Abstract

It is a community wide belief that the Atlantic Multi-decadal Oscillation (AMO) and the Accumulated Cyclone Energy (ACE) are strongly positively correlated and in lock-step for the characterization of a tropical cyclone (TC)—hurricane season; including how many named TCs will form and how many will become hurricanes and major hurricanes [1]-[4]. In this paper, we decompose the AMO and ACE time series into their internal modes of variability using the Hilbert-Huang Transform REF _Ref386094582 \r \h [5] and the Ensemble Empirical Modal Decomposition (EEMD) REF _Ref386094585 \r \h [6], and look into the relationships that exist between the individual corresponding modes of the AMO and the ACE. We then evaluate the degrees of frequency domain correlations between the internal modes of variability of the AMO and the ACE across the entire record length time series. The 2013 North Atlantic Hurricane Season, which had been predicted to be “above normal”, with an ACE estimated to be between 122 and 138 by the National Oceanic & Atmospheric Administration (NOAA), turned out to be one of the quietest on record. The actual 2013 observed ACE was only 33 (unit: 104 kn2) or 29% of the 65 year (1948-2012) average of 103 (with a median of 89.5) and is the 5th lowest value since 1950. Following the visual correlations between the ACE and the AMO in the past, and assuming past is prologue to the future, the “above normal” forecast of the ACE led to a tropical cyclone community wide forecast of a highly active 2013 hurricane season. So why the busted 2013 forecast? This study will address the possible reasons.

Highlights

  • The Accumulated Cyclone Energy (ACE) is a measure used by National Oceanic & Atmospheric Administration (NOAA) to express the wind energy of individual tropical cyclones (TCs) summed over an entire tropical cyclone season in the North Atlantic Ocean Basin (NAOB)

  • The ACE is a measure used by NOAA to express the wind energy of individual tropical cyclones (TCs) summed over an entire tropical cyclone season in the North Atlantic Ocean Basin (NAOB)

  • The Atlantic Multi-decadal Oscillation (AMO) itself has oscillations at different frequency domains influenced by other climate factors

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Summary

Introduction

The ACE is a measure used by NOAA to express the wind energy of individual tropical cyclones (TCs) summed over an entire tropical cyclone season in the North Atlantic Ocean Basin (NAOB) It is defined as the sum of the squares of the maximum sustained surface wind speed times 104 (knots2) measured every six hours for all named systems while they are of tropical storm strength [7]. Using AMO indices as a predictor combined with the El Nino Southern Oscillation (ENSO), the Atlantic Meridional Mode, and the Tropical North Atlantic Index, the hindcasting skill of ACE significantly exceeds the climatology (Figure 3). Major Hurricane Count in North Atlantic Basin (RMSE skill is 47.4% over climatology)

ACE and AMO Data Analyses
Findings
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