Multiyear Predictions of North Atlantic Hurricane Frequency: Promise and Limitations

Gabriel A. Vecchi Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Rym Msadek Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Whit Anderson Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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You-Soon Chang Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Thomas Delworth Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Keith Dixon Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Rich Gudgel Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Anthony Rosati Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Bill Stern Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Gabriele Villarini IIHR–Hydroscience & Engineering, The University of Iowa, Iowa City, Iowa

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Andrew Wittenberg Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Xiasong Yang Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Fanrong Zeng Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Rong Zhang Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Shaoqing Zhang Geophysical Fluid Dynamics Laboratory, NOAA, Princeton, New Jersey

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Abstract

Retrospective predictions of multiyear North Atlantic Ocean hurricane frequency are explored by applying a hybrid statistical–dynamical forecast system to initialized and noninitialized multiyear forecasts of tropical Atlantic and tropical-mean sea surface temperatures (SSTs) from two global climate model forecast systems. By accounting for impacts of initialization and radiative forcing, retrospective predictions of 5- and 9-yr mean tropical Atlantic hurricane frequency show significant correlations relative to a null hypothesis of zero correlation. The retrospective correlations are increased in a two-model average forecast and by using a lagged-ensemble approach, with the two-model ensemble decadal forecasts of hurricane frequency over 1961–2011 yielding correlation coefficients that approach 0.9. These encouraging retrospective multiyear hurricane predictions, however, should be interpreted with care: although initialized forecasts have higher nominal skill than uninitialized ones, the relatively short record and large autocorrelation of the time series limits confidence in distinguishing between the skill caused by external forcing and that added by initialization. The nominal increase in correlation in the initialized forecasts relative to the uninitialized experiments is caused by improved representation of the multiyear tropical Atlantic SST anomalies. The skill in the initialized forecasts comes in large part from the persistence of a mid-1990s shift by the initialized forecasts, rather than from predicting its evolution. Predicting shifts like that observed in 1994/95 remains a critical issue for the success of multiyear forecasts of Atlantic hurricane frequency. The retrospective forecasts highlight the possibility that changes in observing system impact forecast performance.

Corresponding author address: Gabriel A. Vecchi, Geophysical Fluid Dynamics Laboratory, NOAA, U.S. Route 1, Forrestal Campus, Princeton, NJ 08542. E-mail: gabriel.a.vecchi@noaa.gov

This article is included in the North American Climate in CMIP5 Experiments special collection.

Abstract

Retrospective predictions of multiyear North Atlantic Ocean hurricane frequency are explored by applying a hybrid statistical–dynamical forecast system to initialized and noninitialized multiyear forecasts of tropical Atlantic and tropical-mean sea surface temperatures (SSTs) from two global climate model forecast systems. By accounting for impacts of initialization and radiative forcing, retrospective predictions of 5- and 9-yr mean tropical Atlantic hurricane frequency show significant correlations relative to a null hypothesis of zero correlation. The retrospective correlations are increased in a two-model average forecast and by using a lagged-ensemble approach, with the two-model ensemble decadal forecasts of hurricane frequency over 1961–2011 yielding correlation coefficients that approach 0.9. These encouraging retrospective multiyear hurricane predictions, however, should be interpreted with care: although initialized forecasts have higher nominal skill than uninitialized ones, the relatively short record and large autocorrelation of the time series limits confidence in distinguishing between the skill caused by external forcing and that added by initialization. The nominal increase in correlation in the initialized forecasts relative to the uninitialized experiments is caused by improved representation of the multiyear tropical Atlantic SST anomalies. The skill in the initialized forecasts comes in large part from the persistence of a mid-1990s shift by the initialized forecasts, rather than from predicting its evolution. Predicting shifts like that observed in 1994/95 remains a critical issue for the success of multiyear forecasts of Atlantic hurricane frequency. The retrospective forecasts highlight the possibility that changes in observing system impact forecast performance.

Corresponding author address: Gabriel A. Vecchi, Geophysical Fluid Dynamics Laboratory, NOAA, U.S. Route 1, Forrestal Campus, Princeton, NJ 08542. E-mail: gabriel.a.vecchi@noaa.gov

This article is included in the North American Climate in CMIP5 Experiments special collection.

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