2018
DOI: 10.1029/2018gl078070
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The Control of Environmental Stratification on the Hurricane Maximum Potential Intensity

Abstract: This study examines the dependence of the hurricane maximum potential intensity (MPI) on environmental stratification beyond the traditional MPI framework. Unlike the previous formulation in which MPI is a function of the convective available potential energy in the eyewall only, a new MPI formulation is introduced herein that explicitly incorporates the effects of environmental stratification. The new formulation is examined within an axisymmetric modeling framework, using various initial vertical thermodynam… Show more

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Cited by 26 publications
(21 citation statements)
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References 43 publications
(80 reference statements)
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“…When the ELR is less than dry adiabatic lapse rate (DALR), the atmosphere is stratified and inhibits the rising motion of the air parcel. Apart from vertical wind shear (Lin and Chan, 2015;Murakami et al, 2011), the mid-level moisture content (Wang et al, 2010), tropical tropopause layer (Emanuel et al, 2013), and the environmental stratification (Shen et al, 2000;Hill and Lackmann, 2011;Tuleya et al, 2016;Kieu and Zhang, 2018) also play a major role in TC long-term intensity variations. Several model studies have reported that a more stable troposphere tends to be inimical to the development of deep convection, thereby limiting the growth of TC intensity.…”
Section: Thermal Instabilitymentioning
confidence: 99%
“…When the ELR is less than dry adiabatic lapse rate (DALR), the atmosphere is stratified and inhibits the rising motion of the air parcel. Apart from vertical wind shear (Lin and Chan, 2015;Murakami et al, 2011), the mid-level moisture content (Wang et al, 2010), tropical tropopause layer (Emanuel et al, 2013), and the environmental stratification (Shen et al, 2000;Hill and Lackmann, 2011;Tuleya et al, 2016;Kieu and Zhang, 2018) also play a major role in TC long-term intensity variations. Several model studies have reported that a more stable troposphere tends to be inimical to the development of deep convection, thereby limiting the growth of TC intensity.…”
Section: Thermal Instabilitymentioning
confidence: 99%
“…Specifically, the saturated CAPE in the eyewall must be sufficiently larger than the environmental CAPE for TCs to reach the theoretical MPI limit. A recent theoretical and modelling study by Kieu and Wang () and Kieu and Zhang () showed further that the large‐scale tropospheric static stability can additionally impose the potential intensity limit that a TC can reach, thus preventing the development of TCs for any arbitrary SST. In this regard, it is possible that SST must have a lower bound below which TC development would not occur.…”
Section: Resultsmentioning
confidence: 99%
“…The model was configured with a spatial-varying resolution for which the highest horizontal resolution of 3 km is set at the inner-core region and gradually increased to 15 km in the outer-core region. There were 40 vertical levels with the vertical resolution of 500 m. For each SST value, a spin-up run of 3 days in which random temperature and wind perturbations of 0.1 K and 0.1 mÁs −1 were added to trigger the convection in the model domain was conducted so that the model atmosphere can develop a vertical moisture and thermodynamic structure consistent with the assigned SST, similar to the approach used in Kieu and Zhang (2018). The model was then integrated for 20 days with an incipient vortex that has maximum surface wind of 10 mÁs −1 , using the sounding profile obtained as an area average of the temperature and moisture at the end of the 3-day spin-up.…”
Section: Appendixmentioning
confidence: 99%
“…Also, this study only used the elevation data to perform the segmentation to examine the effect of the elevation gradient on the land use. Other features could be selected and tested to generate the stratification with multiple environmental variables [26,27]. Considering the data availability, only temporal scales of partial driving factors with obviously changes from 2000 to 2015 were updated to simulate the land use in 2030 ( Figure 9).…”
Section: Discussionmentioning
confidence: 99%