Variability in tropical cyclone heat potential over the Southwest Indian Ocean. Issue 12 (11th December 2013)

• Record Type: Journal Article
• Authors: Malan, N.; Reason, C. J. C.; Loveday, B. R.
• Is Part Of: Journal of geophysical research. Volume 118:Issue 12(2013:Dec.)
• Page Start: 6734
• Page End: 6746
• Publication Date: 2013-12-11
• Subjects: tropical cyclones -- SW Indian Ocean -- heat potential -- climate variability; Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/2013JC008958
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract : [1] Tropical cyclone heat potential (TCHP) has been proposed as being important for hurricane and typhoon intensity. Here, a climatology of TCHP is developed for the Southwest Indian Ocean, a basin that experiences on average 11–12 tropical cyclones per year, many of which impact on Mauritius, Reunion and Madagascar, and Mozambique. SODA data and a regional ocean model forced with the GFDL‐CORE v.2b reanalysis winds and heat fluxes are used to derive TCHP values during the 1948–2007 period. The results indicate that TCHP increases through the austral summer, peaking in March. Values of TCHP above 40 kJ cm −2, suggested as the minimum needed for tropical cyclone intensification, are still present in the northern Mozambique Channel in May. A time series of TCHP spatially averaged over the Seychelles‐Chagos thermocline ridge (SCTR), an important area for tropical cyclones, is presented. The model time series, which agrees well with XBT‐based observations ( r = 0.82, p = 0.01), shows considerable interannual variability overlaying an upward tendency that matches with an observed increase in severe tropical cyclone days in the Southwest Indian Ocean. Although an increase in severe storms is seen during 1997–2007, the increasing TCHP tendency time series after 1997 coincides with a decrease in total cyclone numbers, a mismatch that is ascribed to increased atmospheric anticyclonicity over the basin. Seasons of increased (decreased) TCHP over the SCTR appear to be associated with dry (wet) conditions over certain areas of southern and East Africa and are linked with changes in zonal wind and vertical motion in the midtroposphere. Key Points: First climatology of TCHP in SW Indian Ocean Interannual and decadal variability of TCHP Potential predictability of rainfall