The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation

This study identified how tropical cyclone precipitation (TCP) in the North Atlantic (NAT) varies in space and time. It also determined how climatic oscillations influence TCP in the NAT using 14 years of satellite-derived (TRMM) precipitation data. The analysis focused on the entire NAT as well as...

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Bibliographic Details
Main Author: Wang, Yue
Other Authors: Quiring , Steven M., Frauenfeld , Oliver W., Korty, Robert
Format: Thesis
Language:English
Published: 2015
Subjects:
Online Access:https://hdl.handle.net/1969.1/155063
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record_format openpolar
spelling fttexasamuniv:oai:oaktrust.library.tamu.edu:1969.1/155063 2023-07-16T03:59:45+02:00 The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation Wang, Yue Quiring , Steven M. Frauenfeld , Oliver W. Korty, Robert 2015-09-21T16:57:04Z application/pdf https://hdl.handle.net/1969.1/155063 en eng https://hdl.handle.net/1969.1/155063 Tropical cyclone precipitation Teleconnection Thesis text 2015 fttexasamuniv 2023-06-27T22:50:27Z This study identified how tropical cyclone precipitation (TCP) in the North Atlantic (NAT) varies in space and time. It also determined how climatic oscillations influence TCP in the NAT using 14 years of satellite-derived (TRMM) precipitation data. The analysis focused on the entire NAT as well as the Gulf of Mexico (GMX), Caribbean (CAR), and East Coast (ECO) sub-basins. Tropical cyclones (TC) contributed a mean of 76 mm of precipitation per year in the NAT. TCP is generally higher in the western and central NAT and little TCP occurs in the eastern NAT and south of 15°N latitude. The highest mean annual TCP occurs in the Gulf of Honduras (333 mm). Although there is substantial interannual variability in TCP, no statistically significant trends was detected in TCP volume, total rainfall, and TCP fraction in the NAT between 1998 and 2011. TCP is strongly correlated with TC frequency and intensity. Seasons with more frequent and intense TCs also receive more TCP. The relationship between TCP and four climate oscillations (El Niño/Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), Quasi-Biennial Oscillation (QBO) and Atlantic Meridional Mode (AMM)) was evaluated. AMM has the strongest influence on TCP, especially in the CAR region. The positive phase of AMM is related to increased TCP. NAO also has an influence on TCP, but the sign of the relationship varies by sub-basin because NAO influences the movement of TCs. TCP tends to increase (decrease) in the CAR (ECO) when NAO is positive. Although ENSO has an influence on TCP in NAT, it is not as strong as AMM or NAO. TCP is enhanced during La Niña phase and suppressed during El Niño phase. There is no obvious correlation between TCP and QBO. Thesis North Atlantic North Atlantic oscillation Texas A&M University Digital Repository
institution Open Polar
collection Texas A&M University Digital Repository
op_collection_id fttexasamuniv
language English
topic Tropical cyclone precipitation
Teleconnection
spellingShingle Tropical cyclone precipitation
Teleconnection
Wang, Yue
The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
topic_facet Tropical cyclone precipitation
Teleconnection
description This study identified how tropical cyclone precipitation (TCP) in the North Atlantic (NAT) varies in space and time. It also determined how climatic oscillations influence TCP in the NAT using 14 years of satellite-derived (TRMM) precipitation data. The analysis focused on the entire NAT as well as the Gulf of Mexico (GMX), Caribbean (CAR), and East Coast (ECO) sub-basins. Tropical cyclones (TC) contributed a mean of 76 mm of precipitation per year in the NAT. TCP is generally higher in the western and central NAT and little TCP occurs in the eastern NAT and south of 15°N latitude. The highest mean annual TCP occurs in the Gulf of Honduras (333 mm). Although there is substantial interannual variability in TCP, no statistically significant trends was detected in TCP volume, total rainfall, and TCP fraction in the NAT between 1998 and 2011. TCP is strongly correlated with TC frequency and intensity. Seasons with more frequent and intense TCs also receive more TCP. The relationship between TCP and four climate oscillations (El Niño/Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), Quasi-Biennial Oscillation (QBO) and Atlantic Meridional Mode (AMM)) was evaluated. AMM has the strongest influence on TCP, especially in the CAR region. The positive phase of AMM is related to increased TCP. NAO also has an influence on TCP, but the sign of the relationship varies by sub-basin because NAO influences the movement of TCs. TCP tends to increase (decrease) in the CAR (ECO) when NAO is positive. Although ENSO has an influence on TCP in NAT, it is not as strong as AMM or NAO. TCP is enhanced during La Niña phase and suppressed during El Niño phase. There is no obvious correlation between TCP and QBO.
author2 Quiring , Steven M.
Frauenfeld , Oliver W.
Korty, Robert
format Thesis
author Wang, Yue
author_facet Wang, Yue
author_sort Wang, Yue
title The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
title_short The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
title_full The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
title_fullStr The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
title_full_unstemmed The Effect of Teleconnections on North Atlantic Tropical Cyclone Precipitation
title_sort effect of teleconnections on north atlantic tropical cyclone precipitation
publishDate 2015
url https://hdl.handle.net/1969.1/155063
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://hdl.handle.net/1969.1/155063
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