atlantic multidecadal variability & inter-american rainfall

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Atlantic Multidecadal Variability & Inter-American Rainfall D. B. Enfield 1 & A. M. Mestas- Nuñez 2 1 NOAA-AOML, Miami, Florida, USA 2 U. Miami/CIMAS, Miami, Florida, USA Research supported by NOAA OGP/PACS & IAI/CRN Enfield et al., 2001: Geophys. Res. Lett.

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Atlantic Multidecadal Variability & Inter-American Rainfall. D. B. Enfield 1 & A. M. Mestas-Nuñez 2 1 NOAA-AOML, Miami, Florida, USA 2 U. Miami/CIMAS, Miami, Florida, USA Research supported by NOAA OGP/PACS & IAI/CRN Enfield et al., 2001: Geophys. Res. Lett. What is the AMO?. - PowerPoint PPT Presentation

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Page 1: Atlantic  Multidecadal Variability  & Inter-American Rainfall

Atlantic Multidecadal Variability & Inter-American Rainfall

D. B. Enfield1 & A. M. Mestas-Nuñez2

1NOAA-AOML, Miami, Florida, USA2U. Miami/CIMAS, Miami, Florida, USA

Research supported by NOAA OGP/PACS & IAI/CRN

Enfield et al., 2001: Geophys. Res. Lett.

Page 2: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

What is the AMO? Documented by Schlesinger & Ramankutty

(1994) Regionally strong component of SSA analysis 65-70 year oscillation in N. Atlantic SST Related to shallow overturning circulation

Other observations Multi-taper SVD analysis of Kushnir et al. Gyre transport variations (Curry et al.)

Model replication GFDL coupled model (Delworth & Mann)

==> Overturning circulation implicated

Page 3: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Global warming model w/ greenhouse gases & solar forcing …residual low-pass observations not explained …residual behaves like AMO

Page 4: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Other evidence …

Supported by paleoclimate data, e.g.:

1650-1983 reconstruction of global air     temperatures by Mann et al. (Nature,    1998)

1500-1999 European reconstruction by    Luterbacher et al.

Page 5: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

1650-1983 tree rings & ice coresMann et al. (Nature, 1998)

Page 6: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

1500-1999 European treesLuterbacher et al. (GRL, 1999)

1500 1600 1700 1800 1900 2000

4

2

8

16

Peri

od (

years

)

32

64

128

256

Wavelet Power Spectrum, NAOI winters, 1500-1999

Page 7: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Our work … Define AMO index, correlate with global SST

Association with hemispheric rainfall

Associated changes in hurricane frequency

AMO slow covariation with US rainfall

Effects on river flows (Okeechobee)

Examine change in ENSO rainfall impacts

Page 8: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

SSTA: global distribution

Correlate AMO index with annual mean gridded SST

…10-year running means

…correlation significance by Monte Carlo          (random phase method of Ebisuzaki, 1997)…pattern like global rotated EOF         (Mestas & Enfield, JC, 1999)

Page 9: Atlantic  Multidecadal Variability  & Inter-American Rainfall

Correlation of AMO with global SSTA

Page 10: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Western Hemisphere rainfall associations

Which season is primarily responsible for the U.S. associations we see?

What rainfall associations exist on a larger, hemispheric scale?

Page 11: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Correlation of AMO vs. Eischeid gridded rainfall (JAS)

Page 12: Atlantic  Multidecadal Variability  & Inter-American Rainfall

Correlation of AMO with U.S. divisional rainfall (1895-1999)

Page 13: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Lake Okeechobee inflow vs. AMO

Page 14: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Q: How are Atlantic hurricanes affected?

The total numbers of tropical storms are not affected by the AMO phase. However,

The intensity *IS* affected:A significantly larger number of MAJOR    HURRICANES occurs during AMO warm    phases

We have been in a cool phase from 1970    through 1994 and have moved back into    another warm phase

Goldenberg et al. (Science 2001)

Page 15: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Page 16: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Page 17: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Q: How is ENSO-related rainfall affected by the

AMO? Previous studies ==> ENSO-PDO interaction

Gershunov & Barnett; Dettinger et al.

20-year running correlations (R-vs-AMO)

Two 30-year correlations: AMO- , AMO+

DJF NINO 3.4 vs. JFM rainfall (unsmoothed)

AMO- ==> 1965-1994

AMO+ ==> 1930-1959

Page 18: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

20-year running correlations

Page 19: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

AMO- ==> 1965-1994

Page 20: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

AMO+ ==> 1930-1959

Page 21: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Principal Results AMO+ ==> less rain, Mississippi basin, most of U.S.,

Mississipi outflow ==> 10% peak-to-peak

AMO+ ==> more rain in Florida, NE & Pacific NW, Okeechobee inflow ==> 40% peak-to-peak

Pattern is dominated by N.H. summer (JAS),  Also N. Europe+, NW Africa+ and NE Brasil- (summer)

Major hurricanes are >2x more frequent for AMO [+]

ENSO-rainfall patterns change with AMO phase (DJF)

Page 22: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Further research needed…

How does the AMO work?

Usual questions RE mechanisms, feedbacks, etc

Role of the Atlantic overturning circulation?

Atlantic-Pacific connection ==> NH annular mode?

Page 23: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Further research needed…

Slow co-variation of rainfall (mainly summer?)

WH warm pool effects on moisture transport to     U.S.

N. Atlantic influence on prevailing summer     circulation patterns over North America

Possible interaction with the North American     Monsoon

Page 24: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Further research needed…

AMO-ENSO interaction (mainly winter)

North Atlantic influence on prevailing winter     circulation over North America

Hypthesis: AMO(+) ==> deepened trough     over eastern U.S.

Page 25: Atlantic  Multidecadal Variability  & Inter-American Rainfall

NOAA Atlantic Oceanographic & Meteorological Laboratory

Relevant documentation

Relevant publications: Enfield & Mestas-Nuñez (J. Clim., 1999) Mestas-Nuñez & Enfield (J. Clim., 1999)

1999 & 2000 reprints are PDF files at<http://www.aoml.noaa.gov/phod/docs.html>

This paper submitted to Geophys. Res.

Lett.Email request to <[email protected]>