The Environmental and Inner-Core Conditions Governing the Intensity of Hurricane Erin (2001)
Author(s) -
Thomas A. Jones,
Daniel J. Cecil,
Jason Dunion
Publication year - 2007
Publication title -
weather and forecasting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.393
H-Index - 106
eISSN - 1520-0434
pISSN - 0882-8156
DOI - 10.1175/waf1017.1
Subject(s) - environmental science , inner core , climatology , meteorology , storm , tropical cyclone , convection , intensity (physics) , eye , core (optical fiber) , front (military) , atmospheric sciences , geology , geography , physics , quantum mechanics , geophysics , optics
The evolution of Hurricane Erin (2001) is presented from the perspective of its environmental and inner-core conditions, particularly as they are characterized in the Statistical Hurricane Intensity Prediction Scheme with Microwave Imagery (SHIPS-MI). Erin can be described as having two very distinct periods. The first, which occurred between 1 and 6 September 2001, was characterized by a struggling tropical storm failing to intensify as the result of unfavorable environmental and inner-core conditions. The surrounding environment during this period was dominated by moderate shear and mid- to upper-level dry air, both caused in some part by the presence of a Saharan air layer (SAL). Further intensification was inhibited by the lack of sustained deep convection and latent heating near the low-level center. The authors attribute this in part to negative effects from the SAL. The thermodynamic conditions associated with the SAL were not well sampled by the SHIPS parameters, resulting in substantial ...
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