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contributor authorMoore, J. C.
contributor authorGrinsted, A.
contributor authorJevrejeva, S.
date accessioned2017-06-09T16:19:25Z
date available2017-06-09T16:19:25Z
date copyright2008/04/01
date issued2008
identifier issn0894-8755
identifier otherams-65747.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207006
description abstractControversy exists over the role of the recent rise in sea surface temperatures (SST) and the frequency of tropical cyclones or hurricanes. Here, 135 yr of observational records are used to demonstrate how sea surface temperature, sea level pressure, and cyclone numbers are linked. A novel wavelet-lag coherence method is used to study cause and effect relations over a large space of time scales, phase lags, and periods. It is found that SST and cyclones are not merely correlated, but are in a negative feedback loop, where rising SST causes increased numbers of cyclones, which reduce SST. This is statistically most significant at decadal and not at longer periods, which is contrary to expectations if long-period natural cycles are important in driving cyclone numbers. Spatial relationships are examined using phase-aware teleconnections, which at the dominant decadal period show the in-phase behavior of the Atlantic SST in the Gulf Stream region, reflecting the role of the transportion of heat northward from the tropical Atlantic. At 5-yr periods there is significant coherence when SST leads cyclones by 2 yr, and this is associated with tropical ENSO activity such that, as predicted, increasing numbers of El Niños cause fewer Atlantic cyclones. The pattern of coherence existing since 1970 strongly favors the decadal coherence band, and despite growing coherence at higher frequencies, there is none at the 5-yr band, perhaps explaining why the observed sensitivity between SST and cyclones is larger than that from general circulation model (GCM) predictions and becoming greater.
publisherAmerican Meteorological Society
titleGulf Stream and ENSO Increase the Temperature Sensitivity of Atlantic Tropical Cyclones
typeJournal Paper
journal volume21
journal issue7
journal titleJournal of Climate
identifier doi10.1175/2007JCLI1752.1
journal fristpage1523
journal lastpage1531
treeJournal of Climate:;2008:;volume( 021 ):;issue: 007
contenttypeFulltext


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