Obviously as sea temps rise,TCHP will increase overall...TCHP is a factor to look at in assessing if rapid intensification of a system is possible....but systems can develop and maintain themselves in area of low TCHP as long as the water closest to the surface is warm enough (generally 80+).
Raises an interesting pre-season question...where do we stand now compared to average for the time of year...latest Heat Anomaly map shows that the 300m depth of water has higher heat content than normal across the Gulf and part of the Atlantic south of 15N. Areas to the north in the central Atlantic are below normal. The Gulf anomalies could lend to early development in that area if it persists....by June the Gulf will be in the 80s (or rapidly approaching)...that's not the question...but if the depth of warm water and the resulting TCHP are higher than normal....could be a factor favoring early storms.
http://www.cpc.ncep.noaa.gov/products/G ... 00.30d.gifOverall, compared to the same time last year, the Gulf is a bit warmer..as is the atlantic off the east-central florida coast. Bay of Campeche is significantly warmer than last year....water already in the 80s.
May 1, 2008:

May 1, 2009:

cycloneye wrote:The Tropical Cyclone Heat Potential factor is important for systems to grow rapidly.But so far 2009 TCHP is less than in 2008 although its still early.