Catalunya (UPC): Theses and Dissertations Online (TDX)
op_collection_id ftupcatalunya
language English
topic Àrees temàtiques de la UPC::Desenvolupament humà i sostenible::Política i gestió ambiental
Cyclone forecasting
Climate--Research
Cluster analysis--Computer programs
Tropical cyclones
Hurricanes
Climate variability
North Atlantic ocean
Storm tracks
Trend
Poisson regression
Model selection
Clima--Observacions
Ciclons
spellingShingle Àrees temàtiques de la UPC::Desenvolupament humà i sostenible::Política i gestió ambiental
Cyclone forecasting
Climate--Research
Cluster analysis--Computer programs
Tropical cyclones
Hurricanes
Climate variability
North Atlantic ocean
Storm tracks
Trend
Poisson regression
Model selection
Clima--Observacions
Ciclons
Boudreault, Mathieu
Caron, Louis-Philippe
Camargo, Suzana J.
Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
topic_facet Àrees temàtiques de la UPC::Desenvolupament humà i sostenible::Política i gestió ambiental
Cyclone forecasting
Climate--Research
Cluster analysis--Computer programs
Tropical cyclones
Hurricanes
Climate variability
North Atlantic ocean
Storm tracks
Trend
Poisson regression
Model selection
Clima--Observacions
Ciclons
description We analyze, using Poisson regressions, the main climate influences on North Atlantic tropical cyclone activity. The analysis is performed using not only various time series of basin-wide storm counts but also various series of regional clusters, taking into account shortcomings of the hurricane database through estimates of missing storms. The analysis confirms that tropical cyclones forming in different regions of the Atlantic are susceptible to different climate influences. We also investigate the presence of trends in these various time series, both at the basin-wide and cluster levels, and show that, even after accounting for possible missing storms, there remains an upward trend in the eastern part of the basin and a downward trend in the western part. Using model selection algorithms, we show that the best model of Atlantic tropical cyclone activity for the recent past is constructed using Atlantic sea surface temperature and upper tropospheric temperature, while for the 1878–2015 period, the chosen covariates are Atlantic sea surface temperature and El Niño–Southern Oscillation. We also note that the presence of these artificial trends can impact the selection of the best covariates. If the underlying series shows an upward trend, then the mean Atlantic sea surface temperature captures both interannual variability and the upward trend, artificial or not. The relative sea surface temperature is chosen instead for stationary counts. Finally, we show that the predictive capability of the statistical models investigated is low for U.S. landfalling hurricanes but can be considerably improved when forecasting combinations of clusters whose hurricanes are most likely to make landfall. The authors would like to thank all the people and organizations who made their data available: the National Hurricane Center, the Earth System Research Laboratory (NOAA), the Climate Prediction Center (NOAA), the Hadley Centre, the National Climatic Data Center, the Joint Institute for the Study of the Atmosphere and Ocean at the University of Washington, the Climatic Research Unit of East Anglia, and the Solar Influences Data Analysis Center (SIDC) of the Royal Observatory of Belgium. Data sources are detailed in sections 2.1 and 2.2. We are also grateful to Phil Klotzbach for his helpful input and Jean-Philippe Baudouin for helping develop the R code used to produce the heatmaps. S.J.C. acknowledges support from NSF grant AGS 1143959 and NOAA grants NA15OAR43100095 and NA16OAR43100079. M.B. acknowledges support from the Natural Sciences and Engineering Research Council of Canada. L.P.C. acknowledges financial support from the Ministerio de Economía y Competitividad (MINECO; project CGL2014-55764-R). Peer Reviewed Postprint (published version)
author2 Barcelona Supercomputing Center
format Article in Journal/Newspaper
author Boudreault, Mathieu
Caron, Louis-Philippe
Camargo, Suzana J.
author_facet Boudreault, Mathieu
Caron, Louis-Philippe
Camargo, Suzana J.
author_sort Boudreault, Mathieu
title Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
title_short Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
title_full Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
title_fullStr Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
title_full_unstemmed Reanalysis of climate influences on Atlantic tropical cyclone activity using cluster analysis
title_sort reanalysis of climate influences on atlantic tropical cyclone activity using cluster analysis
publisher American Geophysical Union (AGU)
publishDate 2017
url http://hdl.handle.net/2117/104581
https://doi.org/10.1002/2016JD026103
geographic Canada
geographic_facet Canada
genre North Atlantic
genre_facet North Atlantic
op_relation http://onlinelibrary.wiley.com/doi/10.1002/2016JD026103/full
info:eu-repo/grantAgreement/MINECO/1PE/CGL2014-55764-R
op_rights Open Access
op_doi https://doi.org/10.1002/2016JD026103
container_title Journal of Geophysical Research: Atmospheres
container_volume 122
container_issue 8
container_start_page 4258
op_container_end_page 4280
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