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7 considering three climate state variables—the El Niño/Southern Oscillation (ENSO), 8 peak (August-October or ‘ASO’) Sea Surface Temperatures (SST) over the main 9 development region (‘MDR’: 6-18°N, 20-60°W), and the North Atlantic Oscillation 10 (NAO)—thought to influence variations in annual TC c...

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Main Authors: Thomas A. Sabbatelli, Michael E. Mann
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.408.3962
http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.408.3962 2023-05-15T17:33:26+02:00 Click Here for Full Article Thomas A. Sabbatelli Michael E. Mann The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.408.3962 http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.408.3962 http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf 25 Tropical Cyclones (TCs) [e.g Gray 1984]. The primary text ftciteseerx 2016-01-08T03:09:46Z 7 considering three climate state variables—the El Niño/Southern Oscillation (ENSO), 8 peak (August-October or ‘ASO’) Sea Surface Temperatures (SST) over the main 9 development region (‘MDR’: 6-18°N, 20-60°W), and the North Atlantic Oscillation 10 (NAO)—thought to influence variations in annual TC counts on interannual and longer 11 timescales. The unconditional distribution of TC counts is observed to be inconsistent 12 with the null hypothesis of a fixed rate random (Poisson) process. However, using two 13 different methods, we find that conditioning TC counts on just two climate state variables, 14 ENSO and MDR SST, can account for much or all of the apparent non-random variations 15 over time in TC counts. Based on statistical models of annual Atlantic TC counts 16 developed in this study and current forecasts of climate state variables, we predicted 17 m = 15 ± 4 total named storms for the 2007 season. 18 Citation: Sabbatelli, T. A., and M. E. Mann (2007), The influence of climate state variables on Atlantic Tropical Cyclone occurrence 19 rates, J. Geophys. Res., 112, XXXXXX, doi:10.1029/2007JD008385. 21 Text North Atlantic North Atlantic oscillation Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic 25 Tropical Cyclones (TCs) [e.g
Gray
1984]. The primary
spellingShingle 25 Tropical Cyclones (TCs) [e.g
Gray
1984]. The primary
Thomas A. Sabbatelli
Michael E. Mann
Click Here for Full Article
topic_facet 25 Tropical Cyclones (TCs) [e.g
Gray
1984]. The primary
description 7 considering three climate state variables—the El Niño/Southern Oscillation (ENSO), 8 peak (August-October or ‘ASO’) Sea Surface Temperatures (SST) over the main 9 development region (‘MDR’: 6-18°N, 20-60°W), and the North Atlantic Oscillation 10 (NAO)—thought to influence variations in annual TC counts on interannual and longer 11 timescales. The unconditional distribution of TC counts is observed to be inconsistent 12 with the null hypothesis of a fixed rate random (Poisson) process. However, using two 13 different methods, we find that conditioning TC counts on just two climate state variables, 14 ENSO and MDR SST, can account for much or all of the apparent non-random variations 15 over time in TC counts. Based on statistical models of annual Atlantic TC counts 16 developed in this study and current forecasts of climate state variables, we predicted 17 m = 15 ± 4 total named storms for the 2007 season. 18 Citation: Sabbatelli, T. A., and M. E. Mann (2007), The influence of climate state variables on Atlantic Tropical Cyclone occurrence 19 rates, J. Geophys. Res., 112, XXXXXX, doi:10.1029/2007JD008385. 21
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Thomas A. Sabbatelli
Michael E. Mann
author_facet Thomas A. Sabbatelli
Michael E. Mann
author_sort Thomas A. Sabbatelli
title Click Here for Full Article
title_short Click Here for Full Article
title_full Click Here for Full Article
title_fullStr Click Here for Full Article
title_full_unstemmed Click Here for Full Article
title_sort click here for full article
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.408.3962
http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.408.3962
http://www.meteo.psu.edu/holocene/public_html/shared/articles/SabbatelliMannJGR07inpress.pdf
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