HR: 14:40h
AN: GC13B-05 INVITED    [Abstracts]
TI: Has Anthropogenic Forcing Caused a Discernible Change in Atlantic Hurricane Activity?
AU: * Knutson, T R
EM: Tom.Knutson@noaa.gov
AF: Geophysical Fluid Dynamics Laboratory/NOAA, P.O. Box 308 Forrestal Campus, U.S. Rt. 1, Princeton, NJ 08542, United States
AU: Vecchi, G A
EM: gabriel.a.vecchi@noaa.gov
AF: Geophysical Fluid Dynamics Laboratory/NOAA, P.O. Box 308 Forrestal Campus, U.S. Rt. 1, Princeton, NJ 08542, United States
AB: There is currently evidence both for and against the existence of a discernible anthropogenic impact on Atlantic hurricane activity. Emanuel's (pers. comm. 2007) Power Dissipation Index shows unprecedented high values in recent decades in the context of the past 60 yr, and correlates remarkably well with low-frequency tropical Atlantic SST variations. The limited record length, partial basin coverage by aircraft in the pre-satellite era, and lack of reconciliation with models limit the usefulness of this result for identifying possible anthropogenic influences. Landsea (EOS, 2007) uses landfalling storm statistics to infer no significant increase in basin-wide tropical storm counts since 1900. Landsea's critical assumption of a constant landfalling fraction over time limits confidence in this assessment. Nonetheless, an important finding is that U.S. landfalling hurricane activity (frequency and PDI) show no increasing trend over the past century or so. Holland and Webster (Phil. Trans. R. Soc. A 2007) conclude that basin-wide tropical cyclone and hurricane counts have increased dramatically during the past century, related to the rise in tropical Atlantic SSTs. Their key assumption is that the existing HURDAT data reliably portrays basin-wide statistics for tropical storms, hurricanes and major hurricanes, at least back to ~1900, which requires further substantiation. We use historical Atlantic ship track and storm track data to estimate the expected number of missing tropical storms each year in the pre-satellite era (1878-1965). After adjustment, the storm counts covary with tropical SSTs on multi-decadal time scales, but their long-term trend (1878-2006) is weaker than the trend in similarly normalized SSTs (though both are nominally positive). The linear trend in adjusted storm counts for 1900-2006 is strongly positive (+4.2 storms/century) and highly significant even after accounting for serial correlation. However, this trend begins near a local minimum in the time series and ends with the recent high activity, perhaps exaggerating the significance of the trend. The trend beginning from 1878 is weakly positive, and not statistically significant with p=0.3. The uncertainty in the late 1800s is larger than that during the 1900s--an important caveat on the results using the earlier start date. Tropical cyclone occurrence rates appear to have decreased in the western part of the basin (consistent with declining U.S. landfalling hurricane counts) but may have increased slightly in the central and eastern basin, suggesting a structural change such as shifts in storm tracks. Important assumptions of our methodology, such as that all landfalling storms since 1878 were detected and reported, require further investigation. In an attempt to reconcile the past observations with models, we have developed a regional modeling framework for downscaling Atlantic hurricane activity. Given observed large-scale atmospheric conditions and SSTs from reanalyses, the model reproduces several aspects of past Atlantic hurricane behavior (1980-2006). However, much further work is needed to produce simulations where hurricane activity changes can be confidently attributed, using such models, to various anthropogenic forcings or natural processes. Based on available evidence, we cannot yet conclude with high confidence that anthropogenic forcing has caused a discernible anthropogenic influence on hurricane activity to date.
DE: 1616 Climate variability (1635, 3305, 3309, 4215, 4513)
DE: 1630 Impacts of global change (1225)
DE: 1637 Regional climate change
DE: 3305 Climate change and variability (1616, 1635, 3309, 4215, 4513)
DE: 3374 Tropical meteorology
SC: Global Environmental Change [GC]
MN: 2007 Fall Meeting