Low Frequency Variability In Globally Integrated Tropical Cyclone Power Dissipation

[1] Surface wind and temperature records from the European Centre for MediumRange Weather Forecasts 40 Year Reanalysis (ERA-40) Project are used to estimate low-frequency variations in globally integrated tropical cyclone (TC) intensity from 1958 to 2001. For the first time, the annually integrated power dissipation (PD) is explicitly calculated on a global scale, and results show an upward trend in PD during much of the ERA-40 project period, although we argue this is at least partially due to limitations in cyclone representation in ERA-40. Comparing our estimated trend in PD with Emanuel’s (2005) approximation to PD reveals good agreement after 1978, coinciding with the onset of a major satellite observing-system epoch in ERA-40. The low pass (>60 months) filtered PD time series correlates with mean annual tropical temperature, thus this result is consistent with the hypothesis that tropical temperatures may directly regulate the integrated intensity of TCs. Citation: Sriver, R., and M. Huber (2006), Low frequency variability in globally integrated tropical cyclone power dissipation, Geophys. Res. Lett., 33, L11705, doi:10.1029/2006GL026167.