Revisiting trough interactions and tropical cyclone intensity change

Abstract An updated climatology of Atlantic basin tropical cyclone (TC) intensity change in the presence of upper tropospheric trough forcing is presented. To control for changes in the background thermodynamic environment, a methodology that normalizes intensity change by the potential intensity of...

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Main Authors: C. M. Peirano, K. L. Corbosiero, B. H. Tang
Format: Article
Language:English
Published: Wiley 2016-05-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2016GL069040
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author C. M. Peirano
K. L. Corbosiero
B. H. Tang
author_facet C. M. Peirano
K. L. Corbosiero
B. H. Tang
author_sort C. M. Peirano
collection DOAJ
description Abstract An updated climatology of Atlantic basin tropical cyclone (TC) intensity change in the presence of upper tropospheric trough forcing is presented. To control for changes in the background thermodynamic environment, a methodology that normalizes intensity change by the potential intensity of the TC is used to more narrowly focus on the effect of troughs compared to previous studies. Relative to the full sample of Atlantic TCs, troughs are a negative influence on intensification: trough interaction cases are 4% less likely to intensify and 5% more likely to weaken. Troughs are especially detrimental compared to TCs without trough forcing: trough interaction cases are 14% less likely to intensify and 13% more likely to weaken. Additionally, eddy flux convergence of angular momentum, previously shown to positively affect TC intensity change, is shown to be a weak predictor of intensity change compared to vertical wind shear, which is enhanced during a trough interaction.
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spelling doaj-art-10a6a7d4a71248eeaff25c5a0e92a8932025-08-20T02:31:41ZengWileyGeophysical Research Letters0094-82761944-80072016-05-0143105509551510.1002/2016GL069040Revisiting trough interactions and tropical cyclone intensity changeC. M. Peirano0K. L. Corbosiero1B. H. Tang2Department of Atmospheric and Environmental Sciences SUNY‐University at Albany Albany New York USADepartment of Atmospheric and Environmental Sciences SUNY‐University at Albany Albany New York USADepartment of Atmospheric and Environmental Sciences SUNY‐University at Albany Albany New York USAAbstract An updated climatology of Atlantic basin tropical cyclone (TC) intensity change in the presence of upper tropospheric trough forcing is presented. To control for changes in the background thermodynamic environment, a methodology that normalizes intensity change by the potential intensity of the TC is used to more narrowly focus on the effect of troughs compared to previous studies. Relative to the full sample of Atlantic TCs, troughs are a negative influence on intensification: trough interaction cases are 4% less likely to intensify and 5% more likely to weaken. Troughs are especially detrimental compared to TCs without trough forcing: trough interaction cases are 14% less likely to intensify and 13% more likely to weaken. Additionally, eddy flux convergence of angular momentum, previously shown to positively affect TC intensity change, is shown to be a weak predictor of intensity change compared to vertical wind shear, which is enhanced during a trough interaction.https://doi.org/10.1002/2016GL069040tropical cyclonehurricanetroughintensityinteraction
spellingShingle C. M. Peirano
K. L. Corbosiero
B. H. Tang
Revisiting trough interactions and tropical cyclone intensity change
Geophysical Research Letters
tropical cyclone
hurricane
trough
intensity
interaction
title Revisiting trough interactions and tropical cyclone intensity change
title_full Revisiting trough interactions and tropical cyclone intensity change
title_fullStr Revisiting trough interactions and tropical cyclone intensity change
title_full_unstemmed Revisiting trough interactions and tropical cyclone intensity change
title_short Revisiting trough interactions and tropical cyclone intensity change
title_sort revisiting trough interactions and tropical cyclone intensity change
topic tropical cyclone
hurricane
trough
intensity
interaction
url https://doi.org/10.1002/2016GL069040
work_keys_str_mv AT cmpeirano revisitingtroughinteractionsandtropicalcycloneintensitychange
AT klcorbosiero revisitingtroughinteractionsandtropicalcycloneintensitychange
AT bhtang revisitingtroughinteractionsandtropicalcycloneintensitychange