2003: North Atlantic decadal variability and the formation of tropical storms and hurricanes
forming south of 23.5N and of Atlantic major hurricanes increased between the 1970’s/1980’s and 1995–2000. These increases are coincident with a multi-decadal warming in North Atlantic SST suggesting that the high activity of 1995–2000 may persist for the next 10 to 40 years. However, during 1950–20...
| Main Authors: | , |
|---|---|
| Other Authors: | |
| Format: | Text |
| Language: | English |
| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.3892 http://www.columbia.edu/itc/journalism/cases/katrina/Academic Journals/Geophysical Research Letters/Molinari GRL 03.pdf |
| Summary: | forming south of 23.5N and of Atlantic major hurricanes increased between the 1970’s/1980’s and 1995–2000. These increases are coincident with a multi-decadal warming in North Atlantic SST suggesting that the high activity of 1995–2000 may persist for the next 10 to 40 years. However, during 1950–2000 strong decadal oscillations are superimposed on the multi-decadal changes in both SST and tropical storms (positive SST anomalies, increased storm activity). We appear to be entering a negative phase of the decadal SST signal implying that tropical storm, and most likely major hurricane, activity may be reduced in the next several years rather than remain at the very high 1995–2000 level when both signals were in their positive phase. Tropical storm activity during 2001 and 2002 is less than the expected only from the multi-decadal signal but for 2002 the main |
|---|