An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles
ABSTRACT This study contrasts the pattern of low-frequency (LF) and high-frequency (HF) climate variability in the eastern Caribbean. A low-pass Butterworth filter is used to study oscillations in rainfall and regional SST on time scales of greater and less than 8 yr in the period 1901-2002. The res...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1051.7553 2023-05-15T17:28:42+02:00 An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles Isabelle Gouirand Bernd Sing The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7553 http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7553 http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf text ftciteseerx 2020-04-12T00:15:05Z ABSTRACT This study contrasts the pattern of low-frequency (LF) and high-frequency (HF) climate variability in the eastern Caribbean. A low-pass Butterworth filter is used to study oscillations in rainfall and regional SST on time scales of greater and less than 8 yr in the period 1901-2002. The results show that the southern and northern Antilles are dominated by HF variability, whereas rainfall fluctuations in the eastern Antilles oscillate at quasi-decadal periods over the 102-yr record. In the southern Antilles, the HF rainfall signal derives from a late-summer response to the ENSO phase: warm and dry versus cool and wet. In the northern Antilles, the HF signal relates to a combination of an ENSO and North Atlantic Oscillation (NAO) phase: a warm ENSO and a negative NAO bring wetter conditions, while a cool ENSO and a positive NAO bring drier conditions. The early rainfall LF signal in SST is characterized by a dipole between the North Atlantic and South Atlantic and is associated with cross-equatorial winds that promote convection in the Caribbean. The study analyzes the upper-ocean structure-in particular, a low (high) salinity signal in the tropical North Atlantic (North Pacific) that relates to LF (HF) climate variability. Text North Atlantic North Atlantic oscillation Unknown Butterworth ENVELOPE(66.733,66.733,-70.700,-70.700) Pacific |
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Open Polar |
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ftciteseerx |
language |
English |
description |
ABSTRACT This study contrasts the pattern of low-frequency (LF) and high-frequency (HF) climate variability in the eastern Caribbean. A low-pass Butterworth filter is used to study oscillations in rainfall and regional SST on time scales of greater and less than 8 yr in the period 1901-2002. The results show that the southern and northern Antilles are dominated by HF variability, whereas rainfall fluctuations in the eastern Antilles oscillate at quasi-decadal periods over the 102-yr record. In the southern Antilles, the HF rainfall signal derives from a late-summer response to the ENSO phase: warm and dry versus cool and wet. In the northern Antilles, the HF signal relates to a combination of an ENSO and North Atlantic Oscillation (NAO) phase: a warm ENSO and a negative NAO bring wetter conditions, while a cool ENSO and a positive NAO bring drier conditions. The early rainfall LF signal in SST is characterized by a dipole between the North Atlantic and South Atlantic and is associated with cross-equatorial winds that promote convection in the Caribbean. The study analyzes the upper-ocean structure-in particular, a low (high) salinity signal in the tropical North Atlantic (North Pacific) that relates to LF (HF) climate variability. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Isabelle Gouirand Bernd Sing |
spellingShingle |
Isabelle Gouirand Bernd Sing An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
author_facet |
Isabelle Gouirand Bernd Sing |
author_sort |
Isabelle Gouirand |
title |
An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
title_short |
An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
title_full |
An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
title_fullStr |
An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
title_full_unstemmed |
An Analysis of Low-and High-Frequency Summer Climate Variability around the Caribbean Antilles |
title_sort |
analysis of low-and high-frequency summer climate variability around the caribbean antilles |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7553 http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf |
long_lat |
ENVELOPE(66.733,66.733,-70.700,-70.700) |
geographic |
Butterworth Pacific |
geographic_facet |
Butterworth Pacific |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7553 http://www.bb-math.com/bernd/pub/JCLI-D-11-00269.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766121559261446144 |